Previous research found ice arches failed to form in the Nares Strait in 2007 and a record amount of sea
ice flowed south that year.
Not exact matches
Changes in
flow patterns of warm Pacific Ocean air from the
south were driving earlier spring snowmelt, while decreasing summer sea
ice had the greatest influence on later onset of snowpack in the fall.
the
south - bound expedition had cleared that vast plain of floating
ice which
flows down from the great mountains of the interior and covers the southern part of Ross Sea throughout an area above 20,000 square miles with an
ice sheet approximately 800 feet in thickness, and had begun to climb the heights which form the mountainous embayment at the head of Ross Sea.
Since a thinner
ice shell retains less heat, the tidal effects caused by Saturn on the large fractures in the
ice at the
south pole are no longer enough to explain the strong heat
flow affecting this region.
As global warming affects the earth and ocean, the retreat of the sea
ice means there won't be as much cold, dense water, generated through a process known as oceanic convection, created to
flow south and feed the Gulf Stream.
«Borehole temperatures in the
ice sheets spanning the last 6000 years show Antarctica repeatedly warming when Greenland cooled, and vice versa... The phenomena has been called the polar see - saw... Attempts to account for it have included the hypothesis of a
south -
flowing warm ocean current with a built in time lag... There is (however) no significant delay in the Anarctica climate anomaly...
If you watch the NRL Hycom animations (sequences of daily arctic
ice concentration) or look at velocity maps, a lot of the arctic cap
flows south.
At times of low solar irradiance the amounts of sea
ice in the Nordic Sea increase, this
ice is then driven
south due to the atmospheric circulation (also due to weak solar conditions) creating a more northerly air
flow in this area.
It is expected that the
ice flowing through Nares Strait will disintegrate and melt before the
south end of the Strait and Baffin Bay.
In 2000,
Ice Stream A, the southern most of several major ice streams draining from Marie Byrd Land into the Ross Ice Shelf, flowing west to Gould Coast to the south of Whillans Ice Stream, Antarctica was renamed the Mercer Ice Stream in his honor.&raq
Ice Stream A, the southern most of several major
ice streams draining from Marie Byrd Land into the Ross Ice Shelf, flowing west to Gould Coast to the south of Whillans Ice Stream, Antarctica was renamed the Mercer Ice Stream in his honor.&raq
ice streams draining from Marie Byrd Land into the Ross
Ice Shelf, flowing west to Gould Coast to the south of Whillans Ice Stream, Antarctica was renamed the Mercer Ice Stream in his honor.&raq
Ice Shelf,
flowing west to Gould Coast to the
south of Whillans
Ice Stream, Antarctica was renamed the Mercer Ice Stream in his honor.&raq
Ice Stream, Antarctica was renamed the Mercer
Ice Stream in his honor.&raq
Ice Stream in his honor.»
The
ice dam
flowing south out of Canada kept
flowing then breaking, like the flapper valve in a toilet, every 50 or so years for a thousand years.
Like a cork removed from a champagne bottle, the early break up in these passages is allowing thick, old sea
ice to
flow south from the Arctic Ocean into the North Atlantic, choking areas used by fishing, shipping and ferry boats.
During the last
ice age, a mile - high North American
ice sheet, that stretched as far
south as Long Island, N.Y., piled so much weight on the Earth that underlying mantle rock
flowed slowly outward, away from the
ice.
Ice and brine
flows south.
and his fellow explorers on their way to the magnetic
South Pole found that they had to cross and recross
flowing streams and lakes on the Nansen
Ice Shelf.
Chemical
ice nucleation of the warm
flow of moisture from the
south is clearly visible in the radar animation above.
The shelf
ice plays an important role in slowing the progress of
south polar glaciers: remove the shelf
ice and the glacier
flow accelerates.
In 1909 Ernest Shackleton and his fellow explorers on their way to the magnetic
South Pole found that they had to cross and recross
flowing streams and lakes on the Nansen
Ice Shelf.
In the map below, major
ice storm impacts (mentioned earlier) are seen in the transition zone where the warm
flow of moisture from the
south is being chemically nucleated.