The oldest ice, trapped in
the deepest part of the ice sheet, could reveal temperatures eons ago.
Not exact matches
Often defined as the area within the Arctic Circle, the unspoiled territory
of the Arctic encompasses
parts of Canada, Norway, Greenland, Iceland and Russia, and cruises here offer an up - close look at snowcapped mountains,
deep fjords and gigantic
ice sheets.
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.
As Earth became colder and continental
ice sheets grew, further increase
of δ18O was due in equal
parts to
deep ocean temperature change and
ice mass change.
Rapid sea - level rise from these processes is limited to those regions where the bed
of the
ice sheet is well below sea level and thus capable
of feeding
ice shelves or directly calving icebergs rapidly, but this still represents notable potential contributions to sea - level rise, including the
deep fjords in Greenland (roughly 0.5 m; Bindschadler et al., 2013),
parts of the East Antarctic
ice sheet (perhaps as much as 20 m; Fretwell et al., 2013), and especially
parts of the West Antarctic
ice sheet (just over 3 m; Bamber et al., 2009).