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Rainfail interception by Swamp meadow and Alpine meadow and its seasonal distribution pattern on the Qinghai-Tibet Plateau, China

机译:沼泽草甸和高山草甸的降雨拦截及其在中国青藏高原的季节性分布格局

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In order to investigate to quantify losses by Alpine vegetation in Qinghai-Tibet Plateau, typical Swamp meadow and Alpine meadow were investigated in the growth period. The intercepting rainfall of Swamp meadow and Alpine meadow were studied by using water balance method and ANOVA statistical analysis method. The experimental results indicate that: under different coverage of Swamp meadow and Alpine meadow, rainfall interception in the growing period (June-September) both show an increasing trend. And, both the maximum rainfall interception and maximum interception rate emerge in September under different vegetation cover of Swamp meadow and Alpine meadow. However, With vegetation degeneration, interception quantity and interception rate of Swamp meadows and Alpine meadows both show decreasd trends. Interception amount and interception rate show decreased tend along with the degradation of Swamp meadow and Alpine meadow, which indicate that the degradation of meadow is unfavorable for Swamp meadow and Alpine meadow to prevent the rain landing the earth directly.
机译:为了研究量化在青藏高原高寒植被的损失,典型的沼泽草甸和高寒草甸中的生长期进行了调查。沼泽草甸和高寒草甸的拦截降雨通过使用水量平衡法和方差统计分析方法研究。实验结果表明:不同的覆盖沼泽化草甸和高寒草甸,在生长期(月 - 9月)降雨截留下都表现出逐年上升的趋势。而且,无论是最大截留和最大拦截率在九月出现沼泽化草甸和高寒草甸的不同植被覆盖下。然而,随着植被退化,拦截量和沼泽草甸的拦截率和高山草甸都显示decreasd趋势。拦蓄量和拦截率下降显示与沼泽化草甸和高寒草甸的退化,这表明草地的退化是不利于沼泽化草甸和高寒草甸,以防止雨水直接登陆土趋于一起。

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