Affected by topography, they were strengthened by the foehn effect caused by west wind and the warm moisture accumulation before mountains caused by south wind.
受地形影响，偏西风造成的焚风效应和高压后部偏南风造成的暖湿空气在山前积聚，分别加剧了两类高温的强度。
Affected by topography, they were strengthened by the foehn effect caused by west wind and the warm moisture accumulation before mountains caused by south wind.
受地形影响，偏西风造成的焚风效应和高压后部偏南风造成的暖湿空气在山前积聚，分别加剧了两类高温的强度。
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