Predictability of SST-Modulated Westerly Wind Bursts

被引:48
作者
Gebbie, Geoffrey [1 ,2 ]
Tziperman, Eli [2 ]
机构
[1] Harvard Univ & Massachusetts Inst Technol, Cambridge, MA USA
[2] Harvard Univ, Dept Earth & Planetary Sci, Sch Engn & Appl Sci, Cambridge, MA 02138 USA
基金
美国国家科学基金会;
关键词
NINO-SOUTHERN-OSCILLATION; EL-NINO; TROPICAL PACIFIC; EQUATORIAL PACIFIC; ENSO; MODEL; VARIABILITY; CLIMATE;
D O I
10.1175/2009JCLI2516.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Westerly wind bursts (WWBs), a significant player in ENSO dynamics, are modeled using an observationally motivated statistical approach that relates the characteristics of WWBs to the large-scale sea surface temperature. Although the WWB wind stress at a given location may be a nonlinear function of SST, the characteristics of WWBs are well described as a linear function of SST. Over 50% of the interannual variance in the WWB likelihood, zonal location, duration, and fetch is explained by changes in SST. The model captures what is seen in a 17-yr record of satellite-derived winds: the eastward migration and increased occurrence of wind bursts as the western Pacific warm pool extends. The WWB model shows significant skill in predicting the interannual variability of the characteristics of WWBs, while the prediction skill of the WWB seasonal cycle is limited by the record length of available data. The novel formulation of the WWB model can be implemented in a stochastic or deterministic mode, where the deterministic mode predicts the ensemble-mean WWB characteristics. Therefore, the WWB model is especially appropriate for ensemble prediction experiments with existing ENSO models that are not capable of simulating realistic WWBs on their own. Should only the slowly varying component of WWBs be important for ENSO prediction, this WWB model allows a shortcut to directly compute the slowly varying ensemble-mean wind field without performing many realizations.
引用
收藏
页码:3894 / 3909
页数:16
相关论文
共 37 条
[31]  
2
[32]  
TZIPERMAN E, 1988, J PHYS OCEANOGR, V18, P506, DOI 10.1175/1520-0485(1988)018<0506:CITELB>2.0.CO
[33]  
2
[34]   Quantifying the dependence of westerly wind bursts on the large-scale tropical pacific SST [J].
Tziperman, Eli ;
Yu, Lisan .
JOURNAL OF CLIMATE, 2007, 20 (12) :2760-2768
[35]   Reassessing the role of stochastic forcing in the 1997-1998 El Nino [J].
Vecchi, GA ;
Wittenberg, AT ;
Rosati, A .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (01)
[36]   GFDL's CM2 global coupled climate models. Part III: Tropical pacific climate and ENSO [J].
Wittenberg, AT ;
Rosati, A ;
Lau, NC ;
Ploshay, JJ .
JOURNAL OF CLIMATE, 2006, 19 (05) :698-722
[37]   Case analysis of a role of ENSO in regulating the generation of westerly wind bursts in the Western Equatorial Pacific [J].
Yu, LS ;
Weller, RA ;
Liu, WT .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2003, 108 (C4)