这一段的锢囚锋和高空暖舌带来与极地空气团天气相反的变化。
The passage is an occluded front and trowal brings a change back to polar air-mass weather.
因此，在一些天气图上，它的位置会单独标识，加拿大气象学家称之为高空暖舌。
Hence its position is indicated separately on some weather maps and it is referred to by Canadian meteorologists as a trowal.
数值实验结果表明：西暖舌是由黄海暖流形成的，而黄海暖流由于冬季季风海流的补偿作用而得到加强。
Numerical experiments based on POM are carried out to study the forming mechanism of this thermal structure and its relation to the Yellow Sea Warm Current (YSWC).
提出SPCZ是反映西太暖池同东太冷舌海气耦合系统以及暖池大气同相邻陆区大气间相互作用的重要特征。
It can be said that the SPCZ represents the air-sea system interaction of the Western Pacific Warm Pool (WPWP) and the eastern Pacific cold tongue, as well as the interaction of.
提出SPCZ是反映西太暖池同东太冷舌海气耦合系统以及暖池大气同相邻陆区大气间相互作用的重要特征。
It can be said that the SPCZ represents the air-sea system interaction of the Western Pacific Warm Pool (WPWP) and the eastern Pacific cold tongue, as well as the interaction of.
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