Roles of different physical processes in upper ocean responses to Typhoon Rammasun (2008)-induced wind forcing
Autor: | Dake Chen, Yuhua Pei, Rong-Hua Zhang |
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Rok vydání: | 2019 |
Předmět: |
010504 meteorology & atmospheric sciences
Mixed layer Wind stress Ocean general circulation model 010502 geochemistry & geophysics Atmospheric sciences 01 natural sciences Wind speed Sea surface temperature Heat flux Typhoon General Earth and Planetary Sciences Environmental science Tropical cyclone 0105 earth and related environmental sciences |
Zdroj: | Science China Earth Sciences. 62:684-692 |
ISSN: | 1869-1897 1674-7313 |
DOI: | 10.1007/s11430-018-9313-8 |
Popis: | This study investigates the roles of different physical processes in the oceanic response to tropical cyclones (TCs) in the Pacific, using an ocean general circulation model with several numerical experiments. A case study is focused on Typhoon Rammasun, which passed through the northwestern tropical Pacific in May 2008. TC-induced wind stress fields are extracted using a locally-weighted regression (Loess) method from a six-hourly Cross-Calibrated Multi-Platform satellite scatterometer wind product. By comparing model experiments with TC wind forcing being explicitly included or not, the effects of TC on the ocean are isolated in a clean way. The local oceanic response is characterized by a cooling in the surface layer that persists along the typhoon track as a cold wake, and a deepening of the mixed layer (ML). The TC-induced wind can affect the ocean through the momentum effects, the ML processes (the stirring effect on the ML depth), and heat flux (via wind speed), repectively. Analyses of numerical experiments with these different underlying processes explicitly represented or not indicate that vertical mixing and upwelling are dominant processes responsible for surface cooling, while the surface heat flux also plays a non-negligible role. Specifically, vertical mixing, upwelling and surface heat flux account for respectively ~53%, ~31% and ~16% of the sea surface temperature cooling. However, for the ML response, the vertical mixing and surface heat flux are dominant processes for the ML deepening, while the contribution from upwelling process is negligible. This study provides new insights into how TC-indcued wind forcing affects the ocean by isolating each different individual process in a clear way, which differs from previous direct heat budget analyses. |
Databáze: | OpenAIRE |
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