Not exact matches
The icebergs that find their way into the paths of transatlantic liners come down from the coast of Greenland; for the interior of Greenland is a
huge ice sheet fringed
by mountains and promontories.
During the last
ice age, much of North America was covered
by a giant
ice sheet that many scientists believe underwent several catastrophic collapses, causing
huge icebergs to enter the North Atlantic — phenomena known as Heinrich events.
The beginning of the last glacial period was characterized in the Northern hemisphere
by significant accumulation of snow at high latitudes and the formation of a
huge polar
ice sheet.
We have fairly high confidence that we observe the history of Heinrich events (
huge discharges of
ice - rafted debris from the Laurentide
ice sheet through Hudson Bay that are roughly coincident with large southern warming, southward shift of the intertropical convergence zone, extensive sea
ice in the north Atlantic, reduced monsoonal rainfall in at least some parts of Asia, and other changes), and also cold phases of the Dansgaard / Oeschger oscillations that lack Heinrich layers and are characterized
by muted versions of the other climate anomalies I just mentioned.
Some programs were
huge, mobilizing cooperation among a dozen or more nations to provide data from weather stations, research ships, and (
by far the most expensive) satellites to monitor temperatures, clouds, ocean currents,
ice sheets and more.
The new results indicate that the similar and seemingly unstoppable melting of
huge swaths of the West Antarctic
Ice Sheet (WAIS) today
by relatively warm ocean waters has precedent in an earlier era, members of the research team and other scientists said.
These authors postulated an extended Barents Sea
Ice Sheet, the western part of the huge Eurasian Ice Sheet51, 55, that had reached the shelf edge causing polynya - like open - water conditions (triggered by strong katabatic winds) with phytoplankton and sea ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 -
Ice Sheet, the western part of the
huge Eurasian
Ice Sheet51, 55, that had reached the shelf edge causing polynya - like open - water conditions (triggered by strong katabatic winds) with phytoplankton and sea ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 -
Ice Sheet51, 55, that had reached the shelf edge causing polynya - like open - water conditions (triggered
by strong katabatic winds) with phytoplankton and sea
ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 -
ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 - 2.
To leap from that to the claimed 3 - 7ºC warming requires that the changes in the
ice sheets and vegetation arising from the current and (medium term) committed warming would increase the radiative imbalance
by another ~ 2 W / m2 — and that is extreme (for reference, the changes between the last
ice age and now from these factors is only about 4 W / m2 (Kohler et al, 2010) with the
huge impact of the N. American and European
ice sheets included).