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Trends of major hydroclimatic variables in the Tarim River basin during the past 50 years

机译:塔里木河流域近50年主要水文气候变化趋势

摘要

The nonparametric Mann-Kendall test was used to detect the trends of major hydroclimatic variables in the Tarim River Basin, the largest inland river basin in China for the period of 1960-2007. Results showed that both mean annual air temperature and precipitation experienced an increasing trend, while annual streamflow demonstrated a mixed trend of decreasing and increasing: The mountainous region upstream showed an increasing trend and the region downstream exhibited a decreasing trend. impacts of the increased air temperature on streamflow have shown different characteristics depending on location and seasons: it has positive effect on the runoff at mountainous region due to snowmelt and glacier-melt in spring, but negative effect on the runoff at plain area due to the increase of actual evaporation in summer. in addition, human activity contributed to the declining of streamflow in the arid plain oases at downstream of the Tarim River Basin. The results obtained in this paper can be used as a reference for the planning and management of water resources to maintain the health of the river system. (C) 2009 Elsevier Ltd. All rights reserved.
机译:使用非参数Mann-Kendall检验来检测1960-2007年间中国最大的内陆河流域塔里木河流域的主要水文气候变量趋势。结果表明,年平均气温和降水量均呈上升趋势,而年流量呈下降趋势和上升趋势混合趋势:上游山区呈上升趋势,下游区域呈下降趋势。气温升高对水流的影响随位置和季节的不同而表现出不同的特征:春季春季由于融雪和冰川融化,对山区径流产生积极影响,而春季对冰川径流产生不利影响。夏季实际蒸发量增加。此外,人类活动导致塔里木河流域下游干旱平原绿洲的水流量下降。本文的研究结果可为水资源的规划和管理,维护河流系统健康提供参考。 (C)2009 Elsevier Ltd.保留所有权利。

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