NASA Satellite Data Uncovers Active Water Movement Beneath West Antarctic Ice Sheet
NASA's ICESat satellite revealed major changes in West Antarctica's ice surface between 2003-2006, indicating a dynamic system of subglacial lakes filling and draining, with one lake releasing ~2 cubic km of water in three years.
AI-generated summary
Antarctica's ice dynamics significantly impact global sea levels.
Antarctica's ice surface changes revealed by NASA's ICESat satellite between 2003-2006 showed a dynamic subglacial water system. Geophysicist Helen Amanda Fricker identified a previously unknown subglacial lake, Subglacial Lake Engelhardt, which drained ~2 cubic km of water in three years. The study, published in "Science", highlighted 14 areas of ice elevation changes, indicating filling and draining lakes. This system affects ice stream speed and, by extension, sea-level changes. Conditions beneath the ice, including Earth's interior heat and ice friction, allow liquid water to exist. The findings changed the understanding of Antarctica's subglacial environment from static to active, with implications for modeling ice sheet behavior. Subsequent research expanded the known scope of such lakes across Antarctica.
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Further ICESat data will reveal more dynamic subglacial activity.
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