Tag: National Geodetic Survey

  • The year 2020 and the surveyor: What we learned

    The year 2020 and the surveyor: What we learned

    If there were ever a time to sit back and reflect on things that have happened in the last calendar year, the year 2020 will be the poster child for the next few generations (at least I hope so…). Because of several things that have happened worldwide in the profession of surveying, let us take this opportunity to look back on a year that was filled with new equipment, emerging technology and government interaction that will have a lasting effect on our surveying horizon.

    Look at all of these wonderful toys

    There was no shortage of introductions to new equipment for surveyors, especially in the GNSS receiver market. While combining GNSS capability with an inertial measurement unit (IMU) is not a new concept, the Big Three of Leica, Topcon and Trimble introduced new or upgraded versions of their latest receivers taking full advantage of the technology. The benefit of having the IMU integrated within the receiver is the ability to “tilt” the instrument yet having the calculated position remain at the tip of the receiver pole.

    Photo: Trimble
    Photo: Trimble

    Leica, however, takes the tilting feature to another level with an integrated camera that allows for close-range photographs to capture additional information through remote sensing software. The data extracted from the photographs can be simple points (and verified in the data collector while in the field) or point clouds that can be integrated into larger projects through the Leica office software.

    These new receivers, along with upgraded models from smaller providers, have opened the GNSS market to many more users well beyond surveying. The combination of more capability through advancing satellite constellations, more robust processors, and reduced receiver sizes have continued to drive GNSS positioning growth.

    Photo: Hexagon
    Photo: Hexagon

    Manufacturers are using these increased capabilities to promote better coverage to obtain positions under heavier canopies and less likelihood for multi-path errors. While I remain cautious about these claims of increased coverage, I also maintain that with any tool, measurements and positions must have proper and appropriate validation. However, I am impressed that the technology continues to advance with what was once seen as only applicable to the open sky.

    Not all the new technology has emerged through the GNSS receiver product lines; several less visible but valuable features have been introduced within the robotic total station lines. The manufacturers continue to push their equipment to react faster, stay locked on targets better, and provide more reliable solutions to data collection and construction layout. Data collectors continue to evolve with larger screens and more software capability, with some rivaling their desktop counterparts.

    As cellular networks grow in both size and speed, more direct connections between field and office are being made with faster response time to data transfer. Data collection can take place in the field and be analyzed by an office technician as it happens. Go another step further and add an aerial background image to the collector and/or the office computer; now each team member can confirm that the information being collected is sufficient for the project in real-time.

    Another technology that continues to advance is remote sensing, with more devices being introduced and with increased software capabilities. Besides new and upgraded offerings from the surveying-based manufacturers, other device makers are introducing products that offer remote sensing to the masses. The biggest news in this arena was the announcement from Apple that the iPhone 12 Pro and iPad Pro would come equipped with lidar sensing technology along with incredible photographic capabilities.

    While there does not seem to be specific apps developed for surveyors at press time, it is safe to say that there will be in short order. It is also a safe bet that having this capability on a mass-produced device will put pressure on the surveying and mapping equipment manufacturers to be cost-competitive on their own proprietary devices or risk losing out on market share.

    UAVs continue to be the fastest-growing segment of the surveying industry. More vehicle, sensor and software providers are coming to market to offer the surveyor a variety of choices. DJI continues to lead the way in the multi-rotor category with new products and sensors while other manufacturers are embracing the fixed-wing and vertical take-off and landing (VTOL) platform for greater range.

    Just like their automobile brethren, flight time continues to increase with discoveries of new battery compositions and weight considerations. The sensor market is expanding to include more affordable lidar units, as well as new technology in multispectral identification, gas and noxious odor detection, and much more.

    Software developers, too, continue to refine and expand the features found in their geospatial offerings with advancing technology and programming. Google Maps is the default navigation app for many smartphone users, but like anything utilizing GNSS in dense urban areas, the users find themselves bouncing all over the map.

    While surveyors recognize this as multipath, the smartphone user does not have any way to remedy this trouble. Google recognizes this issue and has been working on a programming fix to help minimize these positional errors. This is another example of how precise position determination has become a significant goal for our society, with the more correct position, the better.

    Meanwhile, in Washington D.C….

    2020 did not see any shortage of government action for the surveying and mapping community. As with many topics that come out of the nation’s capital, it should not surprise anyone that several of the items considered by the federal government and its agencies were not without controversy.

    The biggest and most controversial item continues to be the advancement of Ligado (formerly known as LightSquared) and the development of new communication technology that has been shown to interfere with the GPS transmission bands. The Federal Communications Commission (FCC), led by Chairman Ajit V. Pai, has been successful in holding off all challenges to the new technology including ones from current legislators and defense staff.

    The main argument from the FCC is the value of the system as a provider of 5G communication to a substantial portion of the country. They also make statements that safeguards are being taken to protect the GPS spectrum, yet many studies from outside parties show otherwise. The fight over this spectrum will continue into 2021, and it will be interesting to see if the new administration will see things from a different perspective.

    Several items to come out of Washington, D.C., late in the year were the blacklisting of DJI and the announcement of new UAV rules for flying over crowds and at night. With the DJI ruling, it is now illegal for government agencies to use the Chinese-based UAV maker for any activities. Based upon the significant market share of DJI, one can only wait to see how this situation plays out, and if the ban is expanded to private individuals.

    The FAA announcement on the new UAV flight rules was surprising but not unexpected. In addition to establishing flight limitations over crowds and at night, it also established a timeframe for requiring most UAVs to transmit a Remote ID during flight for determining who is flying and where they are located. Compliance with these rules will be required by the manufacturer within 18 months and by UAV pilots within 30 months.

    The National Geodetic Survey (NGS) has also been busy during 2020 preparing new datums and specifications for upcoming changes to the National Spatial Reference System (NSRS). Among those changes are the deprecation of the U.S. Survey Foot, beta testing of the latest geoid model (GEOID20), and new software tools for transforming positional information between datums. It was also announced that the release of the modernized NSRS scheduled for 2022 was being delayed.

    NGS continues to work with each state on the improved state plane coordinate systems and/or low distortion projection systems that will be implemented with the new NSRS rollout. All these efforts have been a monumental task (no pun intended) and kudos go out to NGS for getting everything this far.

    Pandemic 2020 (No, this is not a movie or a drill)

    As we covered in the May 2020 Survey Scene article, COVID-19 was unlike anything we had been exposed before. Initial reports tried to relate the virus to typical influenza and the H1N1 outbreak in 2009, but the rapid transmission and sheer volume of cases (and deaths) mostly eliminated those comparisons.

    From a technical viewpoint, the situation with COVID-19 has no bearing on GNSS operations and positional establishment. An operator of a GNSS receiver, and the business of surveying, is greatly affected by the presence of COVID-19 so it does deserve more than a brief mention in a retrospective look at the past year. This virus upended everything; from data collection and survey-related activities to computations and final drafting, the business of surveying felt the effects.

    Once the initial challenges of keeping everyone safe were addressed, it became a year-long marathon of providing surveying services to clients that did not let the pandemic hinder their progress. Field crews were under significant pressure to maintain social distancing at every turn, while office staff dealt with home Wi-Fi and lack of access to normal business conditions such as large-format printing.

    Video calls and instant messaging quickly became the norm, yet also became the scourge of dealing with the day-to-day operations of a business. The “normal” work/life balance with families, school, and social activities has disappeared and a more challenging approach has replaced that balance. Fingers are crossed that people will adhere to social distancing protocols and can get vaccinated as soon as possible so we can resume a portion of our previous lifestyles.

    However, we do have several positive things to take away from the challenges of the pandemic that will make our lives better going forward. Our reliance on geolocation became quite clear throughout the pandemic. Whether it is using it to help establish contact tracing or as simple as having a delivery service bring necessities straight to your door, almost everyone relies on geolocation for helping guide them through the “new normal.”

    We are using our smartphones to track our family members and help keep them out of harm’s way. It would be hard to imagine how much more difficult this situation would have been before cellphone and GNSS integration.

    Graphic: World Health Organization
    Graphic: World Health Organization (https://www.who.int/emergencies/diseases/novel-coronavirus-2019).

    Another leap forward that most people are not aware of is the publicizing of GIS dashboards and incredible analysis of the geolocation of people worldwide. While GIS dashboards have been in existence for many years, it is only now that the public has paid attention to the vast information available to them.

    From providing numbers of cases to graphically depicting “hotspots” across the world, these dashboards are full of useful information to help people understand the size of this pandemic, the places where mitigation is working, and where additional restrictions are being put in place to help reduce the spread of COVID-19.

    The ability to merge geolocations with physical conditions and situations into a real-time mapping solution can help reduce the spread of the virus. By combining GNSS technology with advanced computing power and data storage, the power of GIS has been brought to the front page of public agencies and news sites.

    While we still enjoy watching movies with superheroes, the true heroes during this pandemic are the frontline health workers, first responders and data analysts/programmers who bring us this timely information quickly. A hearty thank you goes out to all of them for their efforts and dedication to the cause.

    In memoriam

    Photo: GPS World staff
    Photo: GPS World staff

    The year 2020 also brought losses to every corner of the world and the surveying community was not spared. There are very few individuals we call pioneers in the surveying industry, so to include Dr. Javad Ashjaee among that group is no small feat. His contributions to the surveying profession helped turn every practitioner into a geospatial information provider.

    From his early days at Trimble pioneering the commercial-grade receiver to creating his company at Ashtech and embracing GLONASS with GPS, he continued to expand the capability of the GNSS receiver. Many surveyors today only know his name through his latest company, Javad GNSS, and the unique line of receivers and measuring devices and their distinctive green color.

    Cover photo: Ed Koziarski
    Cover photo: Ed Koziarski

    Dr. Ashjaee was a big part of the GNSS revolution, so next time you starts up their receiver to collect survey data, take a moment to thank him. It was my pleasure to meet and interview him at the 2017 Intergeo trade show in Berlin to talk about his product line. I was also able to test-drive his incredible GNSS products for a feature in GPS World magazine on using smartphones for data collectors.

    To say the man will be missed is a big understatement and I wish his family well on continuing his company and tradition of making great leaps in technology.

     

  • ArcGIS web app incorporates datasets, NGS data layers for surveyors

    ArcGIS web app incorporates datasets, NGS data layers for surveyors

    My last column described a new National Geodetic Survey (NGS) webtool for obtaining geodetic information about a passive mark in their database. The column highlighted some features that may be of interest to GNSS users. It provides all of the information about a station in a more user-friendly format. This column highlights an ArcGIS web application that incorporates various California specific datasets and NGS data layers to assist surveyors planning vertical control surveys. The GNSS Leveling Web Application was provided to me by Jay Satalich, chief, Office of Surveys, Caltrans (see box titled “Linkedin Notification from Jay Satalich).

    Linkedin Notification from Jay Satalich

    Supervising Transportation Survey (Chief, Office of Surveys) at State of California, Department of Transportation:

    “GNSS Leveling Web Application” [is] an Esri ArcGIS online web app created for my “GNSS Leveling” students at College of the Canyons. Designed as a practical tool when planning vertical control surveys using GNSS. National datasets include: National Spatial Reference System (layers: satellite visibility, stability, and vertical control source), geology, and GEOID18 (layers: GEOID18 height, difference between GEOID18 and GEOID12B, and GEOID18 uncertainty). California-specific datasets include: oil/gas/fracking/injection wells, fault lines, oil fields, groundwater basins, and landslide areas. The NOAA National Geodetic Survey data layers were created and published by Brian Shaw. People who influenced development of this app include Dave Zilkoski, Kevin M Kelly, Ken Hudnut, David D Jackson, Ross S. Stein, and Arthur Sylvester.

    Go to the app here.

    The box titled “GNSS Leveling Web Application” depicts a map of the Los Angeles area that provides the list of published marks in NGS’ database with an overlay of the uncertainty of NGS’ hybrid geoid model GEOID18. Plotting the published marks from NGS’ database is very useful for surveyors reconning marks for a GNSS survey project. The attributes allow users to quickly identify stations that have published heights from leveling adjustments projects (labeled as ADJUSTED) and those that have heights published from GNSS adjustments projects (labeled as GPS OBS). (See here for definition of attributes.)

    GNSS Leveling Web Application

    (https://www.arcgis.com/apps)

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    The list all of the layers of the web application are provided in the box titled “GNSS Leveling Web Application Layers.” (Note: After you open up the web application, click on the Layers icon to obtain the list of available layers.)

