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Winter climate response to continental snow anomalies

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dc.contributor.advisor Dara Entekhabi. en_US
dc.contributor.author Gong, Gavin, 1969- en_US
dc.contributor.other Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. en_US
dc.date.accessioned 2005-05-19T15:17:40Z
dc.date.available 2005-05-19T15:17:40Z
dc.date.copyright 2003 en_US
dc.date.issued 2003 en_US
dc.identifier.uri http://hdl.handle.net/1721.1/16920
dc.description Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2003. en_US
dc.description Includes bibliographical references (p. 137-142). en_US
dc.description This electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections. en_US
dc.description.abstract Climate variability has emerged in recent decades as an important field of geoscience research. A thorough understanding of the patterns and causes of climate variability is required to predict and prepare for upcoming climatic shifts, and also to accurately distill anthropogenic climate change signals from naturally occurring variations. In the extratropical Northern Hemisphere, regional climate patterns are strongly related to a hemispheric-scale mode of variability known as the Arctic Oscillation (AO). A major challenge for current climate variability studies is to predict the phase and magnitude of the AO, as it is a fundamental, internal mode of the atmosphere, but can nevertheless be triggered through a myriad of external perturbations. In this thesis the influence of one hypothesized external perturbation, continental-scale land surface snow anomalies, is investigated. Satellite observations of historical autumn-winter snow cover are used to develop model boundary conditions for a series of snow-forced numerical General Circulation Model (GCM) experiments. Realistic snow forcing over Siberia is found to exert a modulating influence on the winter season AO mode, which is consistent with observations. This winter climate response occurs via anatmospheric teleconnection pathway involving established stationary wave - mean flow interaction processes throughout the troposphere and stratosphere. The pathway is enabled by the specific and unique geographic and orographic conditions that exist in Siberia, and their role in the development of planetary waves. This model-simulated pathway provides a physical explanation for how regional land surface snow anomalies can influence hemispheric-scale winter climate. en_US
dc.description.abstract (cont.) The results of this study may potentially lead to improved seasonal predictions of winter climate, based on remotely-sensed Siberian snow conditions during the preceding autumn. The results also contribute to the field of land surface - atmosphere coupling by demonstrating interactions that occur outside of the warm season, and on broad continental and hemispheric scales. en_US
dc.description.statementofresponsibility by Gavin Gong. en_US
dc.format.extent 142 p. en_US
dc.format.extent 10730242 bytes
dc.format.extent 10729996 bytes
dc.format.mimetype application/pdf
dc.format.mimetype application/pdf
dc.language.iso eng en_US
dc.publisher Massachusetts Institute of Technology en_US
dc.rights M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. en_US
dc.rights.uri http://dspace.mit.edu/handle/1721.1/7582
dc.subject Civil and Environmental Engineering. en_US
dc.title Winter climate response to continental snow anomalies en_US
dc.type Thesis en_US
dc.description.degree Ph.D. en_US
dc.contributor.department Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. en_US
dc.identifier.oclc 52770036 en_US


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