Think sea levels will rise only a bit in response to an increase in global temperature of one degree? Think again!
A new study estimates that global sea levels will rise about
2.3 meters, or more than seven feet, over the next several thousand
years for every degree (Celsius) the planet warms.This international study is one of the first to combine analyses of
four major contributors to potential sea level rise into a collective
estimate, and compare it with evidence of past sea-level responses to
global temperature changes.
Results of
the study, funded primarily by the National Science Foundation and the
German Federal Ministry of Education and Research, are being published
this week in the Proceedings of the National Academy of Sciences.
"The
study did not seek to estimate how much the planet will warm, or how
rapidly sea levels will rise," noted Peter Clark, an Oregon State
University paleoclimatologist and author on the PNAS article. "Instead,
we were trying to pin down the 'sea-level commitment' of global warming
on a multi-millennial time scale. In other words, how much would sea
levels rise over long periods of time for each degree the planet warms
and holds that warmth?"
"The simulations of future scenarios we
ran from physical models were fairly consistent with evidence of
sea-level rise from the past," Clark added. "Some 120,000 years ago, for
example, it was 1-2 degrees warmer than it is now and sea levels were
about five to nine meters higher. This is consistent with what our
models say may happen in the future."
Scientists say the four
major contributors to sea-level rise on a global scale will come from
melting of glaciers, melting of the Greenland ice sheet, melting of the
Antarctic ice sheet, and expansion of the ocean itself as it warms.
Several past studies have examined each of these components, the authors
say, but this is one of the first efforts at merging different analyses
into a single projection.
The researchers ran hundreds of
simulations through their models to calculate how the four areas would
respond to warming, Clark said, and the response was mostly linear. The
amount of melting and subsequent sea-level response was commensurate
with the amount of warming. The exception, he said, was in Greenland,
which seems to have a threshold at which the response can be amplified.
Sea level rise concept photo via Shutterstock.
Source: Oregon State University.
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