    GNSS Leveling Web Application Layers

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    As you can see from the list of layers, the web application enables users to select the layers that are pertinent to their survey project requirements. The application is designed for California surveyors but the concept is transferable to other States. For example, the following layers are not just for California surveyors: Arizona water wells, Louisiana oil and gas well, U.S. oil and natural gas wells, Principal Aquifers of the United States, and, of course, all of the NOAA NGS data layers.

    One layer that is very important to California users is the layer that provides the fault activity in their region. The box titled “Fault Activity Map of California: Pre-Quaternary and Quaternary Faults – Quaternary Faults” depicts the list of published marks in NGS’ database with an overlay of the fault activity map.

    Fault Activity Map of California: Pre-Quaternary and Quaternary Faults — Quaternary Faults

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Another great feature of the application is that it has a layer providing the satellite visibility code for published NSRS marks (see the box titled “Published NSRS Stations (by satellite visibility”). Once again, a great feature for field personnel performing reconnaissance.

    Published NSRS Stations (by satellite visibility)

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    The application also has a feature that lists the marks that were involved in the development of NGS’ hybrid geoid model GEOID18. (see the box titled “GNSS Leveling Web Application GEOID18 GPS on Bench Mark Layer”). Clicking on a mark’s icon provides information and statistics about the mark (see boxes titled “GEOID18 GPS on Bench Mark Layer — PID EW6989” and “Information for GPS on Bench Mark for PID EW6989”). This is one of the layers that provides information for the entire CONUS region. All this information is available from NGS’ website but this application incorporates all of NGS’s data as well as the local information in one application. This web application is very useful to a surveyor planning a survey project and/or providing information to a field reconnaissance team.

    GNSS Leveling Web Application GEOID18 GPS on Bench Mark Layer

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    GEOID18 GPS on Bench Mark Layer — PID EW6989

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Information for GPS on Bench Mark for PID EW6989

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Users that are participating in NGS’ GPS on Bench Mark program can click on the layer for “NGS GPS on Bench Marks Transformation Service Tool, priority 10 km hex” to determine marks that need to be occupied by GNSS to improve a transformation tool being developed by NGS. See boxes titled “NGS GPS on Bench Marks Transformation Service Tool, priority 10 km hex” and “Information for GPS on Bench Mark Priority List for PID EW6989.” There’s also layers that depict the priority mark list for the GPS on Bench Marks program (“NGS GPS on Bench Marks Transformation Tool Service — priority mark list”) and the 2 km hexagon priority grid (“NGS GPS on Bench Marks Transformation Tool Service — priority 2km hex”).

    NGS GPS on Bench Marks Transformation Service Tool, priority 10 km hex

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Information for GPS on Bench Mark Priority List for PID EW6989

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Source: Esri ArcGIS GNSS Leveling Web Application
    Source: Esri ArcGIS GNSS Leveling Web Application

    Individuals interested in participating in NGS’ GPS on Bench Mark program should register for NGS’ Dec. 10 webinar, which will discuss the status of the program. See the box titled “GPSonBM Transformation Tool Campaign Update — 12 months remaining” for the information on the webinar. Users can register for the webinar here. I would encourage all users to access the web application tool developed by Jay and/or NGS’ website before participating in the next NGS GPS on Bench Mark webinar.

    GPSonBM Transformation Tool Campaign Update — 12 months remaining

    (NGS webinar series)

    Screenshot: National Geodetic Survey
    Screenshot: National Geodetic Survey

    Almost all of my columns have focused on establishing accurate GNSS heights. Most of my 45 years of working in the field of geodesy has been focused on heights; that is, leveling-derived orthometric heights, GNSS-derived orthometric heights, and geoid heights. Gravity is very important to estimating all of these types of heights. Recently, a colleague sent me a video proving Galileo’s famous gravity experiment. It’s an older video (November 2014), but it’s really fascinating. You can see the entire video here. Another individual pointed me toward the same experiment performed on the Moon during the Apollo 15 mission. What’s amazing to me is that over 400 years ago an individual spent time studying the effects of gravity and developing the concept of acceleration due to gravity. I wonder what the world would look like today if Galileo would have just accepted Aristotle’s theory of gravity (which states that objects fall at speed proportional to their mass) and decided to focus on other tasks. Saying that, I am amazed that most geospatial users do not realize the importance of gravity (and physical geodesy) in the development of the geospatial products and services that they use daily; and, how critical it is that more research is required to meet future geospatial needs. The advancements in satellites and computers have enabled geodesy to expand into many different disciplines. Geodetic science and technology now underpin many sciences, large areas of engineering (such as driverless vehicles and drones), navigation, precision agriculture, smart cities, cellular telephones, and location-based services. (See the GPS World First Fix column about the shortage of American geodesists).

    When I end one of my presentations, I always emphasize that Geodesy Provides the Foundation for all Geospatial Products and Services, and Integrated and Collaborative Organizations Create Geospatial Solutions. Geodesy is just as important today as it was 400 years ago.

    I hope everyone stays safe during this COVID-19 pandemic and enjoys the holidays.

  • NGS releases beta tool for obtaining geodetic information

    NGS releases beta tool for obtaining geodetic information

    NGS has developed a new beta tool for obtaining geodetic information about a passive mark in their database. This column will highlight some features (available as of Oct. 5, 2020) that may be of interest to GNSS users. It provides all of the information about a station in a more user-friendly format. The box titled “Passive Mark Lookup Tool” is an example of the webtool. The tool provides a lot of information so I have separated the output of the tool into several boxes titled “Passive Mark Lookup Tool — A through D.”

    I will highlight several attributes that I believe will be very useful to users, especially users of leveling-derived and GNSS-derived orthometric heights. I’ve highlighted several attributes in the box titled “Passive Mark Lookup Tool — A” that are important to users such as published coordinates, their datum and source, Geoid18 value, GNSS Useable, and the date of last recovery. All of these values are available on a NGS datasheet but, in my opinion, this provides the information in a more user-friendly format.

    Passive Mark Lookup Tool — A

    (https://beta.ngs.noaa.gov/datasheets/passive-marks/index.html)

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    One calculation that the user can easily compute for marks that have been leveled to and occupied by GNSS equipment, is the difference between the published leveling-derived orthometric height and the computed GNSS-derived orthometric height. This may indicate that the mark has moved since the last time it was leveled to or that its height coordinate has been readjusted since the creation of the published geoid model.

    The table below provides the calculation using the data from the box titled “Passive Mark Lookup Tool — A.” The calculation [HGNSS = hGNSS — NGeoid18; Difference = HGNSS — HNAVD 88] has been described in several of my previous columns (this one, for example).

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    In this example, the difference between the GNSS-derived orthometric height and the Published NAVD 88 height is 6.1 cm. NGS is looking for comments on this beta webtool so if users would like this computation added to the tool, they should send a comment to NGS using the link provided on the site (This is a beta product. NGS is interested in your feedback concerning its function and usability as well as how users would like to interact with NGS datasheet information in the future. Email us at [email protected].) So, the user should ask the question, did the station move since the last time it was leveled?

    Another attribute that would be nice to be part of this tool is which station was used to create the hybrid geoid model. As of Oct. 5, 2020, users have to go to the Geoid18 webpage to get the information. The Excel file and shapefiles provide whether the station was used to create the Geoid18 model. In the case of this example, KK1531, CHAMBERS, the mark was not used in the creation of Geoid18 so NGS felt that the station may have moved and/or the GPS on Bench Mark residual was large relative to its neighbors. See NGS’s technical report on Geoid18 for more information on the creation of Geoid18. The GPS on Bench Mark residual analysis was described in several of my previous columns (see “The differences between Geoid18 values and NAD 83, NAVD 88 values” and “NGS 2018 GPS on BMs program in support of NAPGD2022 — Part 6” for examples).

    The webtool provides a map depicting the location of the station, photos (if available), and previously published, superceded values of the mark. See the box titled “Passive Mark Lookup Tool — B.”

    Passive Mark Lookup Tool — B

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    In the example of Chambers, KK1531, no photos were available. It would be helpful if a user would provide photos to NGS when visiting this station. (Note: NGS has a webtool for users to submit recovery information about a mark as well as to provide current photos of the station.) The new Passive Mark webtool also provides information about the survey projects that the mark has been involved in such as leveling and GNSS projects.

    In this example, mark CHAMBERS was leveled to in a 1984 first-order, class 2 leveling project (Leveling Line number L24838/6) and, in 1995, the mark was part of a GNSS project (GNSS Project GPS1010). It also provides all the descriptive text and recovery information (See boxes titled “Passive Mark Lookup Tool – C” and “Passive Mark Lookup Tool – D”).

    Passive Mark Lookup Tool — C

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    Passive Mark Lookup Tool — D

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    I want to highlight a few other attributes of this webtool. The station, PID AA3862, has an interesting attribute that users should take note of; that is, the NAD 83 (2011) position source is NO CHECK. See box titled “Passive Mark Page for PID AA3862.”

    This means that the mark’s NAD 83 (2011) coordinates were determined without redundant observations. This is not a good survey practice but there are times that a project may contain check observations for some purpose or, more likely, the mark did contain other GNSS vector but they were rejected in the final adjustment. Either way, a good survey practice would be for users to verify the coordinates of these marks before using them.

    Passive Mark Page for PID AA3862

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    As previously mentioned, the tool provides the location of the station on a map and photos if they are available. This is a really nice feature for anyone searching for the mark. The map can be enlarged as well reduced by clicking on the box. See boxes titled “Passive Mark Page for PID AA3862” and “Photos of Mark PID AA3862.” The box titled “Photos of Mark PID AA3862” provides all three photos of mark PID AA3862.

    Photos of Mark PID AA3862

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey
    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    It should be noted, according to the Geoid18 GPS on BMs dataset that users can download, this station, AA3862, was not used in the creation of Geoid18. The table below provides the difference between the GNSS-derived orthometric height and the published NAVD 88 height.

    In this example, the difference between the GNSS-derived orthometric height and the published NAVD 88 height is 9.9 cm. Also, the webtool provides the network accuracy values for the station. In this example, the horizontal network accuracy is 20.65 cm and the vertical network accuracy value is 14.50 cm (see highlighted values in box titled “Passive Mark Page for PID AA3862”). These are very large network accuracy values. This should be a flag to anyone that is using this station as control.

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    As I previously mentioned, as a beta site, users should verify all information from the site. NGS is requesting feedback on this tool so they can improve it and make it an operational webtool. I encourage everyone to access the tool and check out a few of their favorite marks, and then send an email to NGS informing them of what you like, what you would like to change, and what you would like to see added to the tool.

    NGS is releasing this tool as a beta product to get feedback from users. As NGS states in the heading of the tool, they are interested in your feedback concerning its function and usability as well as how users would like to interact with NGS datasheet information in the future. Email NGS at [email protected].

    One last item that may be of interest to GNSS users is that NGS, working with the University Corporation for Atmospheric Research (UCAR), developed another online GNSS lesson (see box titled “New GNSS Lesson by NGS and UCAR”). These lessons are free but users must sign up to access the website and lesson.

    New GNSS Lesson by NGS and UCAR

    Image: National Geodetic Survey
    Image: National Geodetic Survey
  • The expanded role of positioning through advancements in GNSS

    The expanded role of positioning through advancements in GNSS

    Auto Mining: A driverless Cat 793F CMD truck leaves an iron ore pit. (Photo: Caterpillar)
    Auto Mining: A driverless Cat 793F CMD truck leaves an iron ore pit. (Photo: Caterpillar)

    Individuals who use GNSS today may not know the significant advancements that have been accomplished over the past 30 years to obtain accurate GNSS-derived coordinates, especially GNSS-derived orthometric heights.

    Thirty years ago, there were two limiting factors for estimating GNSS-derived heights — estimation of accurate ellipsoid heights in a timely manner and the availability of an accurate geoid model. The geoid model was only good to the decimeter level, between two stations relatively close together. A significant improvement of the measurement of the Earth’s gravity field (such as from the GRACE mission) and digital elevation data (from the Space Shuttle Radar Topography Mission) facilitated the creation of more accurate geoid models. Geoid models went from decimeter values to centimeter, and then sub-centimeter values between closely spaced marks.

    A new national network

    During the past three decades, the U.S. National Geodetic Survey (NGS) has developed a national network of Continuously Operating Reference Stations (CORS). These CORS, along with the states’ real-time networks (RTNs), have provided the ability to compute accurate GNSS-derived coordinates in an efficient and effective manner. The modeling of antenna phase patterns was a critical development for combining different types of antennas.

