Friday, 1 May 2020

Satellites show melting ice sheets in Antarctica and Greenland have contributed to 14 mm sea level rise in 16 years

Extract from ABC News



By Zoe Kean
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A wider section of chasm 1 on the Brunt Ice Shelf in Antarctica
Loss of ice from the margins of Antarctica outweighs the gains in the interior of the continent.(Supplied: British Antarctic Survey)
NASA satellites bearing advanced laser technology have recorded the most accurate picture of large scale ice sheet melting in Greenland and Antarctica to date.
Melting ice sheets in Greenland and Antarctica contributed to 14 millimetres of sea level rise between 2003 and 2019, according to a study published today in the journal Science.
"[Into the future] with that 14 millimetres happening every 16 years, it adds up to a pretty significant amount of sea level rise", said lead author Benjamin Smith of the University of Washington.
If all the melt observed in this study was to flood an area the size of Australia, we would all be wading through 66 centimetres of water, Professor Smith calculated.
Two satellites, the ICESat-1 and the more advanced ICESat-2, were equipped with "laser altimeters" that bounced light pulses off the ice sheets to determine their height.
Researchers compared measurements taken in the early 2000s by ICESat-1 with measurements taken in 2018 and 2019 by ICESat-2.
"The two sets of measurements intersect each other at millions of points, it's those intersections that let us map how the ice changed between ICESat-1 and ICESat-2," Professor Smith said.
"This is a much more significant climatic signal than what you might see if you just surveyed for two or three years," Professor Smith said.

Greenland vs Antarctica

Previous satellite data from NASA shows the rate of global mean sea level rise is accelerating by an average of 3.4 millimetres per year.
Melting ice from Greenland and Antarctica contributes to about a third of the sea level rise we're seeing, Professor Smith said.

Greenland's ice sheet lost an average of 200 gigatons of ice a year, contributing up to two thirds of the sea level rise.
The majority of this ice loss was from thinning of coastal glaciers, which have been impacted by warmer summer temperatures melting the ice on the surface, and warmer ocean temperatures eroding the edges of the ice.
The satellite data showed Antarctica lost an average of 118 gigatons of ice in the same time frame.
While there are gains in ice coverage in the interior, due to increased snowfall, these did not outweigh the losses in coastal areas.
"The total amount of thinning vastly outweighs the small amount of thickening in the interior of the ice sheets," Professor Smith said.
Satellite image of Antarctic ice sheet loss
Satellite data shows the amount of ice gained (blue) or lost (red and purple) by Antarctica between 2003 and 2019(Supplied: Smith et al/Science)
The majority of Antarctica's contribution to sea level rise comes from its glaciers flowing into the ocean as warmer water erodes the ice.
This process is far more rapid in West Antarctica than in East Antarctica where it is quite patchy, with areas of thickening and thinning.

Measuring ice shelf losses

Glaciologist Matt King said a strength of this research is that it observed both ice on the land and ice floating on the sea, whereas previous studies focused on just one or the other.
"We know that ice on land responds to ice on the sea, so looking at the ice sheet as a whole is an advance," said Professor King of the University of Tasmania.
Study co-author Helen Amanda Fricker of the University of California said sea ice has previously been excluded because melting ice on land directly contributes to sea level rises, whereas sea ice melt does not.
But, she said, scientists need to know how ice sheets are changing if we are going to be able to predict how grounded ice might leave the Antarctic continent.
"Knowing this won't slow it down, but it will help us make informed decisions."Illustration of an ice shelf
The anatomy of an ice shelf.(Supplied: Dr Sue Cook)
"We have discovered that where grounded ice changes most is where the ice shelves are thinning," said Professor Fricker
While ice shelves, which float on the ocean, don't contribute to sea level rise, they act like a barrier, anchoring glaciers on the Antarctic landmass.

Research needed where Australia is based

Professor Fricker is calling for more on-the-ground research in East Antarctica, where Australia's research bases are located.
"Key systems are changing in East Antarctica, it's in Australia's backyard," she said.
Professor King agreed.
"Satellite studies provide a great continental view, but we also need good field measurements to understand what's going on in these vulnerable places," said Professor King.
"We don't really know enough about East Antarctica to understand the changes going on," he said.
"So we are left with a general state of confusion, flying blind from both directions."
The latest data showed melting was more extreme in Greenland than in Antarctica.

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