GPS World

Tag: Southwest

  • U.S. Air Force jamming GPS in Southwest sky this week and next

    The U.S. Air Force is intermittently jamming its own GPS signals over southern Nevada and Utah this week and next as part of a massive air-to-air combat training exercise, Red Flag 18-1, based out of Nellis Air Force Base in Nevada. The jamming aims to challenge aircrews and their weaponry under realistic fighting conditions. The Air Force has warned that navigation systems including those found in commercial flights may be disrupted or jammed completely across the southwest U.S. during that time, ending February 16. So far no major commercial airline disruptions, flight delays or re-routings have been reported.

    The U.S. military, heavily and perhaps overly reliant on GPS, is developing a range of position, navigation, and timing (PNT) technologies being to help overcome the loss of GPS during combat, an increasingly likely scenario now and in years to come. Some have speculated that this year’s exercise specifically has in mind a possible conflict on the Korean Penisula. GPS jamming has regularly emanated from North Korea over the past several years.

    “We’re trying a few new and different things with Red Flag 18-1,” said Col Michael Mathes, 414th Combat Training Squadron commander. “This primarily is a strike package focused training venue that we integrate at a command and control level in support of joint task force operations. It’s a lot of words to say that we integrate every capability we can into strike operations that are flown out of Nellis Air Force Base.”

    The exercise, which the Air Force conducts annually, typically involves a variety of attack, fighter and bomber aircraft with added participation from the U.S. Navy, U.S. Army, Marine Corps, Royal Australian Air Force and Royal Air Force. This year’s Red Flag is the largest in the exercise’s 42 year history.

    Nellis Air Force Base in southern Nevada. (Image: USAF)
    Nellis Air Force Base in southern Nevada. (Image: USAF)

    Affected Areas. “Arrivals and departures from airports within the Las Vegas area may be issued non-Rnav re-routes with the possibility of increased traffic disruption near LAS requiring airborne re-routes to the south and east of the affected area,” stated an Air Force bulletin. “Aircraft operating in Los Angeles (ZLA) center airspace may experience navigational disruption, including suspension of Descend-via and Climb-via procedures. Non-Rnav SIDs and STARs may be issued within ZLA airspace in the event of increased navigational disruption. Crews should expect the possibility of airborne mile-in-trail and departure mile-in-trail traffic management initiatives.”

    Alternate Capabilities. Many Air Force planes have onboard inertial navigation systems, using accelerometers, gyroscopes, and magnetic sensors to continuously calculate position without GPS signal data, as well as at a higher hertz rate. When available, GPS signals can be used to correct inertial calculations, which tend to drift over time. Fighter planes can also use AESA-scanned array radars teamed with an inertial system for navigation over short ranges. Aircraft electro-optical and infrared sensors can also read terrain over short distances to provide additional navigation.

    If strike aircraft have reliable communications or datalinks, other aircraft such as E-8 JSTARS, flying outside the GPS-disrupted zone, may be able to relay position and targeting information. Some missiles carried by strike aircraft have laser-guiding instead of or in addition to GPS-guiding.

     

  • On the Edge: Southwest Shakes

    By Tracy Cozzens

    Using a large network of GPS stations, a team of researchers has found that the Rio Valley Rift in the Southwest United States — previously suspected to be dead — is slowly expanding, at a rate of about 0.1 millimeter per year.

    The Rio Grande Rift extends from Colorado’s central Rocky Mountains to Mexico.

    The study was conducted by scientists at the Cooperative Institute for Research in the Environmental Sciences (CIRES) at the University of Colorado at Boulder, in collaboration with the University of New Mexico, New Mexico Tech, Utah State University, and UNAVCO.

    “We don’t expect to see a lot of earthquakes, or big ones, but we will have some earthquakes,” said study author Anne Sheehan, CIRES Fellow and associate director of CIRES Solid Earth Sciences Division. “We use continuous measurements of GPS sites from across the Rio Grande Rift, Great Plains, and Colorado Plateau to estimate present-day surface velocities and strain rates,” Sheehan said.