    Today’s GNSS processing software is basically a “hands-off black-box” system. But 30 years ago, the analyst had to identify cycle slips and ensure that all unknown cycle ambiguities of the carrier-phase data (integers) were determined correctly. It was a time-consuming task, and analysts needed to understand the data. So many things can go wrong when someone relies on an answer from a black box. That said, federal agencies such as NGS and GNSS software companies have produced hands-off software that provides statistics and warning messages, as well as guidelines for ensuring results are consistent and accurate.

    The advancements in estimating GNSS-derived coordinates (including orthometric heights) have changed the way many industries do business. Farmers use it to drive their tractors and combines, mining companies control driverless vehicles, construction companies use automated machine guidance to build roads, and, of course, it has improved how individuals navigate from one location to the next.

    Hands-off farming and mining

    Thirty years ago, few farmers thought they would be able to sit in their cab and let their combine harvester drive itself. Geodesist, surveyors, and engineers had a vision of using GNSS to automate the use of farming and construction equipment, which became a reality.

    What will it be like in another 30 years? Will it be routine for individuals to program their car for a destination, and then sit back and read a book?

    Positioning with GNSS will be critical for the safety factor of driverless vehicles and the use of drones for delivery. Geodesists, surveyors and engineers, once again, need to lead the way to meet the positioning requirements of the future.

  • New NGS study examines GIS surveys for airports

    New NGS study examines GIS surveys for airports

    <a href="http://stage.globalpositioningnews.com/wp-content/uploads/2020/08/ASP-Revised-Final-Socio-Economic-Report-July-29-2020.pdf" target="_blank" rel="noopener noreferrer">Download the report.</a>

    A new study for the National Geodetic Survey (NGS) reviews and validates airport surveys from a safety perspective.

    The study, “Protecting Against Airport Obstructions: Socio-Economic Study of the NGS Aeronautical Survey Program,” is by Irv Leveson and the staff of ARCBridge Consulting and Training Inc.

    Goals of the scoping study are to:

    • provide a better understanding of the activity, uses, users and broader beneficiaries of the National Geodetic Survey’s Aeronautical Survey Program,
    • help define its socio-economic benefits,
    • provide preliminary order of magnitude estimates of benefits of the program, and
    • examine influences on future needs for the program’s services.

    The footprint (trade space) analysis presents data on airport improvement grants, activities of the program, airports, aviation and societal beneficiaries. Methods of estimating socio-economic benefits are considered, preliminary estimates of benefits are made and issues that will affect use of the services in the future are discussed. Additional information is included in 10 appendices.

    The FAA Airport Improvement Program (AIP) provides grants, to public agencies for planning and development of the 3,249 eligible public-use airports and the 72 privately owned civil airports.

    The FAA requires that geographic information system (GIS) contractors submit plans and surveys with geodetic control, runway, navigational aid, obstruction and other aeronautical data under its Airports GIS (AGIS) program. These contracted survey plans and surveys are sent to the NGS Aeronautical Survey Program (ASP) for quality assurance review.

    The GIS information is used by the FAA in establishing flight rules and other requirements to assure safety.

    Download the report here.


    Irv Leveson is an economist with extensive experience examining GNSS markets, applications, benefits and policies. His public studies include: “The Economic Benefits of GPS.” He recently led a National Geodetic Survey study.

  • NGS releases modernized National Spatial Reference System updates

    NGS releases modernized National Spatial Reference System updates

    The National Geodetic Survey (NGS) recently announced two new items related to the modernized National Spatial Reference System (NSRS). First, it announced that there will be a delayed release of the modernized National Spatial Reference System (NSRS). See the box titled “Updates notices from NGS Homepage” for the link to the notice.

    Updates notices from NGS Homepage

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Delayed Release of the Modernized NSRS” provides a summary of the notice. The announcement stated they are performing a thorough review of all tasks and will provide regular updates on their progress. What this means is that the modernized NSRS will not be completed by 2022. Even if it’s delayed a couple of years, it’s never too early to obtain an understanding of the new, modernized NSRS, and start preparing for the transition to the new NSRS.

    Delayed Release of the Modernized NSRS

    (https://www.ngs.noaa.gov/datums/newdatums/delayed-release.shtml)

    NOAA’s National Geodetic Survey (NGS) is announcing a delay in the release of the modernized National Spatial Reference System (NSRS).

    In 2007, NGS began planning for the modernized NSRS, acquiring its first airborne gravimeter, creating and initiating the Gravity for the Redefinition of the American Vertical Datum (GRAV-D) project and by 2008 had codified its modernization plans into a Ten Year Plan. At that time, the target completion date was 2018. By 2013, that date seemed unlikely, due to both the broadening of the GRAV-D coverage area and the experience of five years of operational planning and execution.

    In 2013, NGS revised its 2008 Plan, and targeted 2022 as the date of the release of the modernized NSRS. This date was reinforced with a 2018 Strategic Plan revision. By 2017, confidence in hitting the 2022 target was high enough to reach final agreement with Canada and Mexico on a naming convention for certain components, to include “2022” in their names.

    Since 2017, operational, workforce, and other issues have arisen and compounded, causing NGS to recently re-evaluate whether a successful roll-out by 2022 is possible. The most significant impacts have been in workforce hiring and retention, and in meeting GRAV-D data collection milestones, which underpin the NSRS modernization efforts.

    NGS is currently conducting a comprehensive analysis of ongoing projects, programs and resources required to complete NSRS modernization and will continue to provide regular updates on our progress. To get the latest news on NSRS modernization and track our progress, subscribe to NGS News or visit our “New Datums” web pages.

    The second important announcement by NGS was that two Federal Register Notices related to the modernized NSRS were published on July 24. See the box titled “NGS News.”

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The first Federal notice was titled “Upcoming Changes to the National Spatial Reference System.” See the box titled “Federal Register Notice titled Upcoming Changes to the National Spatial Reference System” for the summary. This announcement provides a statement about the new, modernized NSRS and that it’s going to be published between 2022 and 2025. The information about the modernized NSRS shouldn’t be new to anyone that’s been reading my newsletters, but the Federal Notice makes it official and NGS provides dates of when the modernization will be rolled out.

    Federal Register Notice titled “Upcoming Changes to the National Spatial Reference System”

    (https://www.govinfo.gov/content/pkg/FR-2020-07-24/pdf/2020-16068.pdf)

    Image: Federal Register
    Image: Federal Register

    The second Federal Notice was titled “Consideration of Potential Age Limiting Observations To Be Used To Compute 2020.00 Reference Epoch Coordinates in the National Spatial Reference System.” This is a very important notice that users of NGS published coordinates should read and understand. NGS is considering imposing data age limits that will be part of the new, modernized NSRS. See the box titled “Imposing Age Limits of Data in 2022” for a summary of the Federal Register Notice announcement.

    Imposing Age Limits of Data in 2022

    (https://www.federalregister.gov/d/2020-16084)

    Image: Federal Register
    Image: Federal Register

    My last column highlighted that in the modernized NSRS the only way to get “into the datum” will be through a GNSS survey. It noted that leveling projects generate relative height differences not absolute heights. It emphasized that in the new modernized, time-dependent NSRS, the absolute height will be provided by up-to-date GNSS data; and the relative height differences between leveling marks will be provided by the leveling data. Many of my previous newsletters have explained different aspects of the new NSRS and how it may affect the surveying and mapping community products and services. As the Federal Register Notice implied, at this moment, NGS expects large uncertainties in the vertical component of the Intra-Frame Velocity Model (IFVM) which will translate into the GNSS-derived height Limiting the age of data will help to reduce the amount of uncertainty in the vertical component based on older data. Saying that, this could have an impact on users that rely on coordinates established using data acquired prior to 2010. NGS is requesting that users take new GNSS observations on all stations of interest that haven’t been occupied since the year 2010. The supplementary information in the Federal Register notice contains some very important statements. I have highlighted several statements in the box titled “Supplementary Information from Imposing Age Limits of Data in 2022.”

    NGS hasn’t decided on the date of the age limit but the notice states that “For instance, it is unlikely that such an age-limit will be fewer than 10 years.” This is why NGS recommends the following “that users take new GNSS observations on geodetic control marks of interest that have not been surveyed since January 1, 2010, and asks the users to submit the observations to NGS before December 31, 2021.” Another important item in the supplemental information section is that NGS is enhancing the OPUS-Projects tool to include real-time kinematic and real-time network (RTK/RTN) observations. This should help to facilitate users submitting data on marks of interest so that they will have 2020.0 Reference Epoch Coordinates (REC).

    Supplementary Information from Imposing Age Limits of Data in 2022

    (https://www.federalregister.gov/d/2020-16084)

    SUPPLEMENTARY INFORMATION:
    In 2017, the National Geodetic Survey (NGS) announced its plans to estimate RECs on a five-year cycle in NOAA Technical Report NOS NGS 67, 2019, starting with the first reference epoch at 2020.00, as part of the modernization of the NSRS. In the Technical Report, the exact observations to be used for this estimation were listed as “To Be Determined.” NGS is considering imposing age limits upon the observations that will be used, particularly because of expected uncertainties in the vertical component of the IFVM. These age limits cannot be determined until additional well-structured, data-driven experiments are conducted. Such experiments are expected to occur during the 2020 reference epoch adjustment projects (geometric, orthometric, and gravimetric), which are scheduled for calendar year 2022.

    However, since the cut-off for new observations to enter those adjustment projects is December 31, 2021, any decision to age-limit input observations will come too late for submissions to impact the 2020 RECs. While the cut-off for age-limited observations is unknown, certain assumptions are safe to make. For instance, it is unlikely that such an age-limit will be fewer than 10 years. Older observations may be used in the estimation of 2020 RECs, but this cannot be guaranteed. As such, NGS requests that users take new GNSS observations on geodetic control marks of interest that have not been surveyed since January 1, 2010, and asks the users to submit the observations to NGS before December 31, 2021. Users may either (a) submit existing unsubmitted observations through the OPUS-Share tool or (b) conduct new GNSS observations and submit the data to NGS via the OPUS-Share tool.

    In order to increase the submission of GNSS observations on marks, NGS is prioritizing the finalization of an expanded OPUS-Projects tool, which will allow real-time kinematic and real time network (RTK/RTN) observations to be submitted, rather than the standard four-hour observations required in OPUS-Share. Initial roll-out of this new tool is expected to occur during calendar year 2020.

    This action is designed to increase both the number and the coordinate accuracy of geodetic control points, which in the modernized NSRS will have an estimated 2020.00 REC. Historically, NGS has combined data across multiple decades to estimate geodetic coordinates, yet such efforts have not fully accounted for the lack of information about vertical motion of geodetic control points throughout the years. Since height information is critical to the understanding of floods, failure to compute heights accurately can have negative impacts on property and lives. NGS views periodic re-surveys of geodetic control points, rather than the estimation of coordinates from observations that are years (or even decades) old, as the most effective way to maintain accurate and up-to-date knowledge of geodetic coordinates, including heights. As such, this announcement provides users of the NSRS with advance notice that geodetic control points of interest to them should be re-surveyed for the most accurate representation of geodetic coordinates, including heights.

    NGS has scheduled a webinar for August 27, 2020, to discuss the delayed release of the modernized NSRS. See the box titled “Webinar on Delayed Release of the Modernized NSRS” for the announcement and web link to register for the webinar. I would encourage all users of the NSRS to register for this webinar.

    Webinar on Delayed Release of the Modernized NSRS

    (https://geodesy.noaa.gov/web/science_edu/webinar_series/delayed-release-nsrs.shtml?utm_medium=email&utm_source=GovDelivery)

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Many users are probably wondering if the delay in the new, modernized NSRS will change the dates of other deadlines. The FAQs webpage addresses some of these questions. I have highlighted a few FAQs in the box titled “Questions from NGS FAQ Website.”

    Questions from NGS FAQ Website

    (https://www.ngs.noaa.gov/datums/newdatums/FAQNewDatums.shtml)

    How will the delay affect the GPS on Benchmarks Phase II deadlines?

    The deadline for submittal of GPSonBM data for the 2022 Transformation tool will remain December 31, 2021

    If SPCS2022 zone designs are completed before other parts of NSRS modernization, will SPCS2022 be released sooner?

