区域海气耦合模式对1998年5~8月东亚近海海况的模拟研究  被引量:9

Numerical Simulation of Oceanic Elements at East Asian Coastal Oceans from May to August in 1998 by using a Coupled Regional Ocean-Atmosphere Model

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作  者:任雷娟 钱永甫[1] 

机构地区:[1]南京大学大气科学系,南京210093

出  处:《气候与环境研究》2000年第4期482-485,共4页Climatic and Environmental Research

基  金:国家科技部攀登项目A"南海季风试验研究"资助

摘  要:采用区域海气耦合模式对1998年5~ 8月东亚近海海况进行了模拟研究。耦合模式模拟出了黑潮海流及其右侧的大尺度反气旋式涡旋,对南海表层海流的模拟也与实际基本相符,并模拟出了南海海流受季风影响较大的特点。模式也模拟出了伴随西南季风爆发及推进而发生的海温突增及暖水区北推过程。这为进行区域气候变化与区域海气相互作用问题的研究开辟了一条新途径。The oceanic elements at East Asian coastal oceans from May to August in 1998 are simulated by using a coupled regional ocean-atmosphere model developed in this Paper. The Kuroshio current and the large-scale anticyclonic vortex to its right are simulated by this coupled model. The simulated surface currents of the SCS which are greatly influenced by the monsoon are also basically consistent with the reality. The sudden increase of SST and the northward expending process of warm water region accompanied with the onset of summer monsoon are fairly modeled by the coupled model. This is a new way to study the issues of regional climate change and regional air-sea interaction.

关 键 词:海气耦合模式 1998年 模拟研究 海况 近海 东亚 海气相互作用 区域气候变化 模式模拟 表层海流 季风爆发 反气旋 大尺度 暖水区 南海 涡旋 黑潮 海温 

分 类 号:P732.6[天文地球—海洋科学] S157.1[农业科学—土壤学]

 

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