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Decreasing trend of sunshine hours and related driving forces in Southwestern China

机译:中国西南地区日照时间的减少趋势及相关驱动力

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摘要

Total hours of sunshine are one of the most important factors affecting climate and environment, and its long-term variation is of much concern in climate studies. Trends of temporal and spatial patterns in sunshine hours and related climatic factors over southwestern China are evaluated for the period 1961-2009 based on data from 111 standard meteorological stations. The results showed that southwestern China is experiencing a statistical decrease of sunshine hours, at the rate of 31.9 h/10a during 1961-2009. The decline was particularly strong in summer, whereas it is nonsignificant in winter. Spatially, statistically significant decreases of sunshine hours mainly occurred in lower altitude regions, especially in the Sichuan basin and Guizhou plateau. Sunshine hours have a high correlation with wind speed, relative humidity, precipitation, cloud cover, surface downwards solar radiation flux, and cloud water content, with wind speed showing the strongest relationship to sunshine hours, implicit in the close correlation (temporally and spatially) between the two variables. Changing water vapor and cloud cover influence sunshine hours in southwestern China. In addition, the increased surface downwards solar radiation flux also made some contribution to a rise of sunshine hours during 1991-2009. The larger decreasing trends of sunshine hours at urban stations than rural stations may reflect the effect of urbanization on sunshine hours. Variations are dominated by the comprehensive functions of multiple factors owing to the complex nature of effects on sunshine hours.
机译:日照总小时数是影响气候和环境的最重要因素之一,其长期变化是气候研究中非常关注的问题。基于111个标准气象台站的数据,对中国西南地区1961-2009年的日照时间和相关气候因子的时空分布趋势进行了评估。结果表明,中国西南地区的1961-2009年日照时数减少了31.9 h / 10a,这是一个统计数字。夏季的下降尤为明显,而冬季则无明显下降。从空间上看,日照时数的统计上显着减少主要发生在低海拔地区,尤其是四川盆地和贵州高原。阳光小时与风速,相对湿度,降水量,云量,地表向下的太阳辐射通量和云层水含量具有高度相关性,风速与阳光小时具有最强的关系,暗含着紧密的相关性(在时间和空间上)在两个变量之间。水汽和云层的变化影响中国西南地区的日照时间。此外,1991-2009年期间,地表向下太阳辐射通量的增加也对日照时间的增加做出了一定贡献。与农村站相比,城市站的日照时间减少趋势更大,这可能反映了城市化对日照时间的影响。由于影响日照时间的复杂性,变化受多种因素的综合作用支配。

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  • 来源
    《Theoretical and applied climatology》 |2012年第2期|p.305-321|共17页
  • 作者单位

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Department of Geography, Memorial University, St John's, NL A1B 3X9, Canada;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

    Cold and Arid Region Environment and Engineering Research Institute, Gansu Hydrology and Water Resources Engineering Research Center/Yulong Snow Mountain Glaciers and Environmental Observation Station, Chinese Academy of Sciences, Lanzhou 730000, China Graduate University of Chinese Academy of Sciences, Beijing 100049, China;

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