In the NWP region, multi-year
ice distribution patterns suggest that the coming year will only see limited openings in the northern parts of the route.
Nares Strait Recent ice advection patterns; warm water advances into the Arctic from the Atlantic;
ice distribution patterns: all of these things show that conditions continue to be advantageous for export of ice through Fram Strait.
Not exact matches
So if you think of going in [a] warming direction of 2 degrees C compared to a cooling direction of 5 degrees C, one can say that we might be changing the Earth, you know, like 40 percent of the kind of change that went on between the
Ice Age; and now are going back in time and so a 2 - degree change, which is about 4 degrees F on a global average, is going to be very significant in terms of change in the
distribution of vegetation, change in the kind of climate zones in certain areas, wind
patterns can change, so where rainfall happens is going to shift.
The pair then went over alternative explanations for the
distribution pattern, such as erosion by wind or burial under material flowing from
ice volcanoes.
Predicting sea
ice extent is easy if you can mentally calculate wind variations, momentum, sea currents, multi year
ice compression ratios, tidal synergy with weather
patterns, the AO, the temperature of
ice sea water and air, how cloudy it will be, salinity, pycnocline convection rates, sea surface to air interface, CO2 exchange,
ice thickness
distributions.....
But the issue is not really the global mean temperature (even though that is what is usually plotted), but the
distribution of temperature change, rainfall
patterns, winds, sea
ice etc..
In the Arctic, the tipping points identified in the new report, published on Friday, include: growth in vegetation on tundra, which replaces reflective snow and
ice with darker vegetation, thus absorbing more heat; higher releases of methane, a potent greenhouse gas, from the tundra as it warms; shifts in snow
distribution that warm the ocean, resulting in altered climate
patterns as far away as Asia, where the monsoon could be effected; and the collapse of some key Arctic fisheries, with knock - on effects on ocean ecosystems around the globe.»
Researchers at CIRES» National Snow and
Ice Data Center [About NSIDC] investigate the dynamics of Antarctic ice shelves, new techniques for the remote sensing of snow and freeze / thaw cycle of soils, the role of snow in hydrologic modeling, linkages between changes in sea ice extent and weather patterns, large - scale shifts in polar climate, river and lake ice, and the distribution and characteristics of seasonally and permanently frozen grou
Ice Data Center [About NSIDC] investigate the dynamics of Antarctic
ice shelves, new techniques for the remote sensing of snow and freeze / thaw cycle of soils, the role of snow in hydrologic modeling, linkages between changes in sea ice extent and weather patterns, large - scale shifts in polar climate, river and lake ice, and the distribution and characteristics of seasonally and permanently frozen grou
ice shelves, new techniques for the remote sensing of snow and freeze / thaw cycle of soils, the role of snow in hydrologic modeling, linkages between changes in sea
ice extent and weather patterns, large - scale shifts in polar climate, river and lake ice, and the distribution and characteristics of seasonally and permanently frozen grou
ice extent and weather
patterns, large - scale shifts in polar climate, river and lake
ice, and the distribution and characteristics of seasonally and permanently frozen grou
ice, and the
distribution and characteristics of seasonally and permanently frozen ground.
While total extent and the general
distribution of the
ice cover is similar to last year, the atmospheric
patterns are quite different.
While the effects of higher temperatures are still poorly understood, scientists are concerned that climate change could have a major impact on weather
patterns, the
distribution of
ice, ecosystems, and ocean currents and sea levels.
At this point, the regional outlook on
ice conditions indicates that the large - scale weather
patterns, which dominated in August with cooler conditions and advection of
ice into the eastern North American Arctic, can also help explain much of the observed
ice distribution at the local level.
In the Beaufort and Chukchi seas,
ice distribution mimicks the Beaufort Gyre circulation
pattern with advection of
ice from the high Canadian Arctic into the Beaufort Sea and export of
ice northward in the Chukchi Sea.