ResearchWorks Archive

Annular modes in the atmospheric general circulation

Show simple item record

dc.contributor.author Thompson, David W. J. (David William Jonathan) en_US
dc.date.accessioned 2009-10-07T00:48:24Z
dc.date.available 2009-10-07T00:48:24Z
dc.date.issued 2000 en_US
dc.identifier.other b45525225 en_US
dc.identifier.other 47109926 en_US
dc.identifier.other Thesis 50025 en_US
dc.identifier.uri http://hdl.handle.net/1773/10057
dc.description Thesis (Ph. D.)--University of Washington, 2000 en_US
dc.description.abstract The leading modes of variability of the extratropical circulation in both hemispheres are characterized zonally symmetric or "annular" structures. Whereas the structure and dynamics of the Southern Hemisphere (SH) annular mode have been extensively documented, the existence of an analogous structure in the Northern Hemisphere (NH) has not been recognized. In this thesis we compare the structure and seasonality of the NH and SH modes, document their signature in recent climate trends, and examine the regional climate impacts of the NH annular mode.The structures of the NH and SH annular modes are remarkably similar. Both are characterized by deep, nearly barotropic structures, with geopotential height perturbations of opposing sign in the polar cap region and in the surrounding ring centered near 45 degrees latitude. The annular modes also exhibit a distinctive signature in the tropics. They exist year round in the troposphere, but modulate the strength of the Lagrangian mean circulation in the lower stratosphere only during the "active" seasons for stratospheric planetary-wave-mean flow interaction. The North Atlantic Oscillation may be viewed as a regional expression of the Northern Hemisphere annular mode.The Northern Hemisphere annular mode has exhibited a trend over the past few decades that is clearly reflected in recent climate trends. Virtually all of the wintertime geopotential height falls over the polar cap region and the strengthening of the subpolar westerlies from the surface to the lower stratosphere, ∼30% of the wintertime warming over the NH, and ∼40% of the March total column ozone losses poleward of 40°N are attributable to the trend in the NH annular mode. The SH annular-mode has exhibited an analogous trend at stratospheric levels during the austral spring. Since the Northern Hemisphere annular mode affects the mean wintertime climate and the frequency of occurrence of weather events throughout the Northern Hemisphere, it is argued that its trend over the past few decades has influenced popular perceptions of climate change. en_US
dc.format.extent xii, 179 p. en_US
dc.language.iso en_US en_US
dc.rights.uri en_US
dc.subject.other Theses--Atmospheric sciences en_US
dc.title Annular modes in the atmospheric general circulation en_US
dc.type Thesis en_US


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search ResearchWorks


Advanced Search

Browse

My Account

Statistics