    No. SPCS2022 is explicitly defined with respect the four 2022 terrestrial reference frames (not NAD 83), and SPCS2022 will be released along with the roll-out of those frames. If the frames are rolled out prior to other parts of the NSRS modernization, the frames will be accompanied by SPCS2022 (see the previous FAQ about phased roll-outs).
    However, complete definitions of all SPCS2022 zones will be made available as soon as they are finalized. NGS expects that to occur by the end of 2021. Providing zone definitions early will give software vendors, database administrators, and others ample time to adopt and test them in their systems. Doing so will ensure SPCS2022 is available for immediate use upon roll-out of the 2022 terrestrial reference frames.

    My projected height change seems to return me to NGVD 29 heights. Is this a coincidence?
    This is coincidental. It so happens that, in some areas of the country the actual orthometric height in a region happens to be numerically closer to NGVD 29 than NAVD 88. NGVD 29 itself has biases and tilts which make it as inappropriate of an estimate of true orthometric heights as NAVD 88

    [NOTE: I have heard this question from many of my readers so I provided an approximate estimate of the differences between NAPGD2022 orthometric heights and NGVD 29 height values in my June 2017 Survey Scene column. See figure below labeled “Figure 2 from June 2017 Survey Scene Newsletter.”]

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Figure 2 from June 2017 Survey Scene Newsletter

    Future newsletters will address updates on the modernized NSRS as they become available to the user community.

  • Number of trained US geodesists at crisis level

    Number of trained US geodesists at crisis level

    By David Zilkoski, contributing editor, survey scene

    David B. Zilkoski
    David B. Zilkoski

    I attended The Ohio State University (OSU) to obtain my graduate degree in Geodetic Science in 1979. Therefore, I will admit that I am a little biased — once a geodesist, always a geodesist. The basic definition of geodesy is the applied science for determining the size and shape of the Earth, designing and realizing reference frames, and determining where you (and anything else) is on the Earth.

    In OSU’s geodesy heyday (1960–1990s), many Americans trained were sent by federal agencies: National Geospatial-Intelligence Agency (NGA), NOAA/National Geodetic Survey (NGS), USGS, Army, Navy and Air Force. During the 1970s, NGS was sending two employees back to school every year. These agencies needed geodesists because they were undertaking major projects such as NGS’ to readjust the U.S. national horizontal (NAD83) and vertical geodetic (NAVD88) networks.

    I was one of the employees that NGS sent to OSU to be trained to support the NAD83 and NAVD88.

    The advancements in satellites and computers have enabled geodesy to expand into many different disciplines. Geodetic science and technology now underpin many sciences, large areas of engineering (such as driverless vehicles and drones), navigation, precision agriculture, smart cities and location-based services. Geodesy is actually more important than ever.

    Today, the environment is different. U.S. federal agencies still need geodesists for developing enhanced and refined geodetic models and tools. However, major U.S. companies, such as Google and FedEx, as well as the automobile industry, precision farming companies and mining companies also need more accurate geodetic models, tools and algorithms. Therefore, these companies also need trained geodesists to perform important research on topics that address their specific geodetic requirements.

    Today, OSU’s Geodesy Department is training very few American citizens. As the U.S. moves toward achieving geodetic-grade positioning in real-time in support of new applications such as driverless vehicles and drones, the number of trained geodesists should be increasing, not decreasing [Note: In 1990, there were 92 geodetic science graduate students. In 2019, there were 25; only three were U.S. citizens]. OSU and other universities need to educate and train the next generation of the nation’s scientific workforce of highly skilled research geodetic scientists that will expand industry’s research expertise.

    The shortage of American geodesists poses a significant economic risk for the U.S. Europe and China train many more geodesists than the US. There are very few geodetic science programs in the U.S. today, and education in geodetic proficiencies has been fragmented. The OSU graduate program is one of few surviving geodetic science programs.

    Users of geodetic products and services need to support geodetic departments in universities so that U.S. geodesy programs can grow to meet the geospatial demands of the future. The geospatial component of the economy is worth about $500 billion/year. So why are we allowing its foundational discipline to shrink in this country?

  • Why users will need to perform GNSS occupations as part of a leveling project after 2022

    Why users will need to perform GNSS occupations as part of a leveling project after 2022

    This column will address why users will be required to perform GNSS occupations when submitting a leveling project to the National Geodetic Survey (NGS) after 2022. It will highlight a section of NGS Blueprint for 2022, Part 3, “Working in the Modernized NSRS,” that discusses the process of performing leveling projects after 2022. My October 2017 column briefly discussed NGS’ preliminary plans for incorporating geodetic leveling data into the North American-Pacific Geopotential Datum of 2022 (NAPGD2022) to establish orthometric heights consistent with GNSS-derived NAPGD2022 orthometric heights. It emphasized that after NAPGD2022 is established, the primary means for deriving orthometric heights on monuments will be using GNSS observations combined with the geoid model.

    As a side note, NGS just released NOAA Technical Report NOS NGS 72–GEOID18, a report that provides a comprehensive explanation of the data and methods used to create the latest NGS hybrid geoid model. My February 2020 column provided an analysis of the differences between the latest published hybrid Geoid18 values provided on NGS’ Datasheet and the computed geoid height value using the published NAD 83 (2011) ellipsoid height and NAVD 88 orthometric height.

    In support of the modernization of the National Spatial Reference System (NSRS), NGS has published three documents denoted as Blueprints for 2022 that describe the modernization of the NSRS (see the box titled “NSRS Modernization NGS Blueprint Documents”).

    NSRS Modernization NGS Blueprint Documents

    (https://www.ngs.noaa.gov/datums/newdatums/policy.shtml)

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    There are several sections in NGS Blueprint for 2022, Part 3, “Working in the Modernized NSRS,” that discuss the process of performing leveling projects after 2022. Something that will be new after 2022 is that NGS will require users to perform GNSS occupations in order to incorporate their leveling results into the new modernized NSRS.

    NGS realizes that in the immediate future GNSS will not replace geodetic leveling for determining the most accurate local orthometric height differences. NGS’ plans include preparing a new leveling manual that will explicitly explain how to work in the modernized NSRS. Some of the new surveying procedures are described in Section 2.10 of Blueprint part 3. In section 2.10, NGS states that there will be substantial changes in how they process and serve up survey data, and that there will be some new ways of executing surveys. This column will focus on sections “2.10.2 Leveling” and “2.11.5 Leveling on Passive Marks” that discuss the new procedures for executing leveling surveys in the modernized NSRS. One major change is that leveling surveys will require Global Navigation Satellite System (GNSS) occupations to ensure orthometric heights computed in leveling surveys are up-to-date and are connected to the NSRS through the NOAA CORS Network. After the modernization of the NSRS in 2022, the NOAA CORS Network will be the primary access to the NSRS. This means leveling and classical surveys will require GNSS surveys to be part of the project. NGS’ plans include creating an OPUS option for processing all types of surveys. Users will be able, within OPUS, to adjust their projects using any mix of CORS data and passive control. Saying that, these same projects, on submission, will be deconstructed at NGS and reduced to the raw observations, then adjusted solely to the NOAA CORS Network to determine Final Discrete coordinates every GPS Month. The GPS Month concept may be new to some users. Blueprint Part 3 describes the concept in section “2.11.3 GNSS on Passive Marks.” The basic concept of a GPS Month is that it is four consecutive GPS weeks, with the first week in the GPS month having a GPS week number that is a multiple of four (see box titled “Definition of a GPS Month”).

    Definition of a GPS Month

    GPS month: Four consecutive GPS weeks, with the first week in the GPS month having a GPS week number that is a multiple of 4.

    In this fashion, NGS defines:

    • GPS month 0 = GPS weeks 0, 1, 2, and 3 (1/6/1980 through 2/2/1980)
    • GPS month 1 = GPS weeks 4, 5, 6, and 7 (2/3/1980 through 3/1/1980)
    • GPS month 2 = GPS weeks 8, 9, 10, and 11 (3/2/1980 through 3/29/1980)
    • GPS month 513 = GPS weeks 2052, 2053, 2054, and 2055 (5/5/2019 through 6/1/2019)
    • etc.

    So, what does this really mean to the user when performing a leveling project in 2022? For a leveling project to be processed using NGS software and/or submitted to NGS for inclusion into the NSRS database, the user must follow specific rules.

    The following is from Blueprint, Part 3, section “2.10.2 Leveling:”

    “As GNSS occupations are required for geodetic leveling, the rules for how many and how frequently will be:

    • For a leveling project to be processed using NGS software and/or submitted to NGS for inclusion into the NSRS database, its field observations should not span more than one year. Longer projects should be broken into sub-projects of less than one year.
    • A minimum of three “primary control marks” must be in the level network for every project.
    • More primary control marks should be added so there is never more than a 30-kilometer linear distance between marks in the entire network.
    • Each primary control mark must have the following GNSS occupations (details on using GNSS occupations to work in the NSRS will be found in the update to NGS 58):
      • A minimum of two occupations within +/- 14 days of the beginning of leveling, but also falling within the same GPS month and whose local start times are separated by between 3 and 21 hours.
        • It is preferable, but not required, that all occupations on any primary control mark occur within the same GPS month as those of all other primary control marks.
      • A minimum of two occupations within +/- 14 days of the end of leveling, but also falling within the same GPS month and whose local start times are separated by between 3 and 21 hours.
        • It is preferable, but not required, that all occupations on any primary control mark occur within the same GPS month as those of all other primary control marks.
    • All projects exceeding six months must have a third set of GNSS occupations on all primary control marks some time near the middle of the project, without a rigorous rule as to when. They must follow the “minimum of two occupations” rule as per above, and each mark’s occupation is required to fall in the same GPS month, with a preference that all primary control marks are occupied in the same GPS month.”

    The box titled “GNSS Procedures for Leveling Projects” highlights the GNSS rules that need to be adhered to when performing leveling projects in 2022.

    GNSS procedures for leveling projects

      • For the Immediate Years Following 2022, NGS Will Require That all Leveling Projects Turned in Have GNSS on Primary Control
        • Minimum of 3 Points with a Maximum Spacing of 30 km
        • At Least Two Occupations of Each GNSS Primary Control:
          • +/- 14 days of Beginning of Leveling
            • Within the Same GPS Month
          • +/- 14 days of Ending of Leveling
            • Within the Same GPS Month

    Image: National Geodetic Survey
    Diagram: David B. Zilkoski

    The boxes titled “GNSS + Leveling 2022 Procedures at the Start of the Leveling Project” and “GNSS + Leveling 2022 Procedures at the End of the Leveling Project” provide conceptual diagrams that illustrate what this means to a typical leveling project.

    Image: National Geodetic Survey
    Diagram based on information from Dan Gillins, NGS, and modified by David B. Zilkoski
    Image: National Geodetic Survey
    Diagram based on information from Dan Gillins, NGS, and modified by David B. Zilkoski

    So, why is NGS requiring users to perform GNSS observations in support of leveling project. Leveling is a differential measurement technique; it generates relative height differences not absolute heights. In NGS’ modernized, time-dependent 2022 NSRS, the absolute height will be provided by up-to-date GNSS data; and the accurate relative height differences between leveling marks will be provided by the leveling data. (See box titled “Why NGS Requires GNSS Occupations on Primary Marks.”)

    Why NGS requires GNSS occupations on primary marks

    • The Connection to NAPGD2022 is Obtained Through GNSS and a High-Accuracy Geoid Model
    • Network Accuracy
    • The Accuracy of the Height Differences are Provided Through the Leveling Data
    • Local Accuracy
    • Combining the leveling and GNSS increases the redundancy in a survey network

    NGS is developing models and tools to facilitate the incorporation of leveling survey data and adjustment results into the new modernized NSRS in 2022. Blueprint, Part 3, section “2.13.3 OPUS for Leveling,” describes NGS plans to support leveling surveys through the use of the OPUS web tool. The box titled “OPUS for Leveling” outlines how NGS will modify the OPUS web tool to support leveling surveys.

    OPUS for leveling

    • Support for leveling surveys will follow many of the best aspects of OPUS
      • Uploading and processing digital data files
      • Using a web-based graphical interface
      • Submitting data to NGS
    • Leveling is a differential measurement technique
      • It generates relative height differences not absolute heights
    • For users who need absolute heights in the NSRS
      • OPUS will support a mix of GNSS and leveling in a single project
    • NOTE: NGS will require a GNSS survey to be performed at specific times before and after leveling surveys in order for the data to be submitted for inclusion in the modernized NSRS after 2022.
    • NOTE: Leveling surveys longer than one year must be broken up into multiple projects. Leveling surveys between 6 and 12 months in duration require a third, intermediary GNSS data collection.

