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As with Greenland, warming ocean waters contribute to Antarctic glacier ice loss. This visualization shows ocean currents circulating Pine Island Bay (West Antarctica) and flowing under Pine Island Glacier, eroding the ice where it meets the sea: https://sealevel.nasa.gov/resources/115/video-ocean-flows-under-pine-island-glacier-antarctica/ | NASA Climate Change
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Helheim Glacier is the fastest flowing glacier along the eastern edge of Greenland Ice Sheet and one of the island’s largest ocean-terminating rivers of ice. Named after the Vikings’ world of the dead, Helheim has kept scientists on their toes for the past two decades. Between 2000 and 2005, Helheim quickly increased the rate at which it dumped ice to the sea, while also rapidly retreating inland- a behavior also seen in other glaciers around Greenland. Since then, the ice loss has slowed down a
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