The surface layer is a layer of the atmosphere that is several tens of meters above the earth's surface. Surface friction is dominant in this layer, and the influence of turning forces is small. The vertical distribution of wind speed in this layer is greatly influenced by the vertical distribution of temperature. Source : Heibonsha Encyclopedia About MyPedia Information |
接地境界層,等流速層とも。地表面から数十mまでの大気層。この層内の風では地表面摩擦が卓越し,転向力の影響は小さい。層内の風速の垂直分布は気温の垂直分布に大きく影響を受ける。
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