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.
夏季盛行南风气流，随着城市热岛效应的增强，发生在北部近郊区的弱降水天气过程趋于增多。
However, in summer when the prevailing flow is southern wind, the strengthening UHI is advantageous for occurring weak precipitation in northern suburb.
夏季盛行南风气流，随着城市热岛效应的增强，发生在北部近郊区的弱降水天气过程趋于增多。
However, in summer when the prevailing flow is southern wind, the strengthening UHI is advantageous for occurring weak precipitation in northern suburb.
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