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Winter 2009-2010: A case study of an extreme Arctic Oscillation event
by
Barlow, Mathew
, Foster, James
, Saito, Kazuyuki
, Cohen, Judah
, Jones, Justin
in
Arctic Oscillation
/ Atmospheric sciences
/ climate dynamics
/ Cryosphere
/ Earth sciences
/ Earth, ocean, space
/ El Nino
/ Exact sciences and technology
/ Extreme cold
/ seasonal prediction
/ Snow
/ Southern Oscillation
/ Stratosphere
/ Troposphere
/ Winter
2010
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Winter 2009-2010: A case study of an extreme Arctic Oscillation event
by
Barlow, Mathew
, Foster, James
, Saito, Kazuyuki
, Cohen, Judah
, Jones, Justin
in
Arctic Oscillation
/ Atmospheric sciences
/ climate dynamics
/ Cryosphere
/ Earth sciences
/ Earth, ocean, space
/ El Nino
/ Exact sciences and technology
/ Extreme cold
/ seasonal prediction
/ Snow
/ Southern Oscillation
/ Stratosphere
/ Troposphere
/ Winter
2010
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Winter 2009-2010: A case study of an extreme Arctic Oscillation event
by
Barlow, Mathew
, Foster, James
, Saito, Kazuyuki
, Cohen, Judah
, Jones, Justin
in
Arctic Oscillation
/ Atmospheric sciences
/ climate dynamics
/ Cryosphere
/ Earth sciences
/ Earth, ocean, space
/ El Nino
/ Exact sciences and technology
/ Extreme cold
/ seasonal prediction
/ Snow
/ Southern Oscillation
/ Stratosphere
/ Troposphere
/ Winter
2010
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Winter 2009-2010: A case study of an extreme Arctic Oscillation event
Journal Article
Winter 2009-2010: A case study of an extreme Arctic Oscillation event
2010
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Overview
Winter 2009–2010 made headlines for extreme cold and snow in most of the major population centers of the industrialized countries of the Northern Hemisphere (NH). The major teleconnection patterns of the Northern Hemisphere, El Niño/Southern Oscillation (ENSO) and the Arctic Oscillation (AO) were of moderate to strong amplitude, making both potentially key players during the winter of 2009–2010. The dominant NH winter circulation pattern can be shown to have originated with a two‐way stratosphere‐troposphere interaction forced by Eurasian land surface and lower tropospheric atmospheric conditions during autumn. This cycle occurred twice in relatively quick succession contributing to the record low values of the AO observed. Using a skillful winter temperature forecast, it is shown that the AO explained a greater variance of the observed temperature pattern across the extratropical landmasses of the NH than did ENSO.
Publisher
Blackwell Publishing Ltd,American Geophysical Union,John Wiley & Sons, Inc
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