Sentences with phrase «eurasian winters»

And a second one that explains the cold Eurasian winters, but without affecting the global mean temperature.

And the Eurasian winter cooling could be a separate, superimposed effect, with no impact on global mean temperature and hence nothing to do with the «pause».

A central topic will be teleconnections in the climate system, i.e. how a change in climate in one part of the globe (e.g. temperatures in the Atlantic or shrinking sea ice cover in the Arctic) can influence climate on other parts of the globe (e.g. Eurasian winter temperatures), and how we can use this information to improve regional climate prediction and therefore regional climate service.

Not exact matches

McCusker, K. E., Fyfe, J. C. & Sigmond, M. Twenty - five winters of unexpected Eurasian cooling unlikely due to arctic sea ice loss.

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

The property makes a critical contribution to the conservation of the natural values within the Great Rift Valley, as an integral part of the most important route of the African - Eurasian flyway system where billions of birds are found to travel from northern breeding grounds to African wintering places.

If this Arctic winter was expansive deeply southwards, bi-continental in size, on Eurasian and North American side at once, no way it would have materialized.

Judah has been publishing on the link between Eurasian snow cover in autumn and the NAM / NAO in the following winter for quite some time.

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

It is found that winter sea ice is about 50 cm thinner in high - NAO index years than in low - NAO index years in the Eurasian coastal region mainly due to stronger wind - driven ice export.

The speed of formation of the Eurasian snowfield is correlated with a stronger winter Siberian high and migration into the Arctic.

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.

The dust - induced thermal contrast changes between the Eurasian continent and the surrounding oceans are found to trigger or modulate a rapidly varying or unstable Asian winter monsoon circulation, with a feedback to reduce the dust emission from its sources (Zhang et al., 2002).

Therefore, we suggest that a significant portion of the wintertime temperature trend is driven by dynamical interactions between October Eurasian snow cover, which has increased over the last two decades, and the large - scale NH extratropical circulation in the late autumn and winter.

Physically, one could expect a slight decrease in surface evaporation (a «dimming» effect) and related changes to precipitation, a warming of the tropopause and lower stratosphere (and changes in static stability), increased Eurasian «winter warming» effects (related to shifts in the wind patterns as are seen in the aftermath ofvolcanoes).

Physically, one could expect a slight decrease in surface evaporation (a «dimming» effect) and related changes to precipitation, a warming of the tropopause and lower stratosphere (and changes in static stability), increased Eurasian «winter warming» effects (related to shifts in the wind patterns as are seen in the aftermath of volcanoes).

Most of the proposed mechanisms linking reduced sea ice and / or increased Eurasian snowcover to extreme winter weather across mid-latitude NH continents involve a pathway through the SPV6, 24,25,32,33,55,56,57.

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.