论文部分内容阅读
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 regional sea-atmosphere coupling model was used to simulate the sea conditions in the coastal region of East Asia from May to August in 1998. The coupled model simulates the Kuroshio current and the large-scale anticyclone vortex to its right. The simulations of the surface currents in the South China Sea are also basically consistent with the actual ones, and the characteristics of the South China Sea currents are greatly influenced by the monsoon. The model also simulates the sudden warming of the SST and the North Pushing Process in the warm water region with the onset and advancement of the Southwest Monsoon. This opens up a new way for the research on the regional climate change and the regional sea-air interaction.