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STUDY ON EVAPOTRANSPIRATION AND ITS IMPACT FACTORS OVER YELLOW RIVER UPPER STREAM AREA

Shi Xing-he

Open publisher page 6 citations

Abstract

By using of Penman formula, the authors calculated the evapotranspiration since 1980s, and analyzed the variation tendency of some climatic factors such as evapotranspiration, sunshine duration, air temperature, air saturation deficit etc, and focused on their impact to the evapotranspiration. The results show that the evapotranspiration is increasing annually with the speed of 3.25 mm over Yellow River upper stream area;while the sunshine duration which is considered as main impact factor, is increasing with the speed of 3.6 h/a;air temperature is appearing the increasing tendency, and its climatic tendency is 0.4 ℃ /10 a; air saturation deficit is increasing with 0.02 hPa/a. Therefore, we could think that the evapotranspiration is greatly increasing as increment of sunshine duration and air temperature deficit over Yellow River upper stream area. But the increment of evapotranspiration and decrement of precipitation amount impact directly on the decrement of flow curve and expanding of grassland's desertization over Yellow River upper stream.

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What this paper is about

By using of Penman formula, the authors calculated the evapotranspiration since 1980s, and analyzed the variation tendency of some climatic factors such as evapotranspiration, sunshine duration, air temperature, air saturation deficit etc, and focused on their impact to the evapotranspiration. The results show that the evapotranspiration is increasing annually with the speed of 3.25 mm over Yellow River upper stream area;while the sunshine duration which is considered as main impact factor, is increasing with the speed of 3.6 h/a;air temperature is appearing the increasing tendency, and its climatic tendency is 0.4 ℃ /10 a; air saturation deficit is increasing with 0.02 hPa/a. Therefore, we could think that the evapotranspiration is greatly increasing as increment of sunshine duration and air temperature deficit over Yellow River upper stream area. But the increment of evapotranspiration and decrement of precipitation amount impact directly on the decrement of flow curve and expanding of grassland's desertization over Yellow River upper stream.

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Available abstract

By using of Penman formula, the authors calculated the evapotranspiration since 1980s, and analyzed the variation tendency of some climatic factors such as evapotranspiration, sunshine duration, air temperature, air saturation deficit etc, and focused on their impact to the evapotranspiration. The results show that the evapotranspiration is increasing annually with the speed of 3.25 mm over Yellow River upper stream area;while the sunshine duration which is considered as main impact factor, is increasing with the speed of 3.6 h/a;air temperature is appearing the increasing tendency, and its climatic tendency is 0.4 ℃ /10 a; air saturation deficit is increasing with 0.02 hPa/a. Therefore, we could think that the evapotranspiration is greatly increasing as increment of sunshine duration and air temperature deficit over Yellow River upper stream area. But the increment of evapotranspiration and decrement of precipitation amount impact directly on the decrement of flow curve and expanding of grassland's desertization over Yellow River upper stream.

Key concepts: Evapotranspiration, Sunshine duration, Environmental science, Air temperature, Hydrology (agriculture), Precipitation, Grassland, Streamflow

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