首页> 外文会议>Remote Sensing and Modeling of the Atmosphere, Oceans, and Interactions; Proceedings of SPIE-The International Society for Optical Engineering; vol.6404 >A Comparative Study of Air-Sea Exchange Coefficients and Turbulent fluxes over Indian Sub-continent and Korean Peninsula
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A Comparative Study of Air-Sea Exchange Coefficients and Turbulent fluxes over Indian Sub-continent and Korean Peninsula

机译:印度次大陆和朝鲜半岛海气交换系数和湍流通量的比较研究

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In this article, we describe the variation of air-sea exchange coefficients and air-sea interface fluxes over the East Asian marginal seas surrounding the Korean peninsula and compare them with the similar estimates reported for the tropical Indian Ocean. Surface layer meteorological observations for a period of about five years obtained from five oceanic buoys in the adjoining seas of Korean peninsula form the database for this study. Depending on the stability of the atmosphere, buoy data is classified into three categories - unstable, neutral and stable data. For unstable conditions, sensible and latent heat flux show good correlation with the wind speed, whereas it is not so for the neutral and stable condition. Irrespective of the stability of the atmosphere, momentum flux always shows a steady dependence on the varying wind speed. Sensible and latent heat fluxes also show good correlation with the difference between sea surface temperature and air temperature. Unlike the linear regression between the exchange coefficients and wind speeds reported for the Indian Ocean, we suggest second order and exponential fits for these exchange coefficients, which give better representation of their wind speed dependence. The results presented in this article form very useful input to the coupled ocean atmospheric models and the oceanic wave models, hence significant.
机译:在本文中,我们描述了围绕朝鲜半岛的东亚边缘海的空气-海洋交换系数和空气-海洋界面通量的变化,并将其与热带印度洋报道的相似估计值进行了比较。从朝鲜半岛毗连海中的五个海洋浮标获得的大约五年的表层气象观测资料构成了这项研究的数据库。根据大气的稳定性,浮标数据可分为三类-不稳定,中性和稳定数据。在不稳定的条件下,感热通量和潜热通量与风速具有良好的相关性,而在中性和稳定的条件下则不然。不管大气的稳定性如何,动量通量始终显示出对变化的风速的稳定依赖性。感热通量和潜热通量也与海表温度和气温之间的差异显示出良好的相关性。与印度洋所报道的交换系数和风速之间的线性回归不同,我们建议这些交换系数的二阶和指数拟合,以更好地表示它们的风速依赖性。本文介绍的结果为耦合的海洋大气模型和海浪模型提供了非常有用的输入,因此意义重大。

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