风沿斜坡往上吹的为迎风坡。由于地形对气候的影响,山地的迎风坡和背风坡常形成不同的自然环境,进而形成了不同的人文环境。
迎风坡空气抬升,背风坡空气下沉。
结果表明:新月型沙丘迎风坡基本处于风蚀过程;
The result showed: windward slopes of crescent dune are basically in the process of wind erosion.
此外,台风降雨的落区主要是山区,降水形式是迎风坡降水的特征。
In addition, rainfall is almost distributed in mountain area, and performs the precipitation in the windward slope.
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