根据边界层高度和感热通量的关系，可知感热通量约占地面接收到的太阳直接辐射的30 % 。
According to the relation of the height of atmosphric boundary layer and sensible flux , it is attained that the sensible flux is about 30% of the solar radiation received by the ground.
近地面气温和边界层高度均更贴近实测值。由上述结果引出讨论了下垫面土地利用分类在模式模拟中的重要地位及其他可能原因。
The higher temperature centers appear in the downwind direction by the effects of surface wind fields. Surface temperature and PBL height are both closer to observation values.
近地面气温和边界层高度均更贴近实测值。由上述结果引出讨论了下垫面土地利用分类在模式模拟中的重要地位及其他可能原因。
The higher temperature centers appear in the downwind direction by the effects of surface wind fields. Surface temperature and PBL height are both closer to observation values.
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