Sorry for the forum being offline some hours, guys! DM
The study, published Sunday in the journal Nature Climate Change, is the first to find correlations between rapid Arctic warming and extreme summer weather events, since previous research had focused on the links between Arctic warming and fall and winter weather patterns.
The past decade has seen an exceptional number of unprecedented summer extreme weather events in northern mid-latitudes, along with record declines in both summer Arctic sea ice and snow cover on high-latitude land. The underlying mechanisms that link the shrinking cryosphere with summer extreme weather, however, remain unclear. Here, we combine satellite observations of early summer snow cover and summer sea-ice extent with atmospheric reanalysis data to demonstrate associations between summer weather patterns in mid-latitudes and losses of snow and sea ice. Results suggest that the atmospheric circulation responds differently to changes in the ice and snow extents, with a stronger response to sea-ice loss, even though its reduction is half as large as that for the snow cover. Atmospheric changes associated with the combined snow/ice reductions reveal widespread upper-level height increases, weaker upper-level zonal winds at high latitudes, a more amplified upper-level pattern, and a general northward shift in the jet stream. More frequent extreme summer heat events over mid-latitude continents are linked with reduced sea ice and snow through these circulation changes.
I'd have thought many of us were very interested in the links between ice loss ( esp. across the USA and NW Europe???)?[/url]A bit more weight to Ms Francis and co.?
Since 2007 a large decline in Arctic sea ice has been observed. The large-scale atmosphericcirculationresponsetothisdeclineisinvestigatedinERA-InterimreanalysesandHadGEM3climate model experiments. In winter, post-2007 observed circulation anomalies over theArctic, North Atlantic and Eurasia are small compared to interannual variability. Insummer, the post-2007 observed circulation is dominated by an anticyclonic anomalyover Greenland which has a large signal-to-noise ratio. Climate model experiments drivenby observed SST and sea ice anomalies are able to capture the summertime pattern ofobserved circulation anomalies, although the magnitude is a third of that observed. Theexperiments suggest high SSTs and reduced sea ice in the Labrador Sea lead to positivetemperature anomalies in the lower troposphere which weaken the westerlies over NorthAmerica through thermal wind balance. The experiments also capture cyclonic anomaliesover Northwest Europe, which are consistent with downstream Rossby wave propagation