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A Positive Feedback between Iceberg Calving and Local Sea Level through Hydrostatic Pressure
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A Positive Feedback between Iceberg Calving and Local Sea Level through Hydrostatic Pressure
The Greenland and Antarctic ice sheets have experienced accelerating mass loss over recent decades. When ice is lost from a glacier or ice sheet, the reduction in gravitational pull causes sea level to drop locally. Previous work has established that this local sea level drop can produce a negati...
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