NASA Data Sheds New Light on Changing Greenland Ice
Research using NASA data is giving new insight into one of the processes
causing Greenland's ice sheet to lose mass. A team of scientists used satellite
observations and ice thickness measurements gathered by NASA's Operation
IceBridge to calculate the rate at which ice flows through Greenland's glaciers
into the ocean. The findings of this research give a clearer picture of how
glacier flow affects the Greenland Ice Sheet and shows that this dynamic process
is dominated by a small number of glaciers.
Over the past few years, Operation IceBridge measured the thickness of many
of Greenland's glaciers, which allowed researchers to make a more accurate
calculation of ice discharge rates. In a new study published in the journal
Geophysical Research Letters, researchers calculated ice discharge
rates for 178 Greenland glaciers more than one kilometer (0.62 miles) wide.
Ice sheets grow when snow accumulates and is compacted into ice. They lose
mass when ice and snow at the surface melts and runs off and when glaciers at
the coast discharge ice into the ocean. The difference between yearly snowfall
on an ice sheet and the sum of melting and discharge is called a mass budget.
When these factors are equal, the mass budget is balanced, but for years the
Greenland Ice Sheet has had a negative mass budget, meaning the ice sheet is
losing mass overall.
For years the processes of surface melt and glacier discharge were roughly
equal in size, but around 2006 surface melt increased and now exceeds iceberg
production. In recent years, computer model projections have shown an increasing
dominance of surface melt, but a limited amount of glacier thickness data made
pinpointing a figure for ice discharge difficult.
Ice discharge is controlled by three major factors: ice thickness, glacier
valley shape and ice velocity. Researchers used data from IceBridge's
ice-penetrating radar – the Multichannel Coherent Radar Depth Sounder, or
MCoRDS, which is operated by the Center for Remote Sensing of Ice Sheets at the
University of Kansas, Lawrence, Kan. – to determine ice thickness and
sub-glacial terrain, and images from satellite sources such as Landsat and Terra
to calculate velocity. The team used several years of observations to ensure
accuracy. "Glacier discharge may vary considerably between years," said Ellyn
Enderlin, glaciologist at the University of Maine, Orono, Maine and the study's
lead author. "Annual changes in speed and thickness must be taken into
account."
Being able to study Greenland in such a large and detailed scale is one of
IceBridge's strengths. "IceBridge has collected so much data on elevation and
thickness that we can now do analysis down to the individual glacier level and
do it for the entire ice sheet," said Michael Studinger, IceBridge project
scientist at NASA's Goddard Space Flight Center in Greenbelt, Md. "We can now
quantify contributions from the different processes that contribute to ice
loss."
With data on glacier size, shape and speed, researchers could calculate each
glacier's contribution to Greenland's mass loss and the total volume of ice
being discharged from the Greenland Ice Sheet. Of the 178 glaciers studied, 15
accounted for more than three-quarters of ice discharged since 2000, and four
accounted for roughly half. Considering the large size of some of Greenland's
glacier basins, such as the areas drained by the Jakobshavn, Helheim and
Kangerdlugssuaq glaciers, this was not exactly surprising.
What they also found was that the size of these basins did not necessarily
correlate with glacier discharge rate, shuffling the order of Greenland's
largest glaciers. Previously Helheim Glacier was thought to be Greenland's third
largest glacier, but this study puts it in fifth place and adds two southeast
Greenland glaciers, Koge Bugt and Ikertivaq South to the list of big
ice-movers.
Glacier thickness measurements and this study's calculation methods have the
potential to improve future computer model projections of the Greenland Ice
Sheet. And with a new picture of which glaciers contribute most to mass loss,
IceBridge will be able to more effectively target areas in future campaigns,
promising more and better data to add to the research community's body of
knowledge.

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