    This column highlighted that in the modernized NSRS the only way to get “into the datum” will be through a GNSS survey. It noted that leveling projects generate relative height differences not absolute heights. In NGS’ new modernized, time-dependent NSRS, the absolute height will be provided by up-to-date GNSS data; and the relative height differences between leveling marks will be provided by the leveling data. A major requirement will be that users must collect GNSS data both at the beginning and at the end of a leveling survey project. Leveling survey projects that take longer than one year to complete must be broken up into multiple projects. NGS is developing model and tools to facilitate incorporating all types of survey data into the new NSRS. I would encourage all readers to read NGS’ Blueprint for 2022 documents to obtain a better understanding of the new, modernized NSRS.

  • The differences between published Geoid18 and Geoid12B values in Southern Louisiana

    The differences between published Geoid18 and Geoid12B values in Southern Louisiana

    My February 2020 column provided an analysis of the differences between the latest published hybrid Geoid18 values provided on NGS’ Datasheet and the computed geoid height value using the published NAD 83 (2011) ellipsoid height and NAVD 88 orthometric height. The column highlighted issues on differences due to published heights that have changed since the database pull for Geoid18. It mentioned that future columns will address differences in other portions of CONUS. This column will focus on differences between published Geoid18 values and Geoid12B values in Southern Louisiana. Why are users seeing large differences between the two models?

    My last column mentioned that the technical report on Geoid18 provided a good explanation on the stations used in the United States Gulf Coast region. See box titled “GPS on Bench Marks for GEOID18 in the Gulf Coast Region.”

    GPS on Bench Marks for GEOID18 in the Gulf Coast Region

    (https://www.ngs.noaa.gov/GEOID/GEOID18/geoid18_tech_details.shtml)

    There are areas of complex vertical crustal motion in the Texas/Louisiana Gulf Coast region of the United States which render many control station elevations in the region invalid. The selection of GPS on Bench Marks in this region was limited to the small number of marks where the leveling and GPS data agreed to minimize the influence of crustal motion in the hybrid geoid model. Figure 1 depicts the selection of stations used in the hybrid geoid model along the Texas/Louisiana Gulf Coast. (Image: National Geodetic Survey)
    Figure 1: GEOID18 Gulf Coast selected marks: There are areas of complex vertical crustal motion in the Texas/Louisiana Gulf Coast region of the United States which render many control station elevations in the region invalid. The selection of GPS on Bench Marks in this region was limited to the small number of marks where the leveling and GPS data agreed to minimize the influence of crustal motion in the hybrid geoid model. Figure 1 depicts the selection of stations used in the hybrid geoid model along the Texas/Louisiana Gulf Coast. (Image: National Geodetic Survey)

    As highlighted in the last column, very few stations in Southern Louisiana were used in the creation of the Geoid18 hybrid geoid model. As provided in my last column the box titled “Differences on GPS on Bench Marks in the Gulf Coast Region” depicts the differences between the published Geoid18 value and the computed geoid value using the latest NAD 83 (2011) ellipsoid and NAVD 88 orthometric height.

    Differences on GPS on Bench Marks in the Gulf Coast Region

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The plot indicates that there are many large differences. Many of these differences are to be expected because the Southern Louisiana is an area of known crustal movement. NGS recognizes this and includes the statement below on datasheets for stations published in Southern Louisiana (see box titled “Statement on NGS Datasheet for Stations in Southern Louisiana”).

    Statement on NGS Datasheet for Stations in Southern Louisiana

    This station is in an area of known vertical motion. Due to the variability of land subsidence, uplift, and crustal motion, NGS has, determined the orthometric heights for marks in these suspect subsidence areas should be considered valid only at the epoch date associated with the orthometric height. These heights must always be validated when used as control. All previously superseded orthometric heights are now considered suspect and are available in the superseded section. NGS does not recommend using suspect or superseded heights as control.

    As stated above, Southern Louisiana is an area of crustal movement. There have been many reports that have described the crustal movement in this region. A few examples include “Vulnerability of Louisiana’s coastal wetlands to present-day rates of relative sea-level rise,” “A New Subsidence Map for Coastal Louisiana,” “Spatio-temporal Modeling of Louisiana Land Subsidence Using High-resolution Geo-spatial Data,” “Anthropogenic and geologic influences on subsidence in the vicinity of New Orleans, Louisiana” and “Rates of Vertical Displacement at Bench Marks in the Lower Mississippi Valley and the Northern Gulf Coast.” The figure in the box title “Figure 1 from A New Subsidence Map for Coastal Louisiana,” from a 2017 report, provides an estimate of the subsidence in coastal Louisiana.

    Looking at the figure indicates that there is a significant variation of subsidence occurring in coastal Louisiana. The legend indicates that the subsidence rates range between 0.6 to 1.2 cm/year.

    Figure 1 from A New Subsidence Map for Coastal Louisiana

    (https://www.geosociety.org/gsatoday/groundwork/G337GW/GSATG337GW.pdf)

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Excerpt from Anthropogenic and Geologic Influences on Subsidence in the Vicinity of New Orleans, Louisiana” depicts estimates of crustal movement between 2009 and 2012 in the vicinity of New Orleans. Several of the areas in the plot indicate subsidence rates exceeding -1 cm/year. Once again, the figure shows the local variability of subsidence rates.

    Excerpt from Anthropogenic and Geologic Influences on Subsidence in the Vicinity of New Orleans, Louisiana

    Check out page 5 of this PDF.

    Last year, NGS performed the Multi-Year CORS Solution 2 (MYCS2). This was described in previous columns, which can be viewed here and here. The MYCS2 process generated computed and modeled velocities for CORSs. The box titled “CORS NAD83 (2011) Vu Velocities” is a plot that depicts the velocities in the “upward” component in cm/year for NOAA CORS that are operational and have a computed velocity in Southern Louisiana. So, what does this mean to estimating a hybrid geoid model in Southern Louisiana?

    CORS NAD83 (2011) Vu Velocities

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The plot indicates that the rates vary from -0.1 cm to -0.8 cm. It should be noted that these stations are CORS and they are typically installed on structures that may not capture the entire amount of subsidence at the land surface. The box titled “CORS Position and Velocity for Station GRIS” provides an example of a CORS sheet from NGS CORS website.

    CORS Position and Velocity for Station GRIS

    (https://www.ngs.noaa.gov/cgi-cors/CorsSidebarSelect.prl?site=gris&option=Coordinates14)

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    Now, let’s look at differences between Geoid12B and Geoid18 in Southern Louisiana. The box titled “GPS on Bench Marks Used in Geoid18 and Geoid12B” depicts the stations used in Geoid12 and those used in Geoid 18. As indicated in the plots, there were a lot more stations used in the generation of the Geoid12B model than those used to create the Geoid18 model.

    GPS on Bench Marks Used in Geoid18 and Geoid12B

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    The box titled “Differences between Geoid12B and Geoid18 in Southern Louisiana” provides the values of Geoid12B minus Geoid18 in centimeters on the GPS in Bench Mark stations used in Geoid12B.

    Differences between Geoid12B and Geoid18 in Southern Louisiana

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    As indicated in the plot, there are some large differences between Geoid12B and Geoid18 values; a few differences exceed 15 centimeters. Based on the previous discussion of crustal movement in Southern Louisiana, this probably shouldn’t come as a surprise. The box titled “Differences between Geoid12B and Geoid18 with Vu Velocity Values” depicts the differences in the hybrid geoid models and the NAD83 (2011) CORS Vu rate.

    Differences between Geoid12B and Geoid18 with Vu Velocity Values

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    The box titled “Differences between Geoid12B and Geoid18 in Lafayette, Louisiana” depicts the differences in the two hybrid geoid models and the NAD83 (2011) CORS Vu rate values in the Lafayette, Louisiana, region. This region has some of the largest differences between Geoid12B and Geoid18 values in Southern Louisiana. As indicated in the plot, CORS station TONY has a Vu rate of -0.8 cm/year which is fairly large, and the differences between Geoid12B and Geoid18 values are fairly large at the -10 to -15 cm level. Once again, users should expect differences between the two hybrid geoid models because there has been movement in the area and because different GPS on Bench Mark stations were used in the generation of the hybrid geoid models. In the Lafayette region the two stations used in the generation of Geoid18 were not used in Geoid12B (see stations highlighted in a box).

    Differences between Geoid12B and Geoid18 in Lafayette, Louisiana

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    The box titled “Differences between Geoid12B and Geoid18 in New Orleans, Louisiana” depicts the differences in the hybrid geoid models and the NAD83 (2011) CORS Vu rate values in the New Orleans, Louisiana, region. Two of the same stations that were used in the development of Geoid12B and Geoid18 are highlighted with a box. The difference between the two geoid model values are much less in this region compared with the Lafayette region. The CORS Vu velocities are also less than the CORS station (TONY) value in Lafayette. Saying that, the differences on stations not used in Geoid18 have differences ranging from -4 to -8 cm going southward toward the Gulf of Mexico. Once again, Southern Louisiana is subsiding so these differences are not surprising.

    Differences between Geoid12B and Geoid18 in New Orleans, Louisiana

    Photo: National Geodetic Survey
    Photo: National Geodetic Survey

    This means if someone uses NGS’ OPUS web tool to compute a GNSS-derived orthometric height, the NAVD 88 GNSS-derived orthometric height could be significantly different than the published stations in this region. Some of the difference could be due to the difference between the Geoid12B and Geoid18 published values, and some could be due to crustal movement in Southern Louisiana. Saying that, I mentioned in my last column that NGS performed a large GNSS network project in Southern Louisiana in 2016. The GNSS-derived ellipsoid heights were loaded in NGS’ database in March 2019, but the GNSS-derived orthometric height from the 2016 project are not yet finalized so they have not been loaded into NGS’ database. Once finalized and loaded into the database, the 2016 GNSS-derived orthometric heights should be more consistent with GNSS-derived orthometric heights estimated using the NGS’ OPUS web tool. This column focused on differences between published Geoid18 values and Geoid12B values in Southern Louisiana. It provided reasons why users may see large differences between the two models.

  • The differences between Geoid18 values and NAD 83, NAVD 88 values

    The differences between Geoid18 values and NAD 83, NAVD 88 values

    My last column, December 2019, highlighted the National Geodetic Survey’s (NGS) new Geoid Monitoring Service (GeMS); and, that NGS’ will be publishing a gridded geoid model GEOID2022 that will contain two components: (1) Static Geoid model of 2022 (SGEOID2022) and (2) Dynamic Geoid model of 2022 (DGEOID2022). That’s what going to happen in 2022, but what about today? Since GEOID18 has been officially released for public use, it’s time to look at differences between the Geoid18 published value and estimated geoid values computed using information from NGS’ datasheet. This column will provide an analysis of the differences between the latest published hybrid Geoid18 values provided on NGS’ Datasheet and the computed geoid height value using the published NAD 83 (2011) ellipsoid height and NAVD 88 orthometric height. This is what a user will see if they computed differences using NGS’ datasheets published values. The question will always be asked, why is there a difference between the published Geoid18 value and the computed geoid value. This column will explain some reasons for the differences.

    It’s mostly good news but there are some issues that should be highlighted. This column will highlight issues on differences due to published heights that have changed since the database pull for Geoid18.

    First, it should be noted that NGS’ hybrid geoid models are different than NGS’ experimental gravimetric geoid models. My December 2018 column explains these differences.

    I would like to emphasize that, in my opinion, hybrid geoid models should be denoted as transformation models. Saying that, hybrid geoid models are related to “real” geoid models. Hybrid geoid model GEOID18 was computed based on NGS’ gravimetric geoid model xGeoid19b; therefore, GEOID18 is related to a gravimetric geoid model but its function is to estimate GNSS-derived orthometric heights consistent with NAVD 88 heights. As described in my previous columns, the GPS on Bench Marks (GPSBMs) data provide an estimate of the geoid height ‘N’ by differencing the ellipsoidal height ‘h’ from the orthometric height ‘H’: (N = h – H). These differences are then compared to the gravimetrically-derived geoid model. The box titled “Excerpt from Geoid18 Website Technical Details” provides a summary of the process from NGS Geoid18 web page technical details document.

