Category Archives: NASA

Probing our Atmosphere with GPS

Signals Tell about Hurricanes

Artist’s conception of GPS Block II-F satellite in Earth orbit. Courtesy NASA.

Got a GPS somewhere in one of your electronic devices? If you’ve ever hiked, driven a car, used your smartphone, flown in a plane, taken a train, or seen a barge heading down a river, it’s likely the journey included the use of GPS as a direction and location finder. GPS stands for Global Positioning Satellite system and it works by sending signals between satellites in orbit and receiving stations on Earth. Encoded in the signal stream back and forth between the two is the location of both the satellite and receiver, their rates of travel (velocities), and the precise time at each member of the pair. As you move, the unit records your location and time you were there. In this way, a GPS-enabled receiver can help you determine when you’ll arrive at a destination, assist a pilot in knowing where his or her plane is in relation to the ground, train engineers to know their locations, and so on.

A few years ago I wrote and co-produced (with Mark C. Petersen) on a series of short vodcasts (video podcasts) for MIT’s Haystack Observatory about space weather, and how atmospheric scientists use the effects on GPS signals to measure how solar outbursts affect our planet’s magnetosphere and technology. It’s called Space Weather FX, and well worth watching to learn more about this specialized use of GPS.

It turns out that GPS signals can also be affected as they encounter heavy seas during strong storms. In a paper published in the journal Radio Science, a team of researchers have found a way to use GPS signals to measure and map the wind speeds of hurricanes. How does it work?

A GOES East image of Hurricane Sandy as she approaches the East Coast on October 29, 2012. (Photo Credit: NOAA)

Think of the radio waves bouncing from GPS to the surface of Earth or the ocean the same way you would think of light bouncing off a mirror. When a radio wave from a GPS satellite strikes the ocean, about 60 percent of the signal reflects back toward the sky. Unlike a mirror, however, the surface of the ocean is rarely calm and flat. Wind blowing over it generates heaving waves. According to Stephen Katzberg, a scientist at NASA’s Langley Research Center in Hampton, VA and one of the people developing a technique to use GPS to measure atmospheric disturbances during hurricanes, GPS could allow improved wind speed measurements. These could help meteorologists predict the severity of a storm more accurately.

“Imagine you blow on a hot bowl of soup,” Katzberg explained. “The harder you blow, the bigger the “waves” are in the bowl.”

When a GPS signal strikes a wave on the ocean, the rough surface distorts the reflection by scattering the signals in various directions.  “The radio wave bounces off the waves,” said Katzberg.  “As the surface gets rougher, the reflections get more disturbed and that’s what we measure.”

The technique uses measurements taken by GPS receiver chips, similar to those found in smartphones, located inside the Hurricane Hunter aircraft flown during heavy weather events to gauge the characteristics of hurricanes and tropical storms. A computer compares signals coming directly from satellites above with the reflections from the sea below and calculates an approximate wind speed. The accuracy of the calculation is better than 5 meters per second (about 11 miles per hour) in accuracy. The wind speed of a mid-range, Category 3 hurricane, for comparison, is about 55 meters per second (123 miles per hour).

For years, atmospheric researchers have been using dropsondes to measure wind speeds, temperatures, humidity,  atmospheric pressure and other data about storms. These are instrument packages jammed with scientific instruments, which are attached to little parachutes and dropped into storms. They cost about $750.00 each and each Hurricane Hunter mission uses about 20.  They remain the gold standard of storm measurement systems because they can be dropped in and around storms. They’re also more accurate than the GPS method. But, the advantage of the GPS system is that it can run non-stop and provide data over a much larger area around a storm.  The goal is to use the GPS technique in conjunction with dropsondes to provide a constant view of the changing conditions of a strong storm. With more data, scientists can get ever-finer views of large storms, which will contribute to better storm predictions.

This new GPS measurement technique is being tested on planes, but it may also get implemented on a series of small satellites called the Cyclone Global Navigation System, currently in study and due to be launched by NASA possibly in 2016. They will measure reflected GPS satellite signals from low orbit to monitor storm wind speeds from space. It’s also possible, according to Katzberg, that signals from the  DirecTV and Sirius XM Radio satellites could be used in addition to GPS to provide even more storm monitoring. “Those signals are extremely powerful and easy to detect,” said Katzberg. “These satellites cost hundreds of millions or even billions of dollars, but our system only costs a few hundred. We’re taking advantage of the expensive infrastructure that’s already there.”

What I find interesting is that that these kinds of “Earth-facing” studies are exactly the kind of planetary exploration that we’ve also done at other planets using radio science antennas and radio signals to probe atmospheres. It’s just being done with GPS here on Earth, which brings the idea of planetary exploration close to anyone who’s ever used GPS to explore their neighborhood, a new town, or even a new continent.

(Hat tip to the American Geophysical Union for sending me a heads-up about this so I could delve in and write a story about it. Truly fascinating!)

Voyager 1 Gets Ever Farther Away

Creeping Closer to the “Edge” of the Solar System

The two Voyager spacecraft have always occupied a soft spot in my heart because they were the first ones I ever reported on in my days as a science journalist. They opened up our eyes to what actually exists in the outer solar system around the planets Jupiter, Saturn, Uranus, and Neptune. For the first time, those gas and ice giants became recognizable worlds, with moons and rings and unusual weather patterns.

The Voyagers are on one-way trips out of the Solar System.  Voyager 1 is literally pushing the envelope of the Sun’s influence, currently transiting through a region called the “magnetic highway”. To understand that term, think of the Sun as blowing a bubble of gas out to interstellar space. Like any bubble (or a balloon), it has a thin surface. The region inside the bubble is threaded with the Sun’s magnetic field lines.

Artist’s concept of the Voyager 1 spacecraft’s exploration of a region in the outermost par tof the heliosphere (the bubble blown out by the Sun). In this region solar magnetic field lines (yellow arcs) are piling up and intensifying. The depletion region, where voyager is now, could be the last part of our solar system and once it clears that area, the spacecraft will truly be in interstellar space. Image Credit: NASA/JPL-Caltech

Voyager 1 has been slowly exploring the outermost regions of the bubble. In 2004, it  passed a shockwave known as the “termination shock”. This is where solar wind suddenly slows down and becomes more turbulent. In 2010, Voyager then passed into an area called the “stagnation region” where the outward velocity of the solar wind slowed to zero and sporadically reversed direction.

On Aug. 25, 2012, Voyager 1 entered the depletion region, where the magnetic field acts as a kind of magnetic highway that lets energetic ions from inside the heliosphere escape out, and cosmic rays from interstellar space zoom in. (To learn more about how this region acts as a magnetic highway, click here and read more here about today’s Voyager 1 announcement.)

As Voyager 1 zooms out on its endless journey, eventually it will cross the heliopause—the “skin” of the bubble blown out by the Sun. After that, it’s clear sailing to the next flyby of a celestial object, the star Gliese 445.  However, that won’t happen for about 40,000 years.  Chances are that Voyager 1 will be unable to tell us anything about it (provided we’re still around), since its systems are slowly deteriorating, and astronomers will begin shutting down most of its subsystems in the next few years. Still, it will send signals as long as its power holds out, as it transits interstellar space at the fastest speed relative to the Sun of any human-made object sent to space.

If you’ve never read about the Voyager missions to the outer solar system, they provide quite a tale and one well worth knowing. So, check here and here and here  to learn more about these amazing spacecraft and the discoveries they helped planetary scientists make.