Modulation of Westerly Wind Bursts by Sea Surface Temperature: A Semistochastic Feedback for ENSO
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- 1 September 2007
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 64 (9) , 3281-3295
- https://doi.org/10.1175/jas4029.1
Abstract
Westerly wind bursts (WWBs) in the equatorial Pacific are known to play a significant role in the development of El Niño events. They have typically been treated as a purely stochastic external forcing of ENSO. Recent observations, however, show that WWB characteristics depend upon the large-scale SST field. The consequences of such a WWB modulation by SST are examined using an ocean general circulation model coupled to a statistical atmosphere model (i.e., a hybrid coupled model). An explicit WWB component is added to the model with guidance from a 23-yr observational record. The WWB parameterization scheme is constructed such that the likelihood of WWB occurrence increases as the western Pacific warm pool extends: a “semistochastic” formulation, which has both deterministic and stochastic elements. The location of the WWBs is parameterized to migrate with the edge of the warm pool. It is found that modulation of WWBs by SST strongly affects the characteristics of ENSO. In particular, coupled fe... Abstract Westerly wind bursts (WWBs) in the equatorial Pacific are known to play a significant role in the development of El Niño events. They have typically been treated as a purely stochastic external forcing of ENSO. Recent observations, however, show that WWB characteristics depend upon the large-scale SST field. The consequences of such a WWB modulation by SST are examined using an ocean general circulation model coupled to a statistical atmosphere model (i.e., a hybrid coupled model). An explicit WWB component is added to the model with guidance from a 23-yr observational record. The WWB parameterization scheme is constructed such that the likelihood of WWB occurrence increases as the western Pacific warm pool extends: a “semistochastic” formulation, which has both deterministic and stochastic elements. The location of the WWBs is parameterized to migrate with the edge of the warm pool. It is found that modulation of WWBs by SST strongly affects the characteristics of ENSO. In particular, coupled fe...Keywords
This publication has 37 references indexed in Scilit:
- Westerly Wind Bursts: ENSO’s Tail Rather than the Dog?Journal of Climate, 2005
- Characteristics of Stochastic Variability Associated with ENSO and the Role of the MJOJournal of Climate, 2005
- Tracer Conservation with an Explicit Free Surface Method forz-Coordinate Ocean ModelsMonthly Weather Review, 2001
- Understanding and predicting ENSOReviews of Geophysics, 1995
- Effects of westerly wind bursts upon the western equatorial Pacific Ocean, February–April 1991Journal of Geophysical Research: Oceans, 1993
- An Intercomparison of Methods for Finding Coupled Patterns in Climate DataJournal of Climate, 1992
- Isopycnal Mixing in Ocean Circulation ModelsJournal of Physical Oceanography, 1990
- Dynamics and Thermodynamics of a Warming Event in a Coupled Tropical Atmosphere–Ocean ModelJournal of the Atmospheric Sciences, 1988
- Remote westerly wind forcing of the eastern equatorial Pacific; Some model resultsGeophysical Research Letters, 1988
- Kelvin-Wave-Induced Anomalous Advection and the Onset of Surface Warming in El Niño EventsMonthly Weather Review, 1984