Kalpakkam沿海区域大气-海洋耦合自动模拟系统的开发

S. Bonthu, K. Sasmal, H. Warrior, Subhendu Maity
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引用次数: 5

摘要

本文报道了应用于区域大气-海洋耦合模式(RCAOM)的自动通量耦合机制的发展。耦合器作为两个最先进的模式,即先进天气研究和预报模式(WRF)和普林斯顿海洋模式(POM)之间的接口。它对海表温度、海表环流等海况预报研究具有直接意义。RCAOM模拟了印度东海岸Kalpakkam沿岸的上升流等局部过程,也用于观察马德拉斯核电站(MAPS)和原型快速增殖反应堆(PFBR)两座核电站冷却码头入口位置的热再循环。模拟结果表明,由于逆风系统和热流交换的作用,MAPS和PFBR的进风口位置温度升高;其次,在没有热排放的情况下,由于地形诱导效应,在出风口位置出现了上升流。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of an Automated Regional Coupled Atmosphere-Ocean Modeling System for Coastal Kalpakkam
In this paper the development of an automated flux coupling mechanism applied to a Regional Coupled Atmosphere-Ocean Model (RCAOM) is reported. The coupler serves as an interface between two state-of-the-art models viz. Advanced Weather Research and Forecasting Model (WRF) and Princeton Ocean Model (POM). It has direct significance for ocean state forecasting studies such as prediction of sea-surface temperature (SST), surface circulations etc. RCAOM simulates local processes like upwelling along coastal Kalpakkam situated on the east coast of India and is also used to observe thermal recirculation at intake locations of cooling Jetties for the two nuclear power plants, Madras Atomic Power Plant (MAPS) and Prototype Fast Breeder Reactor (PFBR). The simulations reveal that the rise of temperature at intake locations of MAPS and PFBR occurs due to reversal wind system and exchange of heat fluxes and secondly upwelling is observed at the outfall location due to topographically induced effect in the absence of thermal discharge.
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