Go to  Advanced Search

Nonlinear Northern Hemisphere winter atmospheric response to ENSO

Show full item record

Files in this item

Files Size Format Description   View
Hsieh_AGU_2004_2003GL018885.pdf 3.500Mb Adobe Portable Document Format   View/Open
Title: Nonlinear Northern Hemisphere winter atmospheric response to ENSO
Author: Wu, Aiming; Hsieh, William W.
Issue Date: 2004-01-16
Publicly Available in cIRcle 2011-03-24
Publisher American Geophysical Union
Citation: Wu, Aiming, Hsieh, William W. 2004. Nonlinear Northern Hemisphere winter atmospheric response to ENSO. Geophysical Research Letters, 31 L02203 dx.doi.org/10.1029/2003GL018885.
Abstract: A nonlinear projection of the tropical Pacific sea surface temperature anomalies (SSTA) onto the Northern Hemisphere winter 500-mbar geopotential height (Z500) by a neural network reveals asymmetric atmospheric patterns associated with El Niño and La Niña. While the linear response of Z500 to tropical Pacific SSTA is largely confined over North Pacific and North America, the nonlinear response, mainly a quadratic response to the SSTA, reveals that regardless of the sign of the SSTA, positive Z500 anomalies are found over the central-eastern North America, North Atlantic and western Europe, and negative Z500 anomalies over the west coast of North America, Scandinavia and eastern Europe—consistent with the positive Pacific-North America (PNA) teleconnection pattern and the positive North Atlantic Oscillation (NAO) pattern being excited. An edited version of this paper was published by AGU. Copyright 2004 American Geophysical Union.
Affiliation: Earth and Ocean Sciences, Dept. of (EOS), Dept of
URI: http://hdl.handle.net/2429/32865
Peer Review Status: Reviewed
Scholarly Level: Faculty

This item appears in the following Collection(s)

Show full item record

All items in cIRcle are protected by copyright, with all rights reserved.

UBC Library
1961 East Mall
Vancouver, B.C.
Canada V6T 1Z1
Tel: 604-822-6375
Fax: 604-822-3893