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利用高分辨率的全球大气环流-海浪耦合模式进行了大气环流季节循环的集合模拟,通过与欧洲中期预报中心再分析资料的比较,表明耦合模式可以有效地改进海面气压场的模拟,这种改进得益于考虑了波浪所产生的波生应力.同时,耦合试验结果也清楚地表明了中纬度大气对于海表热通量强迫表现为“热-低压”的响应形式,增进了对中纬度大气对于海洋强迫响应的理解.
A set simulation of the seasonal circulation of the general circulation is carried out by using the high-resolution global atmosphere-ocean-ocean coupling model. The comparison with the reanalysis data of the European Center for Medium-Range Forecast shows that the coupling mode can effectively improve the simulation of the sea surface pressure field. Due to the consideration of the wave-induced stress generated by waves.At the same time, the results of the coupling experiment clearly show that the mid-latitude atmospheric response to the heat flux forced to sea surface is “hot-low pressure” Understanding of forced ocean response.