Northern hemisphere storm tracks in strong AO anomaly winters

Northern Hemisphere winter 300 hPa storm tracks/baroclinic waves and their energetics during strong Arctic Oscillation (AO) anomaly events are investigated. It is shown that during strong positive AO anomaly winters, the Atlantic storm track intensifies significantly and shifts northward and far dow...

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Bibliographic Details
Published in:Atmospheric Science Letters
Main Authors: Nie, Ji, Wang, Peng, Yang, Wenchang, Tan, Benkui
Other Authors: Nie, J (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China., Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: atmospheric science letters 2008
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Online Access:https://hdl.handle.net/20.500.11897/148978
https://doi.org/10.1002/asl.186
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Summary:Northern Hemisphere winter 300 hPa storm tracks/baroclinic waves and their energetics during strong Arctic Oscillation (AO) anomaly events are investigated. It is shown that during strong positive AO anomaly winters, the Atlantic storm track intensifies significantly and shifts northward and far downstream while Pacific storm track extends westward. Baroclinic waves over the Atlantic propagate along central North Atlantic during strong negative AO anomaly winters while during strong positive AO anomaly winters, waves over the Atlantic split into two branches. Distributions of the kinetic energy and energy conversions of different spatial scale over the storm track regions assume different characteristics for different AO phases. Copyright (c) 2008 Royal Meteorological Society http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000263860700008&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geochemistry & Geophysics Meteorology & Atmospheric Sciences SCI(E) 9 ARTICLE 3 153-159 9