The role of the Siberian high in northern hemisphere climate variability

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...

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Bibliographic Details
Main Authors: Cohen, Judah, Saito, Kazuyuki, Entekhabi, Dara
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: American Geophysical Union (AGU) 2017
Online Access:http://hdl.handle.net/1721.1/110326
https://orcid.org/0000-0002-8362-4761

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