Mori, M. et al. (2014) Robust Arctic sea - ice influence on the frequent
Eurasian cold winters in past decades, Nature Geoscience, doi: 10.1038 / ngeo2277
Since the heat is just moved around, with
Eurasian cold linked to a correspondingly warmer Arctic, this hardly affects the global mean temperature — unless you're looking at a data set with a large data gap in the Arctic...
Mori, M. et al. (2014) Robust Arctic sea - ice influence on the frequent
Eurasian cold winters in past decades, Nature Geoscience, doi: 10.1038 / ngeo2277
Not exact matches
The Carnegie Russia and Eurasia Program has, since the end of the
Cold War, led the field of
Eurasian security, including strategic nuclear weapons and nonproliferation, development, economic and social issues, governance, and the rule of law.
However, if you see
Cold War merely as a specific manifestation of a generic geopolitical conflict between Russian interest to create a defensible empire, and US interest to prevent a creation of a powerful
Eurasian empire combining Russia's natural resources and European resources, then you will see why current events show a marked resemblance to
Cold War.
And a second one that explains the
cold Eurasian winters, but without affecting the global mean temperature.
So if you apply a negative sign to the figure at the bottom of / / seaice.apl.washington.edu/AO/, I would expect
colder than normal spring especially in the
Eurasian Arctic, less retreat of sea ice this summer, then
colder than normal this fall in the
Eurasian Arctic....
The AFZ is best developed along the
Eurasian and Alaskan coasts, especially in Eastern Siberia and north of Alaska's Brooks Range, where it appears that temperature gradients are sharpened by topographic trapping of
cold Arctic Ocean air.
For example, giving a skeletal and brief overview: at stage one, a
cold AMO coincides with increased sea ice extent in the West
Eurasian Arctic.
Because low Barents - Kara sea ice and high
Eurasian snow cover favor northwestward expansion of the Siberian high, this atmospheric pattern increases the probability of driving
cold Siberian air southeastward into populous East Asia.
«Those who count the Arctic warmth as evidence for global warming should count the
Eurasian [
cold] as evidence for global cooling»
(Those who count the Arctic warmth as evidence for global warming should count the
Eurasian code [
cold] as evidence for global cooling.)
Hot north pole: the
cold polar air has shifted over to us on the
eurasian continent.
In retrospect, our overall outlook of setting a new record minimum based on the vast amount of FY ice should have been tempered by the fact that the FY ice over the pole should be thicker since it was the first ice to grow last fall and the north pole is also
colder than the
Eurasian and Alaskan coasts, and during summer this ice is subject to less incident sunlight.
NSF - funded research has shown that variability in the extent of
Eurasian snow cover can be used to predict
cold or warm winters across the entire mid-latitudes of the Northern Hemisphere.
Or Arctic sea ice loss could lead to an increase of snow on high - latitude land, which in turn impacts the jet stream resulting in
cold Eurasian and North American winters.
Luo, D., Yao, Y., Dai, A., Simmonds, I. & Zhong, L. Increased quasi stationarity and persistence of winter Ural blocking and
Eurasian extreme
cold events in response to Arctic warming.