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Influences of climate change and human activities on Tarim River runoffs in China over the past half century

机译:半个世纪以来气候变化和人类活动对中国塔里木河径流的影响

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摘要

The changes in annual runoff of the three original rivers and the mainstream of Tarim River were analyzed by the non-parametric tests based on the hydrologic data during the period of 50 years. Using hydrologic data, meteorological data and the fitted equation, the impacts of climate change and human activities on annual runoff of the mainstream were assessed. Based on the analysis, the following conclusions can be drawn: (1) headstream runoff has increased in the past 50 years, and has sharply jumped after 1990; (2) mainstream runoff decreased progressively in the past 50 years, which indicated that interference from human activities was the main cause for the decreasing runoff. This had greater negative influence than positive influence, which caused the mainstream average runoff to decrease by 5.4 × 10~8 m~3 from 1990 to 2008 as compared to 1957-2008; (3) if human activities remained at pre-1990 levels, climate change alone would have caused the runoff of mainstream of Tarim River to increase by 5.4 × 10~8 m~3 annually in the past 20 years; (4) if the climate had remained at pre-1990 conditions, human activities alone would have caused the runoff of mainstream of Tarim River to increase by 5.4 × 10~8 m~3 annually over the past 20 years. However, mainstream average runoff was 42.6 × 10~8 m~3 from 1990 to 2008 with the negative effects of human activities masked by the larger, positive effect of climate changes. The results in this paper provide a scientific basis for conservation strategies, sustainable management, and ecological restoration of the Tarim River Basin.
机译:基于50年的水文资料,通过非参数检验分析了三大原河和塔里木河干流的年径流量变化。利用水文数据,气象数据和拟合方程,评估了气候变化和人类活动对主流年径流量的影响。根据分析,可以得出以下结论:(1)在过去的50年中,源头径流量增加了,1990年以后急剧增加; (2)近50年来,主流径流量逐渐减少,这说明人类活动的干扰是径流减少的主要原因。负面影响大于正面影响,这导致1990-2008年主流平均径流量与1957-2008年相比减少了5.4×10〜8m〜3。 (3)如果人类活动保持在1990年前的水平,仅气候变化就将导致塔里木河干流在过去20年中每年增加5.4×10〜8 m〜3; (4)如果气候保持在1990年前的条件下,仅人类活动就会导致塔里木河干流在过去20年中每年增加5.4×10〜8 m〜3。然而,从1990年到2008年,主流平均径流量为42.6×10〜8 m〜3,人类活动的负面影响被更大,正面的气候变化影响所掩盖。本文的研究结果为塔里木河流域的保护战略,可持续管理和生态恢复提供了科学依据。

著录项

  • 来源
    《Environmental earth sciences》 |2012年第1期|p.231-241|共11页
  • 作者单位

    Xinjiang Institute of Ecology and Geography Chinese Academy of Science, Urumqi 830011, People's Republic of China,Graduate University of Chinese Academy of Sciences,Beijing 100049, People's Republic of China,Xinjiang Tarim River Basin Management Bureau,Kuerle 84100, People's Republic of China;

    Xinjiang Institute of Ecology and Geography Chinese Academy of Science, Urumqi 830011, People's Republic of China;

    Xinjiang Institute of Ecology and Geography Chinese Academy of Science, Urumqi 830011, People's Republic of China;

    Xinjiang Institute of Ecology and Geography Chinese Academy of Science, Urumqi 830011, People's Republic of China,Graduate University of Chinese Academy of Sciences,Beijing 100049, People's Republic of China;

    Xinjiang Institute of Ecology and Geography Chinese Academy of Science, Urumqi 830011, People's Republic of China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    climate change; human activities; runoff; tarim river;

    机译:气候变化;人类活动;径流;塔里木河;

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