Torridity, humidity, raininess are the major climatic characteristics of the YunNan hot-moist area.
炎热、潮湿、多雨是云南湿热地区的主要气候特征。
When the hurricane moves into this large-scale cool, dry, air-descending area, its moist, warm upwelling air is countered by it, and so it weakens.
当飓风来到这一大片低温、干燥并且空气呈现下降趋势的地区时,它所携带的温暖、潮湿而有上升趋势的空气就会与此反作用,从而使得飓风减弱。
Similarly, when a pipeline transverses moist clay areas adjacent to dry loam, steel surfaces in the wet area become anodic to steel surfaces in the dry area.
与此相似,当管道通过与干亚粘土接壤的湿粘土区时,湿粘土区钢表面相对于干土区钢表面为阳极。
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