upper-level trough

基本解釋

They form in the upper-level trough, in the left side of the lower-level jet, and in the surface pre-frontal area.
它們發(fā)生在高空小槽底部，低空偏南風(fēng)急流左側(cè)和地面冷峰西端的南側(cè)或準(zhǔn)靜止鋒上的曖濕輻合區(qū)中。
qk.cams.cma.gov.cn
The main influencing weather systems are: upper-level westerly trough, southern branch trough, subtropical jet, strong low-level southwest jet and quasi-stationary shear line.
高空西風(fēng)槽和南支槽及其前側(cè)的副熱帶急流和低空強(qiáng)西南氣流及準(zhǔn)靜止切變線是誘發(fā)福建省春季冰雹最主要的天氣系統(tǒng)。
Through the analysis, it is shown that the Matsa s extratropical transition and the re-intensification are due to the intrusion of cold air from the upper-level trough into the typhoons circulation.
以一個(gè)在陸上長(zhǎng)久維持并最終演變成溫帶氣旋的登陸臺(tái)風(fēng)“麥莎”為研究對(duì)象，通過對(duì)其北上變性過程的分析發(fā)現(xiàn)，臺(tái)風(fēng)與中高緯西風(fēng)槽的相互作用使得冷空氣侵入是其變性加強(qiáng)的原因。