local thermal forcing 局域热源强迫
localized thermal forcing 局地热力强迫
anomalous thermal forcing 热力异常
atmospheric thermal forcing 大气热力强迫
orographically thermal forcing 地形热力强迫
axis-symmetric thermal forcing 轴对称热力强迫
While thermal forcing plays an important role in the process of summertime AO formation and maintenance, wintertime AO is subject to the dynamic process. This is probably the radical cause of the seasonal discrepancy of AO.
因此热力强迫作用在夏季北极涛动的形成和维持机制中占重要地位，而冬季北极涛动的维持机制主要是动力作用的结果，热力作用只在对流层低层起作用，这也是二者空间模态和结构差异的主要原因。
参考来源 - 北极涛动的季节性差异及其结构机理研究·2,447,543篇论文数据，部分数据来源于NoteExpress
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。
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