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Numerical Simulation of Boundary Layer Structure and Cross-Equatorial Flow in the Eastern Pacific

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  • Recent observations from spaceborne microwave sensors have revealed detailed structure of the surface flow over the equatorial eastern Pacific in the boreal fall season. A marked acceleration of surface wind across the northern sea surface temperature (SST) front of the cold tongue is a prominent feature of the regional climate. Previous studies have attributed the acceleration to the effect of enhanced momentum mixing over the warmer waters. A high-resolution numerical model is used to examine the cross-frontal flow adjustment. In a comprehensive comparison, the model agrees well with many observed features of crossequatorial flow and boundary layer structure from satellite, Tropical Atmosphere Ocean (TAO) moorings, and the recent Eastern Pacific Investigation of Climate Processes (EPIC) campaign. In particular, the model simulates the acceleration across the SST front, and the change from a stable to unstable boundary layer. Analysis of the model momentum budget indicates that the hydrostatic pressure gradient, set up in response to the SST gradient, drives the surface northward acceleration. Because of thermal advection by the mean southerly flow, the pressure gradient is located downstream of the SST gradient and consequently, divergence occurs over the SST front, as observed by satellite. Pressure gradients also act to change the vertical shear of the wind as the front is crossed. However, the model underpredicts the changes in vertical wind shear across the front, relative to the EPIC observations. It is suggested that the vertical transfer of momentum by mixing, a mechanism described by Wallace et al. may also act to enhance the change in shear in the observations, but the model does not simulate this effect. Reasons for this are discussed.
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  • Small, R. Justin, Shang-Ping Xie, Yuqing Wang, Steven K. Esbensen, Dean Vickers, 2005: Numerical Simulation of Boundary Layer Structure and Cross-Equatorial Flow in the Eastern Pacific. Journal of the Atmospheric Sciences, 62(6), 1812–1830.
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  • 62
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  • 6
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  • This study is supported by NASA Grant NAG-10045 and JPL Contract 1216010, NOAA Grant NA17RJ1230, NSF Grant ATM01-04468 and ATM00-02322, and the Japan Agency for Marine– Earth Science and Technology.
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