期刊
JOURNAL OF PHYSICAL OCEANOGRAPHY
卷 48, 期 8, 页码 1651-1674出版社
AMER METEOROLOGICAL SOC
DOI: 10.1175/JPO-D-17-0132.1
关键词
Model evaluation; performance; Ocean models; Primitive equations model
类别
资金
- National Key Research and Development Program of China [2017YFC1404103]
- National Natural Science Foundation of China [41676088, 41606039]
- National Programme on Global Change and Air-Sea Interaction of China [GASI-01-01-12, GASI-IPOVAI-04]
- U.S. Office of Naval Research
Langmuir turbulence (LT) due to the Craik-Leibovich vortex force had a clear impact on the thermal response of the ocean mixed layer to Supertyphoon Haitang (2005) east of the Luzon Strait. This impact is investigated using a 3D wave-current coupled framework consisting of the Princeton Ocean Model with the generalized coordinate system (POMgcs) and the Simulating Waves Nearshore (SWAN) wave model. The Coriolis-Stokes forcing (CSF), the Craik-Leibovich vortex forcing (CLVF), and the second-moment closure model of LT developed by Harcourt are introduced into the circulation model. The coupled system is able to reproduce the upper-ocean temperature and surface mixed layer depth reasonably well during the forced stage of the supertyphoon. The typhoon-induced cold suction and heat pump processes are significantly affected by LT. Local LT mixing strengthened the sea surface cooling by more than 0.5 degrees C in most typhoon-affected regions. Besides LT, Lagrangian advection of temperature also modulates the SST cooling, inducing a negative (positive) SST difference in the vicinity of the typhoon center (outside of the cooling region). In addition, CLVF has the same order of magnitude as the horizontal advection in the typhoon-induced strong-vorticity region. While the geostrophy is broken down during the forced stage of Haitang, CLVF can help establish and maintain typhoon-induced quasigeostrophy during and after the typhoon. Finally, the effect of LT on the countergradient turbulent flux under the supertyphoon is discussed.
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