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，低空偏南風急流左側和地面冷峰西端的南側或準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.
高空西風槽和南支槽及其前側的副熱帶急流和低空強西南氣流及準靜止切變線是誘發(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.
以一個在陸上長久維持并最終演變成溫帶氣旋的登陸臺風“麥莎”為研究對象，通過對其北上變性過程的分析發(fā)現(xiàn)，臺風與中高緯西風槽的相互作用使得冷空氣侵入是其變性加強的原因。