Seasonal variability of thermocline

时间:2023-05-01 13:14:40 天文地理论文 我要投稿
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Seasonal variability of thermocline in the Yellow Sea

Based on the MASNUM wave-tide-circulation coupled numerical model, seasonal variability of thermocline in the Yellow Sea was simulated and compared with in-situ observations. Both simulated mixed layer depth (MLD) and thermocline intensity have similar spatial patterns to the observations. The simulated maximum MLD are 8 m and 22 m, while the corresponding observed values are 13 m and 27 m in July and October, respectively. The simulated thermocline intensity are 1.2℃/m and 0.5℃/m in July and October,respectively, which are 0.6℃/m less than those of the observations. It may be the main reason why the simulated thermocline is weaker than the observations that the model vertical resolution is less precise than that of the CTD data which is 1 m. Contours of both simulated and observed thermocline intensity present a circle in general. The wave-induced mixing plays a key role in the formation of the upper mixed layer in spring and summer. Tidal mixing enhances the thermocline intensity. Buoyancy-driven mixing destroys the thermocline in autumn and keeps the vertical temperature uniform in winter.

作 者: 乔方利 夏长水 施建伟 马建 葛人峰 袁业立   作者单位: 乔方利,夏长水,马建,葛人峰,袁业立(The First Institute of Oceanography, State Oceanic Administration (SOA), Qingdao 266061, China;Key Laboratory of Marine Science and Numerical Modeling (MASNUM), SOA, Qingdao 266061, China)

施建伟(Guest Researcher of MASNUM, SOA, China) 

刊 名: 中国海洋湖沼学报(英文版)  ISTIC SCI 英文刊名: CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY  年,卷(期): 2004 22(3)  分类号:   关键词: thermocline   the Yellow Sea   wave-tide-circulation coupled model   wave-induced mixing   tidal mixing  

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