Next month, NASA will launch into space the most advanced laser instrument of its kind, beginning a mission to measure – in unprecedented detail – changes in the heights of Earth’s polar ice.
NASA’s Ice, Cloud and land Elevation Satellite-2 (ICESat-2) will measure the average annual elevation change of land ice covering Greenland and Antarctica to within the width of a pencil, capturing 60,000 measurements every second.
“The new observational technologies of ICESat-2 – a top recommendation of the scientific community in NASA’s first Earth science decadal survey – will advance our knowledge of how the ice sheets of Greenland and Antarctica contribute to sea level rise,” said Michael Freilich, director of the Earth Science Division in NASA’s Science Mission Directorate.
ICESat-2 will extend and improve upon NASA’s 15-year record of monitoring the change in polar ice heights, which started in 2003 with the first ICESat mission and continued in 2009 with NASA’s Operation IceBridge, an airborne research campaign that kept track of the accelerating rate of change.
A Technological Leap
ICESat-2 represents a major technological leap in our ability to measure changes in ice height. Its Advanced Topographic Laser Altimeter System (ATLAS) measures height by timing how long it takes individual light photons to travel from the spacecraft to Earth and back.
“ATLAS required us to develop new technologies to get the measurements needed by scientists to advance the research,” said Doug McLennan, ICESat-2 project manager at NASA’s Goddard Space Flight Center. “That meant we had to engineer a satellite instrument that not only will collect incredibly precise data, but also will collect more than 250 times as many height measurements as its predecessor.”
ATLAS will fire 10,000 times each second, sending hundreds of trillions of photons to the ground in six beams of green light. The roundtrip of individual laser photons from ICESat-2 to Earth’s surface and back is timed to the billionth of a second to precisely measure elevation.
With so many photons returning from multiple beams, ICESat-2 will get a much more detailed view of the ice surface than its predecessor, ICESat. In fact, if the two satellites were flown over a football field, ICESat would take only two measurements – one in each end zone – whereas ICESat-2 would collect 130 measurements between each end zone.
As it circles Earth from pole to pole, ICESat-2 will measure ice heights along the same path in the polar regions four times a year, providing seasonal and annual monitoring of ice elevation changes.
Tracking Ice Melt
Hundreds of billions of tons of land ice melt or flow into the oceans annually, contributing to sea level rise worldwide. In recent years, contributions of melt from the ice sheets of Greenland and Antarctica alone have raised global sea level by more than a millimeter a year, accounting for approximately one-third of observed sea level rise, and the rate is increasing.
ICESat-2 data documenting the ongoing height change of ice sheets will help researchers narrow the range of uncertainty in forecasts of future sea level rise and connect those changes to climate drivers.
ICESat-2 also will make the most precise polar-wide measurements to date of sea ice freeboard, which is the height of sea ice above the adjacent sea surface. This measurement is used to determine the thickness and volume of sea ice. Satellites routinely measure the area covered by sea ice and have observed an Arctic sea ice area decline of about 40 percent since 1980, but precise, region-wide sea ice thickness measurements will improve our understanding of the drivers of sea ice retreat and loss.
Although floating sea ice doesn’t change sea level when it melts, its loss has different consequences. The bright Arctic ice cap reflects the Sun’s heat back into space. When that ice melts away, the dark water below absorbs that heat. This alters wind and ocean circulation patterns, potentially affecting Earth’s global weather and climate.
Beyond the poles, ICESat-2 will measure the height of ocean and land surfaces, including forests. ATLAS is designed to measure both the tops of trees and the ground below, which – combined with existing datasets on forest extent – will help researchers estimate the amount of carbon stored in the world’s forests. Researchers also will investigate the height data collected on ocean waves, reservoir levels, and urban areas.
Potential data users have been working with ICESat-2 scientists to connect the mission science to societal needs. For example, ICESat-2 measurements of snow and river heights could help local governments plan for floods and droughts. Forest height maps, showing tree density and structure, could improve computer models that firefighters use to forecast wildfire behavior. Sea ice thickness measurements could be integrated into forecasts the U.S. Navy issues for navigation and sea ice conditions.
“Because ICESat-2 will provide measurements of unprecedented precision with global coverage, it will yield not only new insight into the polar regions, but also unanticipated findings across the globe,” said Thorsten Markus, an ICESat-2 project scientist at Goddard. “The capacity and opportunity for true exploration is immense.”
Altering the angles yaw, pitch, and roll “Attitude” at which the satellite orients the Earth obviously requires far less energy than adjusting the altitude of the satellite. The laser must shoot straight down otherwise useless data. They are constantly adjusting the aim of the laser to control for this. The laser is small.
The satellite is over a ton, but far above the Earth. It must stay at a controlled ALTITUDE for several years. Fuel must be burned to control the Altitude, not the Attitude.
Twist your little finger, and then run around the block. Which required a larger effort?
read it again. harder this time.
Just one more comment my friend, They have an extremely sophisticated system of Inertial Guidance Gyros on this satellite, which is already in orbit. What are there for? To keep the laser pointed Plumb which means straight down, O.7 ArcSeconds apparently. Innovative system of Gyros, four of them oriented towards the four joints of a Tetrahedron, very innovative.
Read, and Understand….
still not good enough to match the claims according to nitpickers post above.
“King 2017: ”ICESat-2’s attitude determination requirement is more stringent at 3.7 micro radians or 0.76 arc seconds in attitude determination knowledge [2],[8].” That’d be around seven centimetres of error.”
Michael Moon,
But Steven and Chris have not addressed the question of how, when the satellite makes a repeat pass over an area of Greenland or Antarctica that has experienced melting (i.e. a loss of mass) NASA will be able to tell how much the satellite increases its altitude because of a decrease in gravity. If they try to model the gravity, they will get a value that is too low because the estimate of the amount of ice lost will be too high. So, I have to conclude that they either don’t have the answer, or don’t understand the problem — or both.
its in the atbd.
What’s the point of having that most amazing technology to measure ice and climate and stuff, when the data will be processed in the hands of the likes of Josh Willis? (Wizard who magically changes cooling into warming.) Depressingly pointless.
data is open
go get level 0 files.
Actually, thee timing accuracy has to be closer to ,02 billionths of a second. Light travels approximately 1 foot per nanosecond (billionth of a second). If you only measure within a nanosecond, you only have 30 cm accuracy. They’re looking for about half a centimeter or so — “width of a pencil”.