    The figure in the box titled “GEOID18 Conversion Surface in cm” is the surface that represents the difference between NAVD 88 as a datum and the geopotential (geoid) surface used in the gravimetric geoid. This is the difference between the hybrid geoid and the gravimetric geoid with respect to NAD83 (GEOID18 – xGEOID19B). This surface has three essential components: a bias, a continental tilt, and local warping from the bench marks.

    Excerpt from Geoid18 Website Technical Details

    (https://www.ngs.noaa.gov/GEOID/GEOID18/geoid18_tech_details.shtml)

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    Hybrid Geoid Model Construction
    The residuals obtained in equation 1 are contaminated with a continential tilt and bias that is estimated and removed with a simple two-dimensional planar surface. The bias-free and tilt-free residuals are ultimately used to determine a mathematical model using least squares collocation (LSC) and multiple Gaussian functions to describe the behavior seen at the bench marks. Once the relationship between the points is modeled, the model is used to generate a 1 arcminute regular grid for interpolation purposes. Figure 2 shows the final conversion surface. This surface represents the difference between NAVD 88 as a datum and the geopotential (geoid) surface used in the gravimetric geoid. This is the difference between the hybrid geoid and the gravimetric geoid with respect to NAD83 (GEOID18 – xGEOID19B). This surface has three essential components: a bias, a continental tilt, and local warping from the bench marks.

    GEOID18 Conversion Surface in cm

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Looking at the figure in the box, the bias and tilt between the hybrid geoid model (Geoid18) and the experimental gravimetric geoid model (xGeoid19b) are fairly obvious. It’s the local warping from the bench mark data that may cause some issues to surveyors or, at least at a minimum, raise some concerned by surveyors. The box titled “Plot of the GPS on Bench Marks Involved in Geoid18” provides a plot of the GPS on Bench Marks (GPSBMs) used in the generation of Geoid18. Users can download the list of GPSBMs stations from the NGS Geoid18 website. There were 32,357 stations used to generate the model. This was an increase of approximately 6,800 stations (26%) over the hybrid geoid model Geoid12B.

    Plot of the GPS on Bench Marks Involved in Geoid18

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The boxes titled “Number of GPS on Bench Mark Stations by State” and “Number of GPS on Bench Mark Stations by State in Northeast U.S.” provide the number of data points per state.

    Number of GPS on Bench Mark Stations by State

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Number of GPS on Bench Mark Stations by State in Northeast U.S.

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Table of Number of Data Points per State” provides the number of stations per State in tabular form.

    Table of Number of Data Points per State

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    The box titled “Summary of Overall fit of Geoid18” provides a summary of the fit of residuals of Geoid18 from the NGS GEOID18 technical details document. Looking at the CONUS overall values, the standard deviation is very low 1.27 cm which is a little better than Geoid12B (1.7 cm). It should be noted that there are some large outliers (minimum value of -10.12 cm and maximum value of 8.17 cm).

    Summary of Overall fit of Geoid18

    (https://geodesy.noaa.gov/GEOID/GEOID18/geoid18_tech_details.shtml)

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    For this column, the file of bench marks provided on the NGS Geoid18 web page were combined with the published ellipsoid, orthometric, and Geoid18 heights from NGS’ datasheet. The difference between the published geoid height (Geoid18) and the estimated geoid height [published NAD 83 (2011) ellipsoid height minus NAVD 88 orthometric height] was computed using the following formula:

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    The box titled “Plot of Differences Based on GPS on Bench Marks Used in Geoid18” depicts these differences based on the stations used to generate Geoid18.

    Plot of Differences Based on GPS on Bench Marks Used in Geoid18

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Most of the values depicted on the plot are within the +/- 2 cm which is what you’d expect because the standard deviation of the overall fit is 1.4 cm. One to two centimeters is a very reasonable difference between the modeled and computed values. The question someone may ask is, I thought the model should be good to 1.4 cm so why are there large residual values on the map? There are several reasons why some of these differences are large but each case needs to be investigated to determine why they are large. This column will address one region as an example and provide a method for others to investigate differences in their area of interest.

    The box titled “Plot of GPS on Bench Mark Differences at the ND/MN Border” depicts a very large difference between the modeled geoid model and the estimated geoid height along the ND/MN border. As indicated in the box, the difference exceeds 6 cm.

    Plot of GPS on Bench Mark Differences at the ND/MN Border

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Plot of GPS on Bench Mark Stations in the ND/MN Border Region” depict the bench marks involved in the development of Geoid18. The green circles represent the GPSBMs stations used in the creation of Geoid18 and the red “x” denote the stations that were not used in the creation of the model. As indicated in the plot, there were a lot of GPSBMs stations in the State of Minnesota (11,011).

    Plot of GPS on Bench Mark Stations in the ND/MN Border Region

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Differences on GPS on Bench Marks in ND/MN Border — NOT Used in Model” depict the values of the rejected GPS on BMs stations. These stations were not used to create the hybrid geoid model Geoid18. As the plot indicates there are several large differences. This is not really surprising since these stations were not used in the model.

    Differences on GPS on Bench Marks in ND/MN Border — NOT Used in Model

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    The box titled “Differences on GPS on Bench Marks in ND/MN Border — USED in Model” depict the values of the GPS on BMs stations used to create the Geoid18 model. Some of these differences exceed 8 cm. You would expect these differences to be small since these stations were used to create the model. So, why are there large post-modeled residuals in the Fargo, ND, region of the United States?

    Differences on GPS on Bench Marks in ND/MN Border – USED in Model

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    In August 2019, NGS performed a large leveling network adjustment in the Minnesota. The adjustment was performed after the Geoid18 database pull. The adjustment resulted in a 7- to 9-cm bias between the published height values and the superseded values. The August 2019 Minnesota leveling network adjustment heights were not used in the creation of Geoid18. The post-modeled differences presented in this column were generated using the published NAD 83 (2011) ellipsoid heights and current NAVD 88 orthometric heights from the NGSIDB. It was determined by NGS that the differences in the Fargo region were mostly due to crustal movement. Therefore, since the differences were due to movement, secondary adjustments will need to be performed to feather the 7- to 9-cm differences to maintain consistency between published NAVD 88 heights in the region. The secondary adjustments have not been completed as of the publication of this column so the residuals west of Fargo in North Dakota are small. These values will change after the secondary adjustment is completed and loaded into NGS’ database.

    As an example, I’ve highlighted the station Fargo 0009 (PID DF7623) in the area of Fargo, North Dakota (see box titled “Differences on GPS on Bench Marks Near Fargo, ND”). The difference (-8.3 cm) is between the published Geoid18 value and the computed geoid value using the published ellipsoid height and orthometric height from the NGS’ datasheet. The box titled “Excerpt from Datasheet for Station Fargo 0009 (DF7623)” provides the information from NGS datasheet for station Fargo 0009; the information used in the computations are highlighted in the box. The box titled “Computation of the Difference between the Modeled Geoid Value (Geoid18) and the Computed Geoid Value for Fargo 0009” provides the process used to compute all differences for this column.

    Differences on GPS on Bench Marks Near Fargo, North Dakota

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Excerpt from Datasheet for Station Fargo 0009 (DF7623)

    Data: National Geodetic Survey
    Data: National Geodetic Survey
    Data: National Geodetic Survey
    Data: National Geodetic Survey
    Data: National Geodetic Survey
    Data: National Geodetic Survey

    Computation of the Difference between the Modeled Geoid Value (Geoid18) and the Computed Geoid Value for Fargo 0009
    (Information from NGS Published Datasheet)

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    So, why is this difference so large in this region? A stated above, NGS performed a readjustment in this region and superseded the heights that were used in the creation of the Geoid18 hybrid model. The Geoid18 hybrid model used the previously published orthometric heights, now provided in the superseded section of the NGS datasheet, because that was the current published height at the time of the data pull for the Geoid18 process. Therefore, if we substitute the superseded height from the datasheet into the equation the difference is reduced to 0.1 cm (1 mm). [See the box titled “Computation of the Difference between the modeled geoid value (Geoid18) and the computed geoid value for Fargo 0009 Using the Superseded NAVD 88 Value.”]

    Computation of the Difference between the modeled geoid value (Geoid18) and the computed geoid value for Fargo 0009 Using the Superseded NAVD 88 Value
    (Information from NGS Published Datasheet)

    Data: National Geodetic Survey
    Data: National Geodetic Survey

    This means if someone uses NGS’ OPUS web tool to compute a GNSS-derived orthometric height, the NAVD 88 GNSS-derived orthometric height will be about 8 cm different than the published stations in this region. This should not be an issue if the users follow published NGS Guidelines to estimate the NAVD 88 GNSS-derived orthometric height, and/or uses NGS Beta OPUS-Projects and NGS procedures to estimate the NAVD 88 GNSS-derived orthometric height. These processes will ensure that the height will be consistent with the current published NAVD 88 orthometric heights in the NGS database.

    The technical report on Geoid18 provides a good explanation on the stations used in the United States Gulf Coast region. See box titled “GPS on Bench Marks for GEOID18 in the Gulf Coast Region.”

    GPS on Bench Marks for GEOID18 in the Gulf Coast Region

    (https://www.ngs.noaa.gov/GEOID/GEOID18/geoid18_tech_details.shtml)

    There are areas of complex vertical crustal motion in the Texas/Louisiana Gulf Coast region of the United States which render many control station elevations in the region invalid. The selection of GPS on Bench Marks in this region was limited to the small number of marks where the leveling and GPS data agreed to minimize the influence of crustal motion in the hybrid geoid model. Figure 1 depicts the selection of stations used in the hybrid geoid model along the Texas/Louisiana Gulf Coast.

    Image: National Geodetic Survey
    Figure 1: GEOID18 Gulf Coast selected marks. (Image: National Geodetic Survey)

    As indicated in the box titled “GPS on Bench Marks for GEOID18 in the Gulf Coast Region” very few stations in Southern Louisiana were used in the creation of the hybrid geoid model. The box titled “Differences on GPS on Bench Marks in the Gulf Coast Region” depict the differences between the published Geoid18 value and the computed geoid value using the latest NAD 83 (2011) ellipsoid and NAVD 88 orthometric height. The plot indicates that there are many large differences. This is to be expected because the orthometric heights used in the creation of the hybrid geoid model are all superseded heights. This is because the only published heights in Southern Louisiana are GNSS-derived orthometric heights and leveling-derived orthometric heights were used in the creation of GEOID18.

    Differences on GPS on Bench Marks
    in the Gulf Coast Region

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    Saying that, NGS performed a large GNSS network project in Southern Louisiana in 2016. At the time of the writing of this column, the GNSS-derived orthometric height from the 2016 project were not yet finalized.

    This column provided an analysis of the differences between the latest published hybrid Geoid18 values provided on NGS’ Datasheet and the computed geoid height value using the published NAD 83 (2011) ellipsoid height and NAVD 88 orthometric height. The column highlighted issues on differences due to published heights that have changed since the database pull for Geoid18. Future columns will address differences in other portions of CONUS.

  • How NGS can implement a time-dependent geopotential datum

    How NGS can implement a time-dependent geopotential datum

    The National Geodetic Survey (NGS) has published a technical report that describes options for how NGS can implement a time-dependent geopotential datum and thus a time-dependent geoid model. My last column described the latest version of NGS’ VERTCON model. As mentioned in the column, NGS is developing these models and tools to support the implementation of the North American-Pacific Geopotential Datum of 2022 (NAPGD2022).

    NAPGD2022 is going to be a time-dependent geopotential datum. In other words, the reference geopotential will change over time and therefore the geoid height value will change over time. NAPGD2022 was described in detail in NGS’ publication “Blueprint for 2022, Part 2: Geopotential Coordinates,” and my December 2017 column. Blueprint for 2022, Part 2 states that a gridded geoid model GEOID2022 will be created and it will contain two components:

    1. The first component will be time independent, denoted as the Static Geoid model of 2022 (SGEOID2022).
    2. The second component will be a time-dependent geoid undulation model, encompassing permanent geoid changes greater than or equal to 1 millimeter per year, denoted as Dynamic Geoid model of 2022 (DGEOID2022).

    NGS will publish a GEOID2022 value that will be based on both SGEOID2022 and DGEOID2022. As stated in the document, GEOID2022 will be the official zero-height surface for orthometric heights within NAPGD2022, and thus within the NSRS. The box titled “Excerpt from Blueprint for 2022, Part 2, Figure 10-2” is a diagram that describes the process of creating the regional high resolution gridded GEOID2022 model. I have highlighted the GEOID2022 model and its two components, SGEOID2022 and DGEOID2022.

