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Coupling effect between thermal and dynamic factors on water surface evaporation and in-situ observation

机译:水面蒸发和原位观测水表蒸发与动力学因素的耦合效应

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Water surface evaporation is an important indicator of atmospheric circulation and hydrological cycle. This paper, after selecting representative alluvial plain in north of Haihe River Basin as the experimental point, designs in-situ observation experiment to explore the influence of wind speed on water surface evaporation and puts forward the coupling effect between thermal and air dynamic factors on evaporation, which refers to that actual evaporation is not only depended on the values of thermal factor and dynamic factor, but also on the correlation of the two factors. The observed data show that, the main factors influencing actual evaporation in experimental area are daily average air temperature and wind speed and the two variables are separately the main representation of thermal factor and air dynamic factor. It is proved that there is significant coupling effect between daily average temperature and wind speed on observed evaporation. At last, Penman Formula is analyzed to explore the theoretical evidence of the coupling effect, it is concluded that the structure of Penman Formula should be revised later to further characterize the coupling effect between thermal and air dynamic factors on evaporation. As a whole, coupling effect is a basic principle in evaporation, which could be the reference to explain “Evaporation Paradox”.
机译:水面蒸发是大气循环和水文循环的重要指标。本文在沿海河河北北部选择代表性的冲积平原之后作为实验点,设计原位观察实验,探讨风速对水面蒸发的影响,并提出了热和空气动力因素对蒸发的耦合效应这是指实际蒸发不仅依赖于热因子和动态因子的值,而且还取决于两个因素的相关性。观察到的数据表明,影响实验区中实际蒸发的主要因素是每日平均空气温度和风速,两个变量是分别的热因子和空气动力因子的主要表示。事实证明,在观察到的蒸发方面,每日平均温度和风速之间存在显着的耦合效应。最后,分析了Penman公式以探索耦合效果的理论证据,得出结论,稍后应修改Penman公式的结构,以进一步表征热和空气动力因子之间的耦合效应。蒸发。整体而言,耦合效果是蒸发的基本原理,这可能是解释&#x201c的参考;蒸发悖论”

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