The Hidden Meltdown of Greenland
 
Aug. 28, 2015: More than 90 percent of our planet's freshwater ice is bound in
the massive ice sheets and glaciers of the Antarctic and Greenland. As
temperatures around the world slowly climb, melt waters from these vast stores
of ice add to rising sea levels.  All by itself, Greenland could bump sea
levels by 7 meters (23 feet) if its ice melted completely.
 
And . it's melting.
 
http://youtu.be/xkxjyZmdJgg
 
NASA-supported researchers have found that ice covering Greenland is melting
faster than previously thought. .
 
In August 2014, Eric Rignot, a glaciologist working at the University of
California, Irvine  and NASA's Jet Propulsion Laboratory, led a team in
mapping ice cliffs at the front edges of three outlet glaciers in Greenland.
The researchers found cavities that undercut the base of these leading edges
that can destabilize the ice front and enhance iceberg calving, the process
where parts of the glacier break off and float away.
 
"In Greenland we have melt rates of a few meters a day in the summer months,"
says Rignot.
 
What's causing this `big thaw'?
 
Rignot's team found that Greenland's glaciers flowing into the ocean are
grounded deeper below sea level than previously measured. This means that the
warm ocean currents at depth can sweep across the glacier faces and erode them.
 
"In polar regions, the upper layers of ocean water are cold and fresh," he
explains.  "Cold water is less effective at melting ice."
 
"The real ocean heat is at a depth of 350-400 meters and below. This warm,
salty water is of subtropical origin and melts the ice much more rapidly."
 
Rignot's research team is providing critical information needed to document
this effect and accurately predict where and how fast glaciers will give way.
The team gathered and analyzed around-the-clock measurements of the depth,
salinity, and temperature of channel waters and their intersection with the
coastal edge of Greenland's ice sheet.
 
They found that some of the glaciers balance on giant earthen sills that are
protecting them, for now. But other glaciers are being severely undercut out
of sight beneath the surface, meaning they could collapse and melt much sooner.
 
It's not easy gathering such data. On top of the rough waters, wind, rain, and
cold weather, there's the ice itself.
 
"We came to study glaciers that discharge into the fjord. And the fjords are
full of ice. In some places it can be so full of ice that the boat can't even
push through."
 
But ice holds a peculiar fascination for Rignot. "I've always been interested
in polar regions,"he says. "My friends wanted to cruise in the Caribbean but
I'd rather cruise here in these waters. I don't know why. I just like them."
 
What's next?
 
"OMG," answers Rignot. And he's not using chatspeak.
 
OMG stands for Ocean Melting Greenland -- the name of a new NASA-funded 5-year
project that will take their investigation even further, to the four corners
of Greenland by ship and by plane.
 
`'We hope that the data collected will be a game changer for studying
ice-ocean interaction in Greenland,'' says Rignot. `'It will help modelers
make better projections of Greenland ice sheet melt in the future.''
 
Rignot's results have been accepted for publication in the journal Geophysical
Research Letters and are now available online.
 
 
Regards,
 
Roger

--- D'Bridge 3.99
 * Origin: NCS BBS - Houma, LoUiSiAna (1:3828/7)