These new maps show 16 years of ice sheet loss

Using satellite data, scientists have made precise, detailed maps of how the Greenland and Antarctic ice sheets have changed over 16 years. How the maps were made, and what they tell us.

A new study, published April 30, 2020, in Science, used an advanced Earth-observing laser instrument aboard a satellite to make precise, detailed measurements of how the elevation of the Greenland and Antarctic ice sheets have changed between 2003 and 2019.

The study results show that small gains of ice in East Antarctica are dwarfed by massive losses in West Antarctica. According to the scientists, the net loss of ice from Antarctica, along with Greenland’s shrinking ice sheet, has been responsible for 0.55 inches (14 millimeters) of sea level rise between 2003 and 2019 – slightly less than a third of the total amount of sea level rise observed in the world’s oceans.

The findings compared the recent data from NASA’s Ice, Cloud and land Elevation Satellite 2 (ICESat-2), launched in 2018, with measurements taken by the original ICESat from 2003 to 2009.

Aerial view of ice-covered mountainous landscape, glacier, ice-covered sea.

Using data from the ICESat and ICESat-2 laser altimeters, scientists precisely measured how much ice has been lost from ice sheets in Antarctica and Greenland between 2003 and 2019. The Antarctic Peninsula, seen here, was one of the fastest changing regions of the continent. Image via NASA/ K. Ramsayer.

The study found that Greenland’s ice sheet lost an average of 200 gigatons of ice per year, and Antarctica’s ice sheet lost an average of 118 gigatons of ice per year.

How much ice is that? One gigaton of ice is enough to fill 400,000 Olympic-sized swimming pools or cover New York’s Central Park in ice more than 1,000 feet (300 meters) thick, reaching higher than the Chrysler Building.

The new data comes from what NASA describes as its most advanced Earth-observing laser instrument ever flown in space:

ICESat-2’s instrument is a laser altimeter, which sends 10,000 pulses of light a second down to Earth’s surface, and times how long it takes to return to the satellite – to within a billionth of a second. The instrument’s pulse rate allows for a dense map of measurement over the ice sheet; its high precision allows scientists to determine how much an ice sheet changes over a year to within an inch.

The researchers took tracks of earlier ICESat measurements and overlaid the tracks of ICESat-2 measurements from 2019, and took data from the tens of millions of sites where the two data sets intersected. That gave them the elevation change, but to get to how much ice has been lost, the researchers developed a new model to convert volume change to mass change. The model calculated densities across the ice sheets to allow the total mass loss to be calculated.

False-color satellite view of Greenland with red rim around it showing ice loss on coasts.

Greenland. Image via NASA.

Ben Smith is a glaciologist at the University of Washington and lead author of the new paper. Smith said in a statement:

If you watch a glacier or ice sheet for a month, or a year, you’re not going to learn much about what the climate is doing to it. We now have a 16-year span between ICESat and ICESat-2 and can be much more confident that the changes we’re seeing in the ice have to do with the long-term changes in the climate.

Bottom line: New maps made using satellite data show 16 years of ice sheet loss on Antarctic and Greenland.

Source: Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes

Via NASA

Eleanor Imster