When the extent of the pack of
sea ice drifting around the North Pole hit a remarkable low in 2007 (animation below), the resulting, and persistent, front - page thought was that the system was in a «death spiral» far more dramatic than any climate model had foreseen.
The video report I posted above is drawn from footage I shot five years ago, when I was lucky enough to land with an intrepid crew of scientists on the drifting, cracking, huffing, chugging
sea ice drifting around the North Pole.
Not exact matches
You can experience 41 days of conditions
around the North Pole in 44 seconds, thanks to the web cams left behind by an international research team (funded by the National Science Foundation) that annually ventures northward to install and retrieve instruments on and under the
drifting sea ice at the top of the world.
Leading
ice experts in Europe and the United States for the first time have agreed that a ring of navigable waters has opened all
around the fringes of the cap of
sea ice drifting on the warming Arctic Ocean.
These result in westerly winds (clockwise
around the pole as viewed from below) just above the edge of Antarctica in the region where the seasonal
sea ice forms, ie, the west wind
drift:
Given that calving Patagonia glaciers were far more sensitive to climate fluctuations than western Antarctica, and given the likelihood that paleo
sea -
ice extent
around Antarctica deflected iceberg
drift from present pathways, it would be helpful to know how they confirmed the respective continental sources of any dated sediments.
Thickness surveys and
drifting buoys that are part of the Arctic Observing Network (AON) suggest that much of the growth of first - year
sea ice in the Pacific sector approaches an end - of - season thickness of
around 1.7 m, independent of the starting time of freeze - up in the fall (H. Eicken, personal communication).
Cumulative
ice motions for April — July 2008 derived from
drift buoys indicate the overall transport of
ice out of the Beaufort
Sea around the Beaufort Gyre to the central Arctic was actually much stronger than in 2007, but it appears to be converging (motion is slowing) over the Amundsen and Nansen Basins.