Unprecedented melting of Greenland's ice sheet this month has stunned
NASA scientists and has highlighted broader concerns that the region is
losing a remarkable amount of ice overall.
According to a NASA press release,
about half of Greenland's surface ice sheet naturally melts during an
average summer. But the data from three independent satellites this
July, analyzed by NASA and university scientists, showed that in less
than a week, the amount of thawed ice sheet surface skyrocketed from 40
percent to 97 percent.
In over 30 years of observations,
satellites have never measured this amount of melting, which reaches
nearly all of Greenland's surface ice cover.
When Son Nghiem of
NASA's Jet Propulsion Laboratory observed the recent melting phenomenon,
he said in the NASA press release, "This was so extraordinary that at
first I questioned the result: Was this real or was it due to a data
error?"
Scientists at NASA's Goddard Space Flight Center,
University of Georgia-Athens and City University of New York all
confirmed the remarkable ice melt.
NASA's cryosphere program
manager, Tom Wagner, credited the power of satellites for observing the
melt and explained that, although this specific event may be part of a
natural variation, "We have abundant evidence that Greenland is losing
ice, probably because of global warming, and it's significantly
contributing to sea level rise."
Wagner said that ice is clearly
thinning around the periphery, changing Greenland's overall ice mass,
and he believes this is primarily due to warming ocean waters "eating
away at the ice." He cautiously added, "It seems likely that's
correlated with anthropogenic warming."
This specific extreme
melt occurred in large part due to an unusual weather pattern over
Greenland this year, what the NASA press release describes as a series
of "heat domes," or an "unusually strong ridge of warm air."
Notable melting occurred in specific regions of Greenland, such as the area around Summit Station,
located two miles above sea level. Not since 1889 has this kind of
melting occurred, according to ice core analysis described in NASA's
press release.
Goddard glaciologist Lora Koenig said that similar
melting events occur about every 150 years, and this event is
consistent with that schedule, citing the previous 1889 melt. But, she
added, "if we continue to observe melting events like this in upcoming
years, it will be worrisome."
"One of the big questions is 'What's happening in the Arctic in general?'" Wagner said.
Just last week, another unusual event occurred in the region: the calving of an iceberg twice the size of Manhattan from Greenland's Petermann Glacier.
Over the past few months, separate studies have emerged that suggest humans are playing a "dominant role" in ocean warming, and that specific regions of the world, such as the U.S. East Coast, are increasingly vulnerable to sea level rise.
Wagner
explained that in recent years, studies have observed thinning sea ice
and "dramatic" overall changes. He was clear, "We don’t want to lose
sight of the fact that Greenland is losing a tremendous amount of ice
overall."
NASA
CAPTION: Extent of surface melt over Greenland’s ice sheet on July 8
(left) and July 12 (right). Measurements from three satellites showed
that on July 8, about 40 percent of the ice sheet had undergone thawing
at or near the surface. In just a few days, the melting had dramatically
accelerated and an estimated 97 percent of the ice sheet surface had
thawed by July 12. In the image, the areas classified as “probable melt”
(light pink) correspond to those sites where at least one satellite
detected surface melting. The areas classified as “melt” (dark pink)
correspond to sites where two or three satellites detected surface
melting. The satellites are measuring different physical properties at
different scales and are passing over Greenland at different times. As a
whole, they provide a picture of an extreme melt event about which
scientists are very confident. Credit: Nicolo E. DiGirolamo, SSAI/NASA GSFC, and Jesse Allen, NASA Earth Observatory
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