A Major Glacier is Undermined: Ocean Currents Speed Melt of Antarctic Ice
Global warming nightmare?
Ocean Currents Speed Melting of Antarctic Ice
Stronger ocean currents beneath West Antarctica’s Pine Island Glacier Ice Shelf are eroding the ice from below, speeding the melting of the glacier as a whole, according to a new study in Nature Geoscience. A growing cavity beneath the ice shelf has allowed more warm water to melt the ice, the researchers say—a process that feeds back into the ongoing rise in global sea levels. The glacier is currently sliding into the sea at a clip of four kilometers (2.5 miles) a year, while its ice shelf is melting at about 80 cubic kilometers a year - 50 percent faster than it was in the early 1990s - the paper estimates.
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Tags: Columbia University, Pine Island Glacier Ice Shelf
Permission to reprint this blog post in whole or in part is hereby granted, provided that the author (or authors) and Dave Lucas are properly cited. Permission to reprint any comments below is granted only for those comments written by Dave Lucas and staff.
Tags: Columbia University, Pine Island Glacier Ice Shelf
Permission to reprint this blog post in whole or in part is hereby granted, provided that the author (or authors) and Dave Lucas are properly cited. Permission to reprint any comments below is granted only for those comments written by Dave Lucas and staff.