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Assessing the effect of climate change on reference evapotranspiration in China

机译:评估气候变化对中国参考蒸散量的影响

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摘要

Reference evapotranspiration (ET_0) is a key parameter in hydrological and meteorological studies. In this study, the FAO Penman-Monteith equation was used to estimate ET_0, and the change in ET_0 was investigated in China from 1960 to 2011. The results show that a change point around the year 1993 was detected for the annual ET_0 series by the Cramer's test. For the national average, annual ET_0 decreased significantly (P < 0.001) by -14.35 mm/decade from 1960 to 1992, while ET_0 increased significantly (P < 0.05) by 22.40 mm/decade from 1993 to 2011. A differential equation method was used to attribute the change in ET_0 to climate variables. The attribution results indicate that ET_0 was most sensitive to change in vapor pressure, followed by solar radiation, air temperature and wind speed. However, the effective impact of change in climate variable on ET_0 was the product of the sensitivity and the change rate of climate variable. During 1960-1992, the decrease in solar radiation was the main reason of the decrease in ET_0 in humid region, while decrease in wind speed was the dominant factor of decreases in ET_0 in arid region and semi-arid/semi-humid region of China. Decrease in solar radiation and/or wind speed offset the effect of increasing air temperature on ET_0, and together led to the decrease in ET_0 from 1960 to 1992. Since 1993, the rapidly increasing air temperature was the dominant factor to the change in ET_0 in all the three regions of China, which led to the increase in ET_0. Furthermore, the future change in ET_0 was calculated under IPCC SRES A1B and B1 scenarios with projections from three GCMs. The results showed that increasing air temperature would dominate the change in ET_0 and ET_0 would increase by 2.13-10.77,4.42-16.21 and 8.67-21.27 % during 2020s, 2050s and 2080s compared with the average annual ET_0 during 1960-1990, respectively. The increases in ET_0 would lead to the increase in agriculture water consumption in the 21st century and may aggravate the water shortage in China.
机译:参考蒸散量(ET_0)是水文和气象研究中的关键参数。在这项研究中,使用FAO Penman-Monteith方程估算ET_0,并在1960年至2011年期间对中国ET_0的变化进行了研究。结果表明,1993年前后,年度ET_0系列检测到一个变化点。克莱默的考验。对于全国平均值,从1960年到1992年,年ET_0显着下降(P <0.001)-14.35毫米/十年,而从1993年到2011年,ET_0显着增加(P <0.05)22.40毫米/十年。采用微分方程方法将ET_0的变化归因于气候变量。归因结果表明,ET_0对蒸气压的变化最敏感,其次是太阳辐射,气温和风速。但是,气候变量变化对ET_0的有效影响是敏感性和气候变量变化率的乘积。 1960-1992年,太阳辐射的减少是湿润地区ET_0减少的主要原因,而风速下降是中国干旱地区和半干旱/半湿润地区ET_0减少的主要原因。 。太阳辐射和/或风速的降低抵消了气温升高对ET_0的影响,并共同导致ET_0从1960年到1992年的下降。自1993年以来,迅速升高的气温是导致ET_0变化的主要因素。所有三个地区,导致ET_0的增加。此外,根据IPCC SRES A1B和B1情景,根据三个GCM的预测计算了ET_0的未来变化。结果表明,与1960-1990年期间的年平均ET_0相比,气温升高将主导ET_0和ET_0的变化,分别在2020年代,2050年代和2080年代分别增加2.13-10.77、4.42-16.21和8.67-21.27%。 ET_0的增加将导致21世纪农业用水量的增加,并可能加剧中国的水资源短缺。

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  • 作者单位

    Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, No. 11A, Datun Road, Chaoyang District, Beijing 100101, China,University of Chinese Academy of Sciences,No.l9A Yuquan Road, Beijing 100049, China;

    Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, No. 11A, Datun Road, Chaoyang District, Beijing 100101, China;

    Jiangxi Provincial Meteorological Observatory,Jiangxi Meteorological Bureau, No. 109 ShengfuBeier Road,Nanchang 330046, China;

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  • 原文格式 PDF
  • 正文语种 eng
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  • 关键词

    Reference evapotranspiration; Climate change; Trend; GCMs;

    机译:参考蒸散量;气候变化;趋势;GCM;

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