Observed forcing-feedback processes between Northern Hemisphere atmospheric circulation and Arctic sea ice coverage
A lagged maximum covariance analysis is applied to investigate linear covariability between monthly sea ice concentration (SIC) and atmosphere circulation in the Northern Hemisphere. The dominant signal is the atmospheric forcing of SIC anomalies throughout the year, but a wintertime atmospheric sig...
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Veröffentlicht in: | Journal of Geophysical Research: Atmospheres 2010-07, Vol.115 (D14), p.n/a |
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Format: | Artikel |
Sprache: | eng |
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