Following up on my post from last week on the Arctic Oscillation, Ken Chang has written a Week in Review story with a bit more detail on
the unusual atmospheric patterns behind the big, but very constrained, chill, and the dominance of warm conditions — just not where a lot of Western media are situated.
Another factor that conspired to accelerate the ice loss this summer was
an unusual atmospheric pattern, with persistent high atmospheric pressures over the central Arctic Ocean and lower pressures over Siberia.
Not exact matches
Air naturally poor in ozone was, for example, lifted into the lower stratosphere above Britain from the sub-tropical Atlantic, by an
unusual pattern of
atmospheric circulation.
But I believe there is little doubt that the record - breaking scale and potential destructiveness of Sandy is due in large part to the amplifying effects of warmer ocean temperatures, higher
atmospheric moisture content, and
unusual Arctic weather
patterns.
The
unusual pattern of
atmospheric high and low pressure over and around the Arctic that has contributed to the recent snow and cold from Alabama to Washington, to East Anglia, England (and rain and warmth along the west coast of Greenland) is also an important influence on the shifting sheath of sea ice on the Arctic Ocean.
Some respondents note that
atmospheric circulation played a role in 2007, but that it is not probable that such an
unusual wind
pattern will repeat itself in 2008.
This very
unusual atmospheric configuration — in which the large - scale
atmospheric wave
pattern appears to be largely «stuck» in place — has been characterized by a seemingly ever - present West Coast ridge and a similarly stubborn trough over central and eastern United States (commonly referred to in media coverage as the «Polar Vortex,» though this terminology is arguably problematic).
In 2007, the NSIDC explained the ice loss as «the
atmospheric pressure
pattern over the Arctic has been
unusual this summer.
Because the longwave
atmospheric weather
patterns (Rossby waves) have a scale of several thousand kilometers, it is not
unusual for the temperature of a region the size of the United States to be substantially warmer or co lder during a single season than the zonal mean temperature.
Most persistent
atmospheric anomalies are ultimately linked to
unusual patterns of ocean surface temperature.
NASA scientist Son Nghiem says «The winds causing this trend in ice reduction were set up by an
unusual pattern of
atmospheric pressure that began at the beginning of this century,» (Oct 2007)