Dynamic and numerical methods are used to discuss the atmospheric response imposed by SST thermal forcing.
用动力分析和数值计算的方法讨论了大气对海温热力强迫的响应。
For synoptic scale systems, the SST thermal forcing mainly excites the atmospheric low-frequency oscillation.
对于天气尺度系统，海温热力场则主要激发出大气低频振荡。
For synoptic scale systems, the SST thermal forcing mainly excites the atmospheric low - frequency oscillation.
对于天气尺度系统，海温热力场则主要激发出大气低频振荡。
At this frequency band EU and ea teleconnection patterns can be excited by the thermal forcing of the variation of the sea ice cover.
在这一频带上，海冰面积变化的热力强迫作用可分别激发出EU和EA大气遥相关型。
The total heating field and the components, their vertical and horizontal distribution characteristics can be used for some numerical experiment in the designs of thermal forcing.
本文所得到的日平均总加热场和各分量场的水平和垂直分布特征，有助于对夏季平均气候场形成机制的理解并可供数值试验中设计固定加热场时参考。
The differences between results of simulations with different equilibrium temperatures reflect the effects of local thermal forcing on the anomalous response of the global circulations.
本文对不同平衡温度模拟结果的差异(偏差场)进行了分析，探讨某局地热力强迫对全球其它区域环流异常的影响效应。
In this paper, with a view to the effect of sea-land thermal forcing contrast in East Asian, the early summer circulation in East Asia and Meiyu cause of formation in Jianghuai valley are studied.
着眼于东亚海陆热力强迫差异的影响，探讨了东亚初夏环流与江淮梅雨成因。
In this paper, with a view to the effect of sea-land thermal forcing contrast in East Asian, the early summer circulation in East Asia and Meiyu cause of formation in Jianghuai valley are studied.
着眼于东亚海陆热力强迫差异的影响，探讨了东亚初夏环流与江淮梅雨成因。
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