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GEOPHYSICAL RESEARCH LETTERS, VOL. 28, NO. 2, PAGES 299–302, 2001

The Role of the Siberian High in Northern Hemisphere Climate Variability

Judah Cohen

Atmospheric and Environmental Research, Inc., Cambridge, Massachusetts


Kazuyuki Saito

Massachusetts Institute of Technology Cambridge, Massachusetts


Dara Entekhabi

Massachusetts Institute of Technology Cambridge, Massachusetts


Abstract

The dominant mode of sea level pressure (SLP) variability during the winter months in the Northern Hemisphere (NH) is characterized by a dipole with one anomaly center covering the Arctic with the opposite sign anomaly stretched across the mid-latitudes. Associated with the SLP anomaly, is a surface temperature anomaly induced by the anomalous circulation. We will show that this anomaly pattern originates in the early fall, on a much more regional scale, in Siberia. As the season progresses this anomaly pattern propagates and amplifies to dominate much of the extratropical NH, making the Siberian high a dominant force in NH climate variability in winter. Also since the SLP and surface temperature anomalies originate in a region of maximum fall snow cover variability, we argue that snow cover partially forces the phase of winter variability and can potentially be used for the skillful prediction of winter climate.

Received 20 June 2000; accepted 21 September 2000.

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Citation: Cohen, J., K. Saito, and D. Entekhabi (2001), The Role of the Siberian High in Northern Hemisphere Climate Variability, Geophys. Res. Lett., 28(2), 299–302.