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- W1567991993 abstract "the middle reaches of the Heihe Rive r during the s ummer months based on the heat balance method. The rate of evaporation from irrigation canals depends on the temperature difference between canal water and air, the air humidity, and the wind speed. The present observations showed that the seasonal variations of the temperature diffe rence and the wind speed were not large in the observation peri od, and the seasonal variation of air h umidity had a large innuence on the evaporation rate. Since the Heihe Rive r rises from the Qilian Mountains and the river water is melt-water, the water temperature is rather low compared to the air temperatuJe. As a result, daily evaporation depth was often almost zero or negative. The resulLS of this study were obtained by applying the relationship be tween the heat transfer coefficients and the surface wind speed empirically der ived by :.iihara et al. (1959b), so the results are only approximate. Hence, these results s hould be verified against obse rvational evidence before a final conclusion can be drawn." @default.
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- W1567991993 date "2013-09-01" @default.
- W1567991993 modified "2023-10-07" @default.
- W1567991993 title "Evaporation from Irrigation Canals in the Middle Reaches of the Heihe River in the Northwest of China : A Preliminary Study" @default.
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- W1567991993 doi "https://doi.org/10.5109/27369" @default.
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