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)