Tuesday, December 19, 2023

Loss of ice on the Antarctic glacier has accelerated rapidly as a result of ocean warming

   Antarctic Glacier Collapse: Unprecedented Ice Loss and Acceleration

Several Antarctic glaciers, including the severely damaged Hektoria Glacier, are experiencing unprecedented acceleration and ice loss, with Hektoria losing 25 kilometers of ice from its front in just 16 months. The dramatic retreat, caused by warm ocean temperatures causing retreating sea ice, has scientists worried about possible similar events in other regions of Antarctica.


Hector Glacier, along with Green Glacier and Crane Glacier near the tip of the Antarctic Peninsula, faced a significant change in 2002 when the Larsen B Ice Shelf, which had supported and stabilized the glaciers for more than 10,000 years, suddenly burst into thousands of icebergs. . Ice shelves, no longer contained by the ice shelf, rushed into the ocean and dumped billions of tons of ice.
After a period of stabilization since 2011, characterized by the formation of land-bearing ice, the glaciers suffered an unexpected failure in early 2022. Unusual waves, more than 1.5 meters high, came in from the northeast and broke the ice holding the land. This event caused an accelerated retreat of the glaciers, with Hektoria losing an astonishing 25 kilometers of ice, including both floating and stable ice on the sea floor.


The study, presented at a meeting of the American Geophysical Union, emphasizes the role of sea ice in the dynamics of the glacier, which was previously overlooked in the projections of sea level rise. As Antarctic sea ice shrinks from 2022, there are concerns that exposed coastal areas could face increased waves, which could accelerate glacier retreat.
As the current Antarctic summer progresses,

As the current Antarctic summer progresses, scientists, including UC Boulder glaciologist Ted Scambos, are keeping an eye on the situation. The continued retreat during the summer months when sea ice is absent highlights the importance of understanding the interplay between sea ice dynamics and glacier stability in Antarctica.


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