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Changes of flow regimes and precipitation in Huai River Basin in the last half century

机译:淮河流域近半个世纪来水流态和降水的变化

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摘要

Huai River Basin, as the sixth largest river basin in China, has a high-regulated river system and has been facing severe water problems. In this article, the changing patterns of runoff and precipitation at 10 hydrological stations from 1956 to 2000 on the highly regulated river (Shaying River) and less-regulated river (Huai River) in the basin are evaluated at the monthly, seasonal and annual scales using the Mann-Kendall test and simple linear regression model. The results showed that: (1) No statistically significant trends of precipitation in the upper and middle Huai River Basins were detected at the annual scale, but the trend of annual runoff at Baiguishan, Zhoukou and Fuyang stations in Shaying River decreased significantly, whereas the others were not. Moreover, the decreasing trends of runoff for most months were significant in Shaying River, although the trend of monthly precipitation decreased significantly only in April in the whole research area and the number of months in the dry season having significantly decreasing trends in runoff was more than that in the wet season. (2) The rainfall-runoff relationship was significant in both highly regulated river and less-regulated river. In regulated river, the reservoirs have larger regulation capacity than the floodgates and thus have the smaller correlation coefficient and t-value. In Huai River, the correlation coefficients decreased from upper stream to downstream. (3) The regulation of dams and floodgates for flood control and water supply was the principal reason for the decreasing runoff in Huai River Basin, although the decreasing precipitation in April in this basin was statistically significant. The findings are useful for recognizing hydrology variation and will provide scientific foundation to integrated water resources management in Huai River Basin.
机译:淮河流域是中国第六大流域,河流系统高度管制,面临严重的水问题。本文以月度,季节和年度尺度评价了流域内高调节河(沙ying河)和非调节河(淮河)1956年至2000年10个水文站的径流和降水变化规律。使用Mann-Kendall检验和简单的线性回归模型。结果表明:(1)淮河流域中上游年降水量没有统计学意义,但沙trends河白桂山站,周口站和阜阳站的年径流量趋势明显减少,而其他不是。此外,虽然整个研究区的月降水量趋势仅在四月份才显着下降,而径流显着下降的干旱季节数大于在雨季。 (2)在高度管制的河流和管制较少的河流中,降雨-径流关系均很显着。在调节河中,水库的调节能力大于闸门,因此相关系数和t值较小。在淮河,相关系数从上游到下游减小。 (3)淮河流域水坝和防洪堤的调节是造成淮河流域径流量减少的主要原因,尽管该流域4月份降水减少具有统计学意义。研究结果对于认识水文变化具有重要意义,为淮河流域水资源综合管理提供科学依据。

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