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Sea levels respond directly to global temperatures, both through the melting of ice shelves and through the expansion of water as it warms. |
Sea surface temperatures today are strikingly similar to
those during the last interglacial period, when sea levels were six to nine
metres above their present height, according to research.
The findings provide compelling evidence that Greenland and
Antarctica’s continental ice sheets are highly sensitive to slight increases in
ocean temperatures, and raise the prospect of sea levels continuing to rise for
many centuries.
Previous research had shown that sea levels rose by several
metres during the last interglacial (LIG), between 129,000 to 116,000 years
ago, but until now the picture of how sea temperatures had varied over the same
period had remained patchy.
The latest research, based on marine sediment core records
from 83 sites, concludes that sea temperatures towards the end of the LIG were
comparable to those seen today.
Rob DeConto, a climate scientist at the University of Massachusetts, Amherst, who was not involved in the research said: “This tells
us that the big ice sheets are really sensitive to just a little bit of
warming. That’s a really powerful message.”
Read The Guardian
story - “Sea levels could rise by six to nine metres over time, new study warns.”
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