Physical mechanism and numerical simulations of surface layer temperature inversion in tropical ocean

The one-dimensional Kraus-Tumer mixed layer model improved by Liu is developed to consider the effect of salinity and the equations of temperature and salinity under the mixed layer. On this basis, the processes of growth and death of surface layer temperature inversion is numerically simulated under different environmental parameters. At the same time, the physical mechanism is preliminarily discussed combining the observations at the station of TOGA-COARE 0°N, 156°E. The results indicate that temperature inversion sensitively depends on the mixed layer depth, sea surface wind speed and solar shortwave radiation, etc., and appropriately meteorological and hydrological conditions often lead to the similarly periodical occurrence of this inversion phenomenon.

作 者： FAN Haimei LI Bingrui ZHANG Qinghua LIU Zhiliang   作者單位： FAN Haimei(Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266003, China;Key Laboratory of Marine Science and Numerical Modeling of State Oceanic Administration, Qingdao 266061, China)

LI Bingrui(Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266003, China)

ZHANG Qinghua(Key Laboratory of Marine Science and Numerical Modeling of State Oceanic Administration, Qingdao 266061, China)

LIU Zhiliang(Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China) 

刊 名： 海洋學(xué)報(bào)（英文版）  SCI 英文刊名： ACTA OCEANOLOGICA SINICA  年，卷(期)： 2005 24(3)  分類號(hào)： P7  關(guān)鍵詞： surface layer temperature inversion   barrier layer   mixed layer depth   sea surface wind speed   solar shortwave radiation  

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