Not exact matches
The three regions with a most notorious
sea ice area reduction in the summer last year were the East Siberian Sea Ice Area, the Chukchi Sea Ice Area and the Arctic Basin Sea Ice Ar
sea ice area reduction in the summer last year were the East Siberian Sea Ice Area, the Chukchi Sea Ice Area and the Arctic Basin Sea Ice Ar
ice area
reduction in the summer
last year were the East Siberian
Sea Ice Area, the Chukchi Sea Ice Area and the Arctic Basin Sea Ice Ar
Sea Ice Area, the Chukchi Sea Ice Area and the Arctic Basin Sea Ice Ar
Ice Area, the Chukchi
Sea Ice Area and the Arctic Basin Sea Ice Ar
Sea Ice Area and the Arctic Basin Sea Ice Ar
Ice Area and the Arctic Basin
Sea Ice Ar
Sea Ice Ar
Ice Area.
The article in The Independent makes its predictions based on the increased speed of
reduction of the
Sea Ice Area compared to
last year.
The corresponding future temperatures in Greenland are comparable to those inferred for the
last interglacial period 125,000 years ago, when paleoclimatic information suggests
reductions of polar land
ice extent and 4 to 6 m of
sea level rise.
The influence of anthropogenic forcing has also been detected in various physical systems over the
last 50 years, including increases in global oceanic heat content, increases in
sea level, shrinking of alpine glaciers,
reductions in Arctic
sea ice extent, and
reductions in spring snow cover (Hegerl et al., 2007).
For anyone else interested (and please correct me if I get this wrong, Judy) the
reduction of
sea ice extent for September is more pronounced than any other month over the
last ~ 30 years.
Drastic
reductions in Arctic
sea ice in the
last decade may be intensifying the chemical release of bromine into the atmosphere, resulting in ground - level ozone depletion and the deposit of toxic mercury in the Arctic, according to a new NASA - led study.
Post-glacial rebound - The vertical movement of the land and
sea floor following the
reduction of the load of an
ice mass, for example, since the
Last Glacial Maximum (21 ka).
Both the observations of mass balance and the estimates based on temperature changes (Table 11.4) indicate a
reduction of mass of glaciers and
ice caps in the recent past, giving a contribution to global - average
sea level of 0.2 to 0.4 mm / yr over the
last hundred years.
Last September, the Royal Society hosted a Workshop on Arctic
sea ice reduction: the evidence, models, and global impacts.
Based on the
last 20 years, the
reduction in
sea ice cover and its thickness have enhanced the warming of the Arctic throughout the year.
Predictions of future
sea - level rise and
reduction in volume of
ice sheets are consistent with what the evidence indicates during the
Last Interglacial.
Higher levels of
sea salts favor
reduction processes and thus GEM destruction in the snow interstitial air (30), but no long - term trends have been reported for
sea salt impurities deposited on the Greenland
ice sheet during the
last century (33).
Nevertheless, as I have said, the impact of the
reductions in Arctic
sea ice extent, which we have seen in the
last few years on our winter climate, is only one of a number of factors, and certainly
last year was probably not the dominant factor.
The
last time the polar regions were significantly warmer than present for an extended period (about 125,000 years ago with Co2 at 287ppm),
reductions in polar
ice volume led to 4 to 6 meters of
sea level rise.
The
Last Interglacial was also a period with higher global
sea - level and a corresponding
reduction in
ice sheet area and volume, which are consistent with IPCC predictions for responses to future global warming.