Not exact matches
In August 2015, University
of Delaware oceanographer Andreas Muenchow and colleagues deployed the first UD ocean sensors underneath Petermann Glacier in North Greenland, which
connects the great Greenland
ice sheet directly with the ocean.
A March study shows that one large swath
of the
ice sheet sits on beds as deep as 8,000 feet below sea level and is
connected to warming ocean currents.
The new result focuses on
ice loss due to a major retreat
of an outlet glacier
connected to a long «river»
of ice — known as an
ice stream — that drains
ice from the interior
of the
ice sheet.
Increased
ice flow in this region is particularly troubling, Khan said, because the northeast
ice stream stretches more than 600 kilometers (about 373 miles) into the center
of the
ice sheet, where it
connects with the heart
of Greenland's
ice reservoir.
I would like to echo Mr. Edmonds inquiry as to the stability
of the Pine Island and Thwaites glaciers which seem to
connect directly to the Byrd Subpolar Basin, where the
ice sheets are grounded far below sea level.
For example: much
of the Antarctic
ice sheet is grounded below sea level, and some
of the deepest parts are
connected all the way to the open ocean by
ice grounded below sea level.
I would like to echo Mr. Edmonds inquiry as to the stability
of the Pine Island and Thwaites glaciers which seem to
connect directly to the Byrd Subpolar Basin, where the
ice sheets are grounded far below sea level.
«Since the last Intergovernmental Panel on Climate Change report [in 2007], which highlighted uncertainties
connected with
ice sheets, almost every significant piece
of research we've produced has increased the significance
of the ocean for West Antarctica and Greenland,» said Prof Vaughan.
The Petermann glacier is one
of the largest glaciers
connecting the Greenland inland
ice sheet with the Arctic Ocean.