    Excerpt from Blueprint for 2022, Part 2, Figure 10-2

    Image: National Geodetic Survey
    Image: National Geodetic Survey

    First, it’s important to note the role of the geoid in estimating GNSS-derived orthometric heights. As described in a previous column, GNSS-derived Orthometric Heights are computed using the following formula: orthometric height (H) = ellipsoid height (h) minus geoid height (N). See the box titled “NAPGD2022 GNSS-Derived Orthometric Height.”

    NAPGD2022 GNSS-Derived Orthometric Height

    Source: Slide 9 from Gillins and Fancher presentation titled ‘Leveling after 2022’ presented at the 2017 Geospatial Summit
    Source: Slide 9 from Gillins and Fancher presentation titled “Leveling after 2022” presented at the 2017 Geospatial Summit

    So, what does it take to compute a time-dependent geoid model and what is NGS’ plan to accomplish this project The technical report titled “ A Preliminary Investigation of the NGS’s Geoid Monitoring Service (GeMS)” describes options for how NGS can implement a time-dependent geopotential datum and thus a time-dependent geoid model (See box titled “NGS Publishes Report on GeMS”). The report contains too much information for a single column. This column will highlight some of the sections of the report. The document does contain a lot of technical information and I would encourage everyone to download the document.

    NGS Publishes Report on GeMS

    Screenshot: National Geodetic Survey
    Screenshot: National Geodetic Survey

    The technical report describes the current state of knowledge and outlines next steps required to define a time-dependent geopotential datum for the Nation. NGS created a project called “The Geoid Monitoring Service,” or simply GeMS, to accomplish their long-term goal of establishing a time-dependent geopotential model.

    The report addressed the following five topics:

    1. A foundational introduction to the various types of geophysical phenomena that are causing both size and shape change to the geoid,
    2. Geodetic observing techniques that are presently available to monitor geoid change,
    3. An objective evaluation of NGS’s current ability to incorporate these techniques into a long-term monitoring service like GeMS,
    4. Known barriers to accomplishing such a project, and
    5. Potential observing techniques that might become available in the next 10-20 years, but are not currently mature enough for operational use.

    The document presents a roadmap of options for how NGS could realize a time-dependent geopotential datum, and how NGS can support the dynamic datum into the future with independent validation surveys and datasets.

    The report discusses the available geoid monitoring techniques that NGS has to support modeling the changes in the geoid. There are three existing NGS program areas and associated technical expertise that could be utilized in an operational GeMS:

    1. NGS’s Gravity Program,
    2. the NOAA CORS Network, and
    3. GPS/geodetic leveling campaigns.

    It is noted that individuals these techniques cannot provide 100% of what GeMS requires but combining various programs would be sufficient. The report does a great job of describing these three program areas. The box titled “Summary of Geoid Monitoring Techniques within NGS’ Current Expertise” is Table 3 from the Technical Report. The table list the affordability and accuracy attributes for each of the program areas. NGS’ Gravity Program provides high quality gravity data to internal and external stakeholders. The program provides gravity data required for NGS’s geoid modeling.

    Summary of Geoid Monitoring Techniques within NGS’ Current Expertise

    Source: National Geodetic Survey
    Source: National Geodetic Survey

    The report provides a good overview of the expertise and instrumentation of NGS’ Gravity Program. The table titled “Summary of NGS’ Terrestrial Gravity Instruments” is a compilation of information on historical methods and instrumentation from the technical report.

    Summary of NGS’ Terrestrial Gravity Instruments

    The document highlights something about the United States gravity data that most users don’t think about. That is, gravity values are referenced to a gravity network just like NGS’ published orthometric heights are referenced to the NAVD 88. In the mid-1950s, a coordinated effort was initiated by the International Association of Geodesy (IAG) to make gravimeter ties throughout collaborating parts of the world to support establishment of an International gravity datum.

    It incorporated intercontinental, north-south, calibration lines and long-distance ties established by airplane. The majority of USA relative gravimeter work was done from 1965 – 1967, resulting in the network shown in the box titled “International Gravity Station Net of 1971 (IGSN71) in CONUS.” The report states that the calculations were completed by Urho A. Uotila of The Ohio State University around 1970.

    The gravity network was constrained by a network of ballistic absolute gravimeters. Five of the eight absolute gravimeter sites were in CONUS. It was a world-wide, simultaneous adjustment and published as The International Gravity Standardization Net 1971 (I.G.S.N. 71). A

    s of December 2019, the IGSN71 remains the official international gravity datum. Many of these stations have been destroyed over the decades, in particular those at passenger airport terminals.

    International Gravity Station Net of 1971 (IGSN71) in CONUS

    (Source: Figure 14 from geodesy.noaa.gov)

    Figure 14: IGSN71 Gravity Stations. (Source: National Geodetic Survey)
    Figure 14: IGSN71 Gravity Stations. (Source: National Geodetic Survey)

    In the mid-1970s, NGS was involved in two major readjustment projects, replacement of NAD27 with NAD 83 and the replacement of NGVD 29 with NAVD 88. At the same time, the NGS gravity group were evaluating the gravity data in NGS database and the gravity stations involved in the IGSN71. During the period 1975 and 1979, NGS and NGA (formally DMA) performed relative gravity surveys around CONUS to evaluate the stations.

    A report by Robert Moose titled “The National Geodetic Survey Gravity Network” published by NGS in 1986 documents the results of the surveys. This network is denoted as the National Geodetic Survey Gravity Network (NGSGN) and depicted in the box titled “National Geodetic Survey Gravity Network (NGSGN) in CONUS.” The NGSGN was constrained by 8 absolute gravimeter stations and consisted of 232 stations. Differences between NGSGN values and IGSN71 values were computed to evaluate or detect change in gravity values.

    The box titled “Gravity Differences between NGSGN and IGSN71 Common Stations” depict these differences. The report states “In summary, the gravity differences between NGSGN and IGSN are generally small and many of the larger differences may be due to vertical motion.

    National Geodetic Survey Gravity Network (NGSGN) in CONUS

    (Source: Figure 15 from geodesy.noaa.gov)

    Figure 15: NGSGN Stations. Destroyed stations known as of July 2019. (Source: National Geodetic Survey)
    Figure 15: NGSGN Stations. Destroyed stations known as of July 2019. (Source: National Geodetic Survey)

    Gravity Differences between NGSGN and IGSN71 Common Stations

    (Source: Figure 16 from geodesy.noaa.gov)

    Figure 16: Difference between NGSGN and IGSN71 AG values [mgal] (Source: National Geodetic Survey)
    Figure 16: Difference between NGSGN and IGSN71 AG values [mgal] (Source: National Geodetic Survey)
    The basic rule of thumb for estimating land movement using gravity changes is: 1 meter of change equals 0.3086 mgals (1 cm of change equals 0.003086 mgals). It should be noted that a positive difference in gravity in the figure indicated apparent subsidence. As stated by the 1986 report by Moose, the large difference in Houston-Galveston region is most likely due to subsidence.

    A report documenting the apparent movement in the Houston-Galveston region was published by NGS in 1980. The boxes titled “ Estimate of Subsidence in Houston-Galveston Area During 1963-78 Epoch” and “Estimate of Subsidence in Houston-Galveston Area During 1973-78 Epoch” provide estimates of the movement in the region that include the same epoch of the two gravity networks. These two plots agree with the summary statement in the 1986 report.

    Estimate of Subsidence in Houston-Galveston Area During 1963-78 Epoch

    (Source: Figure 7 from ngs.noaa.gov)

    NOTE: 30 cm approximately equals to 1 foot (Source: National Geodetic Survey)
    NOTE: 30 cm approximately equals to 1 foot (Source: National Geodetic Survey)

    Estimate of Subsidence in Houston-Galveston Area During 1973-78 Epoch

    (Source: Figure 8 from https://www.ngs.noaa.gov/PUBS_LIB/The1978Houston_Galveston_and_Texas_GulfCoast_VerticalControlSurveys_TM_NOS_NGS27.pdf)

    NOTE: 30 cm approximately equals to 1 foot (Source: National Geodetic Survey)
    NOTE: 30 cm approximately equals to 1 foot (Source: National Geodetic Survey)

    What does all this mean to the geoid? Accurate and current gravity data are critical to the development of an accurate geoid model that includes estimating changes in the geoid model over time.

    The technical report on NGS’ Geoid Monitoring Service (GeMS) describes geodetic and geophysical techniques that are currently known to NGS and show promise for GeMS (see the box titled “Summary of Known Geoid Monitoring Techniques that are currently outside of NGS’s Expertise). It should be noted that all of these techniques rely on a non-NGS entity to create a product (such as a model or dataset) that NGS can utilize in their products and services. This is nothing new; NGS leverages partnerships for other products such as the GOCO05S satellite gravity model produced by an ESA consortium led by the Technical University of Munich. This model is used by the NGS geoid team in static geoid modeling.

    Summary of Known Geoid Monitoring Techniques that are currently outside of NGS’s Expertise

    (Source: Table 7 from Technical Report NOS NGS 69)
    (Source: Table 7 from Technical Report NOS NGS 69)

    Continuation of Summary of Known Geoid Monitoring Techniques that are currently outside of NGS’s Expertise

    (Source: Table 7 from Technical Report NOS NGS 69)
    (Source: Table 7 from Technical Report NOS NGS 69)

    As apparent by all of the types of data required to monitor the geoid, NGS has a challenging task to establish a Geoid Monitoring Service. Why is it important to invest resources to monitor the geoid? Analyzes of temporal satellite gravity missions provide changes in gravity values that can be use to create changes in the geoid. The GRACE (Gravity and Climate Experiment) satellite mission was designed to provide the temporal gravity field variations throughout its mission (duration 2002 – 2017). There are analysis centers that produce models using the GRACE data – University of Texas at Austin Center for Space Research (UTCSR), NASA Jet Propulsion Laboratory (JPLEM), and GFZ German Research Center for Geosciences (GFZOP). Release 6 denoted as RL06 is the most current GRACE data from these groups.

    The data can be used to illustrate the magnitudes and resolutions that GRACE models provide to the seculargeoid rates for CONUS and Alaska. The boxes titled “GRACE Trend over CONUS from UTCSR RL06” and “GRACE Trend over Alaska from UTCSR RL06” are plots from Technical Report NOS NGS 69 that show these secular geoid trends from UTCSR-RL06. The plots indicate very small changes in the geoid but they are significant if the goal is to monitor the geoid model to the mm/year level.

    GRACE Trend over CONUS from UTCSR RL06

    Figure 27: GRACE Trend over CONUS from UTCSR RL06 Model [mm/yr] (Source: Figure 27 from Technical Report NOS NGS 69)
    Figure 27: GRACE Trend over CONUS from UTCSR RL06 Model [mm/yr] (Source: Figure 27 from Technical Report NOS NGS 69)

    GRACE Trend over Alaska from UTCSR RL06

    Figure 28: GRACE Trend over Alaska from UTCSR RL06 GRACE Model [mm/yr] (Source: Figure 28 from Technical Report NOS NGS 69)
    Figure 28: GRACE Trend over Alaska from UTCSR RL06 GRACE Model [mm/yr] (Source: Figure 28 from Technical Report NOS NGS 69)
    Another product available from various processing centers are surface mass concentrations (mascons) as observed by the GRACE satellites. Once again, these mascons can be used to generate a secular geoid rate. The boxes titled “Geoid rate over CONUS based on the GSFC mascon model” and “Geoid rate over Alaska from GSFC mascon model” are plots from Technical Report NOS NGS 69 that provide the secular geoid rate based on the NASA GSFC mascon model. Once again, the plots indicate very small changes in the geoid but there is a systematic change to the geoid based on the analysis of the data from the GRACE mission.

    Geoid rate over CONUS based on the GSFC mascon model

    Figure 32 From Technical Report NOS NGS 69: Geoid rate over CONUS based on the GSFC mascon model [mm/yr] (Source: Figure 32 From Technical Report NOS NGS 69)
    Figure 32 From Technical Report NOS NGS 69: Geoid rate over CONUS based on the GSFC mascon model [mm/yr] (Source: Figure 32 From Technical Report NOS NGS 69)

    Geoid rate over Alaska from GSFC mascon model

    Figure 33 From Technical Report NOS NGS 69: Geoid rate over Alaska from GSFC mascon model [mm/yr] (Source: Figure 33 From Technical Report NOS NGS 69)
    Figure 33 From Technical Report NOS NGS 69: Geoid rate over Alaska from GSFC mascon model [mm/yr] (Source: Figure 33 From Technical Report NOS NGS 69)
    The report stated that when considering monitoring the geoid, the greatest change to the geoid from glacial isostatic adjustment (GIA) processes is centered in northern Canada, but there is “still a significant geoid height trend in the Northern Plains, Great Lakes, and Northeast regions of CONUS.”

