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Coupled modeling of land hydrology-regional climate including human carbon emission and water exploitation

机译:土地水文-区域气候的耦合模型,包括人类碳排放和水的开采

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摘要

Carbon emissions and water use are two major kinds of human activities.To reveal whether these two activities can modify the hydrological cycle and climate system in China,we conducted two sets of numerical experiments using regional climate model RegCM4.In the first experiment used to study the climatic responses to human carbon emissions,the model were configured over entire China because the impacts of carbon emissions can be detected across the whole country.Results from the first experiment revealed that near-surface air temperature may significantly increase from 2007 to 2059 at a rate exceeding 0.1 ℃C per decade in most areas across the country;southwestern and southeastern China also showed increasing trends in summer precipitation,with rates exceeding 10 mm per decade over the same period.In summer,only northern China showed an increasing trend of evapotranspiration,with increase rates ranging from 1 to 5 mm per decade;in winter,increase rates ranging from 1 to 5 mm per decade were observed in most regions.These effects are believed to be caused by global warming from human carbon emissions.In the second experiment used to study the effects of human water use,the model were configured over a limited region-Haihe River Basin in the northern China,because compared with the human carbon emissions,the effects of human water use are much more local and regional,and the Haihe River Basin is the most typical region in China that suffers from both intensive human groundwater exploitation and surface water diversion.We incorporated a scheme of human water regulation into RegCM4 and conducted the second experiment.Model outputs showed that the groundwater table severely declined by ~10 m in 1971-2000 through human groundwater overexploitation in the basin;in fact,current conditions are so extreme that even reducing the pumping rate by half cannot eliminate the groundwater depletion cones observed in the area.Other hydrological and climatic elements,such as soil moisture,runoff generation,air humidity,precipitation,wind field,and soil and air temperature,were also significantly affected by anthropogenic water withdrawal and consumption,although these effects could be mitigated by reducing the amount of water drawn for extraction and application.
机译:碳排放和用水是人类的两种主要活动。为了揭示这两种活动是否可以改变中国的水文循环和气候系统,我们使用区域气候模型RegCM4进行了两组数值实验。对人类碳排放的气候响应,该模型在整个中国进行了配置,因为可以在全国范围内检测到碳排放的影响。第一个实验的结果表明,从2007年到2059年,近地表气温可能会显着升高。全国大部分地区每十年超过0.1℃;西南和东南地区也显示出夏季降水增加的趋势,同一时期每十年超过10毫米。夏季,只有中国北方显示出蒸散量增加的趋势,速率每十年增加1到5毫米;冬天,速率每十年增加1-5毫米据认为,这些影响是由于人类碳排放引起的全球变暖所致。在用于研究人类用水影响的第二个实验中,该模型在北半球有限区域-海河流域进行了构造在中国,由于与人类碳排放相比,人类用水的影响更多地域和区域性,而海河流域是中国最典型的地区,该地区遭受着大量的人类地下水开采和地表水转移的困扰。模型输出表明,由于流域内人类地下水的过度开采,1971-2000年地下水位严重下降了约10 m;实际上,当前的条件非常极端,甚至减少了。抽水速率的一半不能消除该地区观察到的地下水枯竭锥。其他水文和气候要素,例如土壤潮湿当然,人为的取水量和消耗量也显着影响了水,径流的产生,空气湿度,降水,风场以及土壤和气温,尽管可以通过减少抽取和使用的水量来减轻这些影响。

著录项

  • 来源
    《气候变化研究进展(英文版)》 |2017年第2期|68-79|共12页
  • 作者单位

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China;

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Institute of Oceanographic Instrumentation, Shandong Academy of Sciences, Qingdao 266001, China;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-19 03:58:03
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