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The evolvement mechanism of hydro-meteorological elements under climate change and the interaction impacts in Xin'anjiang Basin, China

机译:气候变化下水力气象因素的演变机制及新安江盆地的互动影响

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摘要

In order to explore the evolvement mechanism of hydrological elements under climate change and the interaction impacts, the hydro-meteorological elements, like temperature, precipitation, runoff, and evaporation, are studied by statistical analysis method and cause analysis approach in this paper. Initially, in terms of climate change across Anhui province, the average temperature data from 1960 to 2009 at 15 meteorological stations are selected from China Meteorological Data Sharing Network to analyze the spatio-temporal variation of temperature characteristics. Secondly, from the perspective of Xin'anjiang Basin, evolution rules of hydro-meteorological elements are studied through deviation variation of every 10years and the long-term development trend from 1981 to 2010 at 9 hydrological stations. And the influence of climate change on runoff is analyzed according to the principle of runoff formation, and the response of runoff to precipitation and temperature is predicted with the simulating future climate change by climate models. The results show that, through statistics, the average temperature in Anhui province is in a fluctuating downward state from 1960 to 1990. After 1990, the uptrend is significant. In Xin'anjiang Basin, the annual precipitation declines overally, especially at some stations it is obvious. The variation of runoff is in a downtrend consistent with precipitation, but it is not noticeable, taken as a whole. The average evaporation changes unremarkably, except in summer and winter. Under three scenarios of A1B, A2 and B1, it is assumed that temperature, precipitation and runoff are all increasing in the future. Through cause analysis, these mainly seem to be affected by the circulation of weather background and sea surface temperature. Based on the analysis of hydro-meteorological elements under climate change and the forecasting of their future changes, the development of regional water resources can be grasped which is of great significance for human interests to water supply scheme, water conservancy project planning, and the economic-social sustainablility.
机译:为了探讨气候变化下水文元素的演变机制和相互作用影响,通过统计分析方法研究了水流 - 气象元素,液体气象元素,如温度,沉淀,径流和蒸发,并在本文中引起分析方法。最初,在安徽省气候变化方面,1960年至2009年的平均气温数据在15个气象站中选自中国气象数据共享网络,分析温度特性的时空变化。其次,从新安江盆地的角度来看,通过每10年的偏差变化和1981年至2010年在9个水文站的长期发展趋势来研究水流元素的演化规则。根据径流形成原理分析了气候变化对径流的影响,并通过气候模型模拟未来气候变化来预测径流与降水和温度的响应。结果表明,通过统计数据,安徽省的平均气温从1960年到1990年的波动中的下行状态。1990年后,上升趋势是显着的。在新安江盆地,年降水量过于下降,特别是在某些站点上显而易见。径流的变化在于沉淀的下降趋势,但它不明显,作为一个整体。除夏季和冬季外,平均蒸发不起作用。在A1B,A2和B1的三种情况下,假设将来的温度,降水和径流都在增加。通过原因分析,这些主要似乎受到天气背景和海面温度的影响。基于气候变化下水力气象因素分析及其未来变化的预测,区域水资源的发展可以掌握,对人类利益对供水计划,水利项目规划和经济的影响是重要意义 - 社会可持续性。

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    Nanjing Univ Informat Sci & Technol Jiangsu Key Lab Agr Meteorol Collaborat Innovat Ctr Forecast & Evaluat Meteoro Nanjing 210044 Jiangsu Peoples R China|Nanjing Hydraul Res Inst Nanjing 210029 Jiangsu Peoples R China|Nanjing Univ Informat Sci & Technol Sch Hydrol & Water Resources Nanjing 210044 Jiangsu Peoples R China;

    Nanjing Univ Informat Sci & Technol Jiangsu Key Lab Agr Meteorol Collaborat Innovat Ctr Forecast & Evaluat Meteoro Nanjing 210044 Jiangsu Peoples R China|Nanjing Univ Informat Sci & Technol Sch Hydrol & Water Resources Nanjing 210044 Jiangsu Peoples R China;

    Nanjing Hydraul Res Inst Nanjing 210029 Jiangsu Peoples R China;

    Hefei Univ Technol Sch Civil Engn Hefei 230009 Anhui Peoples R China;

    Nanjing Univ Informat Sci & Technol Sch Hydrol & Water Resources Nanjing 210044 Jiangsu Peoples R China;

    Nanjing Univ Informat Sci & Technol Sch Hydrol & Water Resources Nanjing 210044 Jiangsu Peoples R China;

    Shanghai Cathay Advertising Co LTD Shanghai 200030 Peoples R China;

    Jiaxing Airport Jiaxing 314000 Zhejiang Peoples R China;

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  • 正文语种 eng
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  • 关键词

    Hydro-meteorological elements; Climate change; The interaction impacts; Prediction;

    机译:水流气象元素;气候变化;互动影响;预测;

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