    Using GPS instruments at 25 sites in Colorado and New Mexico, the team tracked the rift’s miniscule movements from 2006 to 2011. The team found an average strain rate of 1.2 nanostrain each year across the experimental area. A nanostrain is a change in length of one part per billion, thus 1.2 nanostrain per year is equivalent to 1.2 millimeter per year extension over a 1000-kilometer length.“If you picked two points in New Mexico, and one of them lies 100 kilometers to the west of the other, then they would be moving apart at a rate of 0.1 millimeter per year,” explained researcher Henry Berglund.

    Researchers used data from 25 continuous GPS stations installed as part of the EarthScope Rio Grande Rift GPS experiment, supplemented by data from other GPS monuments in the southwestern U.S., resulting in a data set of daily position estimates of 284 GPS monuments for the years 2006 through 2010. Credit: Tracy Cozzens
    Researchers used data from 25 continuous GPS stations installed as part of the EarthScope Rio Grande Rift GPS experiment, supplemented by data from other GPS monuments in the southwestern U.S., resulting in a data set of daily position estimates of 284 GPS monuments for the years 2006 through 2010.

    “It is lower than we thought but it does exist,” Sheehan said. “Some people thought it was zero but we are seeing things are extending slowly.”

    The slow rates of motion made previous attempts to determine tectonic activity difficult. Previously, geologists had estimated the rift had spread apart by up to 5 millimeters each year but the errors introduced by the measuring instrumentations were significant. “The GPS has reduced the uncertainty dramatically,” Sheehan said. “This is the most comprehensive and accurate set of geodetic measurements in this area to date.”

    The extensional deformation is not concentrated in a narrow zone centered on the Rio Grande Rift. Instead, it is distributed broadly from the western edge of the Colorado Plateau into the western Great Plains — a span of more than 370 miles. “This unexpected pattern of broadly distributed deformation at the surface has important implications for our understanding of how low strain-rate deformation within continental interiors is accommodated,” Sheehan said. “Questions we wanted to answer are: how is the Rio Grande Rift deforming? Is it alive or dead? Is it opening or not?”

    Along the rift, spreading motion in the crust has caused magma to rise to the surface, creating long basins susceptible to earthquakes. “The rift is still active,” Sheehan said.

    The team plans to continue monitoring the Rio Grande Rift, and may attempt to determine vertical as well as horizontal activity to determine whether the Rocky Mountains are still uplifting.

    University of Colorado (Boulder) student Henry Berglund services GPS site RG20 west of Silverton, Colorado. Credit: Tracy Cozzens
    University of Colorado (Boulder) student Henry Berglund services GPS site RG20 west of Silverton, Colorado.

    The study’s findings shed light on how continents deform away from plate boundaries, Sheehan said. At plate boundaries scientists can clearly see what is going on. “Things move past each other and crash into each other. At active plate boundaries, the rates of motion detected by GPS can be centimeters per year. Compare that with the fraction of a millimeter per year that we have measured for the Rio Grande Rift.”

    “Present day measurements of deformation within continental interiors have been difficult to capture due to the typically slow rates of deformation within them,” Berglund said. “Now, with the recent advances in space geodesy, we are finding some very surprising results in these previously unresolved areas.”

    The National Science Foundation funded the study. EarthScope and UNAVCO provided instruments, equipment, and engineering services. Results of the study were published in the January 2012 issue of Geology magazine.

    GPS monuments in the vicinity of the Rio Grande Rift and southern Rocky Mountains. The study included construction of 25 GPS monuments (blue circles) in Colorado and New Mexico in 2006 and 2007. Regional EarthScope Plate Boundary Observatory and Continuously Operating Reference Station monuments are shown by gray triangles. Credit: Tracy Cozzens
    GPS monuments in the vicinity of the Rio Grande Rift and southern Rocky Mountains. The study included construction of 25 GPS monuments (blue circles) in Colorado and New Mexico in 2006 and 2007. Regional EarthScope Plate Boundary Observatory and Continuously Operating Reference Station monuments are shown by gray triangles.