The 200ft (60m) front of the Getz Ice Shelf in Antarctica is scored with cracks where icebergs are likely to break off, or calve, in this 2016 photo.
The first estimate of Antarctic calving has found that since 1997 ice shelves have lost as much ice from calving as from melting.
From Meteorological Tech Int by Elizabeth Baker
New research from NASA on Antarctica – including the first map of iceberg calving – has found double the previous estimates of loss from ice shelves and details how the continent is changing.
The agency has stated that the greatest uncertainty in forecasting global sea level rise is how Antarctica’s ice loss will accelerate as the climate warms.
Two studies published August 10 and led by researchers at NASA’s Jet Propulsion Laboratory in Southern California reveal unexpected new data about how the Antarctic Ice Sheet has been losing mass in recent decades.
One study, published in the journal Nature, maps how iceberg calving – the breaking off ice from a glacier front – has changed the Antarctic coastline over the last 25 years.
The researchers found that the edge of the ice sheet has been shedding icebergs faster than the ice can be replaced.
This unexpected finding doubles previous estimates of ice loss from the Antarctic’s floating ice shelves since 1997, from six trillion to 12 trillion metric tons.
Ice loss from calving has weakened the ice shelves and enabled Antarctic glaciers to flow more rapidly to the ocean, accelerating the rate of global sea level rise.
The other study, published in Earth System Science Data, shows in unprecedented detail how the thinning of Antarctic ice as ocean water melts has spread from the continent’s outward edges into its interior, almost doubling in the western parts of the ice sheet over the past decade.
Combined, the complementary reports give the most complete view yet of how the frozen continent is changing.
Changes in elevation of the Antarctic ice sheet from 1985 to 2021 are shown.
Ice height diminishes (red) as the ice sheet melts by contact with ocean water; it rises (blue) where accumulation exceeds melting. Ice shelves are shown in gray.
The missions that supplied data are listed at bottom. Credit: NASA/JPL-Caltech
Chad Greene, JPL scientist and lead author of the calving study, said, “Antarctica is crumbling at its edges. And when ice shelves dwindle and weaken, the continent’s massive glaciers tend to speed up and increase the rate of global sea level rise.”
Most Antarctic glaciers flow to the ocean, where they end in floating ice shelves up to two miles (3km) thick and 500 miles (800km) across.
Ice shelves act like buttresses to glaciers, keeping the ice from simply sliding into the ocean.
When ice shelves are stable, they have a natural cycle of calving and replenishment that keeps their size fairly constant over the long term.
However, in recent decades, the warming ocean has been reportedly destabilizing Antarctica’s ice shelves by melting them from below, making them thinner and weaker.
Satellite altimeters measure the thinning process by recording the changing height of the ice, but NASA has pointed out that until this study, there hasn’t been a comprehensive assessment of how climate change might be affecting calving around the continent.
This is partly because satellite imagery has been challenging to interpret.
Greene continued, “For example, you can imagine looking at a satellite image and trying to figure out the difference between a white iceberg, white ice shelf, white sea ice, and even a white cloud.
That’s always been a difficult task.
But we now have enough data from multiple satellite sensors to see a clear picture of how Antarctica’s coastline has evolved in recent years.”
For the new study, Greene and his co-authors synthesized satellite imagery of the continent in visible, thermal infrared (heat), and radar wavelengths since 1997.
Combining these measurements with an understanding of ice flow gained from an ongoing NASA glacier-mapping project, they charted the edges of ice shelves around 30,000 linear miles (50,000km) of the Antarctic coastline.
Losses from calving have outpaced natural ice-shelf growth so greatly that the researchers think it’s unlikely Antarctica can grow back to its pre-2000 extent by the end of this century.
In fact, the findings suggest that greater losses can be expected: Antarctica’s largest ice shelves all appear to be headed for major calving events in the next 10 to 20 years.
In the complementary study, JPL scientists have combined almost three billion data points from seven spaceborne altimetry instruments to produce the longest continuous data set on the changing height of the ice sheet – an indicator of ice loss – from as early as 1985.
They used radar and laser measurements of ice elevation, accurate to within centimeters, to produce the highest-resolution monthly maps of change ever made of ice loss.
The unparalleled detail in the new record reveals how long-term trends and annual weather patterns affect the ice.
It even shows the rise and fall of the ice sheet as subglacial lakes regularly fill and empty miles below the surface.
JPL’s Johan Nilsson, the lead author of the study, said, “Subtle changes like these, in combination with an improved understanding of long-term trends from this data set, will help researchers understand the processes that influence ice loss, leading to improved future estimates of sea level rise.”
Synthesizing and analyzing the massive archives of measurements into a single, high-resolution data set took years of work and thousands of hours of computing time on NASA’s servers.
Nilsson said, “Condensing the data into something more widely useful may bring us closer to the big breakthroughs we need to better understand our planet and to help prepare us for the future impacts of climate change.”
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