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dc.contributor.authorVecchi, Gabriel Andrésen_US
dc.date.accessioned2009-10-07T02:59:37Z
dc.date.available2009-10-07T02:59:37Z
dc.date.issued2000en_US
dc.identifier.otherb45145246en_US
dc.identifier.other46452850en_US
dc.identifier.otherThesis 49540en_US
dc.identifier.urihttp://hdl.handle.net/1773/11046
dc.descriptionThesis (Ph. D.)--University of Washington, 2000en_US
dc.description.abstractThe role of sub-seasonal western and central Pacific surface zonal wind variability in the evolution of El Nino sea surface temperature anomaly (SSTA) is examined. The surface wind structure and atmospheric convection variability of tropical Pacific westerly wind events (WWEs) is described. The average tropical Pacific SSTA variability following and in the absence of equatorial WWEs is examined over the period 1986--1998. The surface wind structure of the Madden-Julian Oscillation is examined (MJO), along with relationships between the MJO and WWEs. The response of an ocean general circulation model (OGCM) to composite MJO and WWE surface wind stress forcing is explored.WWEs can be classified into eight types based on the location of the maximum zonal wind anomalies. WWEs are found to be compact in space and time, exhibiting little translation during their lifetime. Typical scales for WWEs are derived over the period 1986--1995. It is found that certain WWE types exhibit significant seasonality, and some have a significant correlation with the Troup Southern Oscillation Index.In the absence of equatorial WWEs, tropical Pacific SSTA tends to remain at or return towards climatology. Following equatorial WWEs, tropical Pacific SSTA warms towards or remains at El NiNo type conditions.WWEs are significantly associated with atmospheric convection. The MJO surface wind stress anomaly fields exhibit two regimes in the equatorial Pacific. In the western equatorial Pacific there are both easterly and westerly anomalies with the westerlies dominating, in the central and eastern equatorial Pacific the main anomalies are easterlies. The WWEs which occur during the MJO are modulated by the convective variability of the MJO. West-of-dateline WWEs exhibit a strong relationship to tropical cyclone activity.Following a composite MJO, the tropical Pacific SSTA in the OGCM does not tend to warm; the composite MJO does not provide a simple mechanism for El Nino waveguide warming. Idealized WWEs drove tropical Pacific SSTA warming in the OGCM; enhanced WWE activity provides a mechanism for the onset of El Nino.en_US
dc.format.extentix, 187 p.en_US
dc.language.isoen_USen_US
dc.rightsCopyright is held by the individual authors.en_US
dc.rights.urien_US
dc.subject.otherTheses--Oceanographyen_US
dc.titleSub-seasonal wind variability and El Niñoen_US
dc.typeThesisen_US


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