Incredible Map Shows Vanishing Land Due To Rising Ocean
Sea
levels are rising faster than expected from global warming
1
November, 2012
Sea
levels are rising faster than expected from global warming, and
University of Colorado geologist Bill Hay has a good idea why. The
last official IPCC report in 2007 projected a global sea level rise
between 0.2 and 0.5 meters by the year 2100. But current sea-level
rise measurements meet or exceed the high end of that range and
suggest a rise of one meter or more by the end of the century.
Past
and possible future changes in sea level
Map
by Emanuel Soeding, Christian-Albrechts University, using U.S.
National Oceanic & Atmospheric Administration Click
here for larger map.
“What’s
missing from the models used to forecast sea-level rise are critical
feedbacks that speed everything up,” says Hay. He will be
presenting some of these feedbacks in a talk on Sunday, 4 Nov., at
the meeting of The Geological Society of America in Charlotte, North
Carolina, USA.
One
of those feedbacks involves Arctic sea ice, another the Greenland ice
cap, and another soil moisture and groundwater mining.
“There
is an Arctic sea ice connection,” says Hay, despite the fact that
melting sea ice — which is already in the ocean — does not itself
raise sea level. Instead, it plays a role in the overall warming of
the Arctic, which leads to ice losses in nearby Greenland and
northern Canada. When sea ice melts, Hay explains, there is an
oceanographic effect of releasing more fresh water from the Arctic,
which is then replaced by inflows of brinier, warmer water from the
south.
“So
it’s a big heat pump that brings heat to the Arctic,” says Hay.
“That’s not in any of the models.” That warmer water pushes the
Arctic toward more ice-free waters, which absorb sunlight rather than
reflect it back into space like sea ice does. The more open water
there is, the more heat is trapped in the Arctic waters, and the
warmer things can get.
Then
there are those gigantic stores of ice in Greenland and Antarctica.
During the last interglacial period, sea level rose 10 meters due to
the melting of all that ice — without any help from humans. New
data suggests that the sea-level rise in the oceans took place over a
few centuries, according to Hay.
“You
can lose most of the Greenland ice cap in a few hundred years, not
thousands, just under natural conditions,” says Hay. “There’s
no telling how fast it can go with this spike of carbon dioxide we
are adding to the atmosphere.”
This
possibility was brought home this last summer as Greenland underwent
a stunning, record-setting melt. The ice streams, lubricated by water
at their base, are speeding up.
Hay
notes, “Ten years ago we didn’t know much about water under the
Antarctic ice cap.” But it is there, and it allows the ice to move
— in some places even uphill due to the weight of the ice above it.
“It’s
being squeezed like toothpaste out of a tube,” explains Hay. The
one thing that’s holding all that ice back from emptying into the
sea is the grounded ice shelves acting like plugs on bottles at the
ends of the coastal glaciers. “Nobody has any idea how fast that
ice will flow into the oceans once the ice shelves are gone.”
Another
missing feedback is the groundwater being mined all over the world to
mitigate droughts. That water is ultimately added to the oceans (a
recent visualization of this effect in the U.S. was posted by NASA’s
Earth
Observatory: http://earthobservatory.nasa.gov/IOTD/view.php?id=79228).
All
of these are positive feedbacks speeding up the changes in climate
and sea-level rise.
“You
would expect negative feedbacks to creep in at some point,” says
Hay. “But in climate change, every feedback seems to go positive.”
The reason is that Earth’s climate seems to have certain stable
states. Between those states things are unstable and can change
quickly. “Under human prodding, the system wants to go into a new
climate state.”
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