    It was noted that if GIA processes are not considered, a 1 cm error in the geoid undulation would occur within 18 years. NADGPD2022 orthometric heights are going to be established using a NATRF2022 ellipsoid height and a GEOID2022 geoid height. This is why the geoid needs a time-dependent component.

    This column highlighted NGS new Geoid Monitoring Service (GeMS); and, that NGS’ will be publishing a gridded geoid model GEOID2022 that will contain two components:

    1. The first component will be time independent, denoted as the Static Geoid model of 2022 (SGEOID2022) and
    2. The second component will be a time-dependent geoid undulation model, denoted as Dynamic Geoid model of 2022 (DGEOID2022).

    NGS will publish a GEOID2022 value that will be based on both SGEOID2022 and DGEOID2022. The column provided examples of how GRACE data can be used to illustrate the magnitudes of secular geoid rates for CONUS and Alaska.

  • New developments coming with the NGS 2022 datum change

    New developments coming with the NGS 2022 datum change

    Heraclitus (Photo: NPR.org)
    Heraclitus (Photo: NPR.org)

    A famous quote applies to almost everything in our lives: “There is nothing permanent except change.”

    This well-known saying is generally credited to the Greek philosopher Heraclitus (500 B.C.E.), although many historians and philosophy experts tend to agree the quote is a combination of many topics found in writings by Heraclitus.

    However the quote came to be, it aptly describes the world we live in; especially now with lightspeed advancements in technology. Change is markedly evident in today’s surveying world, and almost no practitioner is exempt from revolutionary enhancements and necessary upgrades to stay current in our profession.

    Change is on the horizon

    Photo: Trimble
    Photo: Trimble

    The upcoming NGS 2022 datum change, triggered by advancements in positional accuracies and measurement techniques, has quietly created a groundswell of questions, concern and curiosity of how and why we are at these crossroads. In my September 2019 Survey Scene article, we discussed the background behind the necessity of the upgrade and moving toward a standardized measurement unit, (the “foot”). (For purposes of this article, let’s put aside any mention of using the meter/metric system; the U.S. went down that road in the late 1970s / early 1980s, yet crashed and burned upon implementation. I agree the meter is a more practical unit of measurement, but we need to leave that talk for another day.)

    This article will be concentrating on the actual coordinate systems and how significant changes are coming for almost everyone performing surveying measurements. Yes, this means all those construction-based users of GNSS receivers and total stations performing pre-, in-progress and post- construction tasks. Our coordinate world will be turning upside down but, in this case, it will be changes for the good.

    Origins of X/Y (otherwise known as Northing/Easting)

    We have another philosopher to credit for the concept of coordinate geometry; he is the French scientist Rene Descartes (1596-1650) who was heavily influenced by Plato.

    While he may be more well known for his famous quote “I think, therefore I am,” Descartes created what is believed to be the first graphical depiction of geometrical expressions and assigning coordinate values to the results; hence the background behind “Cartesian coordinates.” It is this coordinate system that was utilized by late 1800s/early 1900s surveyors who began using this system to create small networks within urban settings, including New York City, Cincinnati and Atlanta.

    As economic expansion continued through the Great Depression and beyond, the need for larger survey networks became more evident. The first state plane coordinate system (SPCS) began in North Carolina in 1933-34 with more states quickly falling in behind them. The main force behind this effort was the U.S. Coastal & Geodetic Survey (now known as National Geodetic Survey), as they utilized many surveyors and engineers that were unemployed due to the Stock Market Crash of 1929 and Great Depression. Technology for the era was limited to theodolites and steel tapes, with most computations being based upon triangulation.

    Enter the Electronic Age of surveying

    "Big Red" Geodimeter 4D (Photo: National Oceanic and Atmospheric Administration)
    “Big Red” Geodimeter 4D (Photo: National Oceanic and Atmospheric Administration)

    Positional and measurement technology remained stagnant until the 1950s and 1960s with the introduction of the electronic distance meter (EDM). Longer measurements could be made with increased accuracy and helped expand our coordinate system capabilities.

    These enhancements also led to faster expansion of a nationwide highway system (championed by President Dwight Eisenhower) by simply surveying more efficiently. It is along these highway corridors that state plane coordinate systems were expanded into remote areas and used to verify fractured SPC systems created through solar and/or astronomical means. While positional values at common monuments were found to have significant differences by today’s standards, most error was distributed throughout the network.

    Because of the work necessary to complete a survey using a SPCS, it was not practical for any non-governmental project to attempt tying into a known system. Fundamental use of coordinate geometry (CoGo) typically utilized a project base point with a low assumed positional value, (i.e. northing of 1,000, easting of 2,000).

    Most surveyors used the same coordinate values for each project and did not have any positional relationship between their projects. While the field portion of the project took a significant amount of time to traverse and collect, the office calculations and manual drafting were also tedious and time-consuming tasks.

    Prior to the introduction of the handheld calculator in the early 1970s, traverse computations were completed manually using sine/cosine/tangent tables, traverse adjustment (i.e. compass, transit and Bowditch rule) and double distance meridian (DMD) methods. Even as the programmable calculator became the computation method of choice, regularly producing survey data in SPCS was still years away.

    Along with the electronic theodolite and the personal computer with computation software, the introduction of the data collector quietly revolutionized the amount of data that could be stored and efficiently plotted for surveys. But even with the increased efficiencies, there was one big drawback to utilizing this electronic data collection with SPCS; most hardware was limited to values and significant figures not acceptable to using large coordinate values. Some tried truncating SPCS values but often found the trouble not worth the effort, not to mention having projects large enough to be affected by grid-to-ground scale factors (another topic for another day).

    Fast forward to the 1980s and the introduction of ultimate surveying black box, the GPS receiver. Positional accuracy through static GPS sessions was now better than ever and allowed surveyors to cover greater distances in shorter time periods. It was the implementation of the GPS receiver (and subsequent reduction in cost of entry for its use) that allowed the surveyor to embrace the state plane coordinate system more than ever. Also addressed with the new technology was the ability for the data collector to handle larger coordinate values with increased significant figures.

    As RTK and subsequent RTN systems have allowed for more efficient use of GNSS technology, the surveying profession has now overwhelmed the existing monument network and exposed the deficiencies of NAD83 and our various SPCS zones nationwide. NGS has done an excellent job for many years refining and adjusting the national datums (both horizontal and vertical) by augmenting the systems with new data and “turning the screws” as deemed necessary to provide a reliable network.

    If it is not broken, why fix it?

    The existing SPCS zones and overall NAD83 system works well but we will need to circle back to the quote in the opening paragraph: “There is nothing permanent except change.”

    Research, not just completed by NGS but many other respected agencies and laboratories worldwide, has shown that our existing datums have significant flaws due to many factors. These factors include, but are not limited to, tectonic plate shifting, previous survey data that doesn’t meet today’s positional and measurement standards, and limitations in terrestrial measurements.

    We are overdue for an upgrade to the national system and design of new policies and procedures has taken time and lots of hard work. NGS has created a new framework that will adapt to the changing needs of a state and/or regional authority.

    But what does this mean for the surveyor, the contractor and anyone else in the geospatial world that uses state plane coordinates for the basis of data?

    Image: National Geodetic Survey (Michael Dennis)
    Image: National Geodetic Survey (Michael Dennis)

    As discussed in the last article, NGS has been busy creating a new framework with a proposed implementation of 2022-2023. While NGS is creating the specifications, policies and procedures for the new system, it will be up to each state to decide if they want to keep their existing SPCS zones, change to a new scheme, and/or request that additional smaller zones be included for consideration. NGS, in keeping with existing policy, will work with each state to update their SPC definitions, but only if the state engages NGS during the setup period. Otherwise, NGS will apply the new datum specification to the existing zone(s).

    What does this mean to the everyday surveyor?

    For an example on how a state can revise their SPCS, let’s use Illinois and its plan to revise current zones. Illinois currently implements a two-zone system (East and West, lengthwise through the state) based upon a transverse Mercator projection.

    For several years, GIS users and other agencies have discussed creating a single-zone system across the entire state for ease of use. Because of the size of the state and availability of RTN coverage to some remote areas, the realization of this new system has been on hold. Also, it is understood the distortion in data accuracy across a system this large would not be suitable for survey-grade applications.

    Forward to 2019 and the NGS datum upgrade along with a substantial effort by several equipment manufacturers to install CORS stations across the state for broader RTN coverage (and the not-too-distant future rollout of 5G cellphone service). RTN coverage for mapping grade data collection is now readily available nearly everywhere in Illinois, so the potential of a single-zone system is now not far-fetched.

    It should be noted that if Illinois decides to convert to a single-zone system, NGS will only recognize that system for future computations and documentation and the two-zone system will be scrapped. It will fall to each practitioner to convert their existing data and projects to the single-zone system if they choose to use it, but it will have some drawbacks due to the distortion of the larger system.

    Image: National Geodetic Survey (Michael Dennis)
    Image: National Geodetic Survey (Michael Dennis)

    Enter the low distortion projection (LDP) system. Like other states, Illinois is discussing a potential LDP system containing 32-34 regions statewide for more accurate coordinate system development. These regions are being studied to concentrate on larger urban centers and areas where growth potential is predicted. Regions such as the Chicago, St. Louis and Peoria metropolitan areas are being highlighted for major LDP system use by not just surveyors but government and GIS analysts.

    Having a coordinate system with less distortion and more accuracy can provide more reliable information for the survey but also provide more value for the residents and businesses. By concentrating the coordinate system on smaller areas through an LDP, surveyors will literally be using a communal network like their old calibrated or localized network systems of days past. The coordinates will still be large but the integrity of the data will be higher due to the reduced distortion of the system projection.

    This system will also virtually eliminate the need to have a grid-to-ground scale factor because of the lack of distortion. So we will now have a large statewide system for mapping and smaller regional systems for accurate survey data going forward; sounds like a good plan, right?

    Making a significant change increases our capabilities

    Not to sound like a broken record, but let’s revisit the quote by Heraclitus one more time: “There is nothing permanent except change.”

    Most people don’t like change, even if it is for the better. Surveyors are notoriously famous for not wanting change. Many surveyors I know would not embrace early GPS not simply due to cost, but more of not understanding how it works. They also didn’t understand how to embrace state plane coordinates and having survey data that will be compatible with their competitors. Most of those surveyors now are using it, but only because the data collectors have become more user friendly.

    But why will this change be harder for most? Depending on where one is and how their state is going to adapt will affect that change. If your state is not changing any zones, they will have a -2 to +4.5-meter coordinate shift depending on where they are located. For states like Illinois and potentially changing from two zones (East and West) to a single zone and dozens of regional LDP systems, it will be a bit harder to translate all your existing survey data to the new systems if necessary.

    There are several potential pitfalls in front of us if we aren’t careful. Here are a couple of scenarios to consider:

    Image: National Geodetic Survey (Michael Dennis)
    Image: National Geodetic Survey (Michael Dennis)
    • Understanding the general change in datum values
    • Converting old data to new system for reuse (additional time consideration)
    • For practitioners working in several LDP regions, emphasize the importance of correct zone
    • Software and equipment firmware updates
    • Older unsupported data collectors
    • Compatibility with current and archived GIS data
    • Conversions of government agency-specific data and benchmark

    Major milestone dates:

    • Establishing a date in which all new survey data will use the new datum
    • Establish a date in which all design projects will utilize the new datum
    • Establish a date when all construction layout will utilize the new datum

    These zone/LDP system changes also will be affected if your state is currently recognizing the U.S. Survey Foot and will be changing to the “foot” per my last article and ongoing NGS discussions. That change will also precipitate additional review and care for compliance of any old data to new systems.

    As creatures of habit, change and adaptation moves us forward

    Here’s the bottom line: We need to make this change in order to efficiently address future mapping needs and positional accuracies. Because of technology and evolution of measuring devices, we now know there are other factors that play into our coordinate systems.

    As the world becomes more reliant on digital data and information, it will be critical that the right geospatial information is tied to it. There is nothing permanent except change, but change can also be for the better.