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Spatial and temporal variability of daily temperature during 1961-2010 in the Yangtze River Basin, China

机译:长江流域1961-2010年日温度的时空变化

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摘要

This study investigated the spatial and temporal variability of daily minimum, mean and maximum temperature and the diurnal temperature range (DTR) in the Yangtze River Basin (YRB) during 1961 -2010. Three variability patterns of daily minimum temperature and four variability patterns of daily mean and maximum temperatures were detected. Results indicate that the rugged topography causes more complex temperature variability in the mid YRB, and daily mean temperature shows more complex variability rather than daily minimum and maximum temperatures. Under the control of both topography and atmospheric circle, three temperature variables have mean values decreasing spatially with longitude, although the Sichuan Basin has larger mean values compared with the surrounding areas, and there are smaller variations in the Jinsha River Basin relative to other areas. The variations of three temperature variables became smaller over time. After the 1980s, the three temperature variables show upward trends in most areas of YRB, except in the Jinsha River Basin where complex temperature trends appeared. In the five decades, both negative and positive magnitudes of DTR were detected, reflecting the different upward speeds of daily minimum and maximum temperatures in different areas of YRB. Rapid urbanization caused notably increasing temperature and DTR in the 2000s at the Wuhan and Shanghai urban agglomerations. In summary, the Dongting and Poyang Lake basins and the Yangtze River Delta in YRB are more sensitive and susceptible to climate change.
机译:本研究调查了1961-2010年长江流域(YRB)的每日最低,最高和最高温度以及日温度范围(DTR)的时空变化。检测到每日最低温度的三种变化模式以及每日平均温度和最高温度的四种变化模式。结果表明,崎top的地形会在YRB中部造成更复杂的温度变化,并且日平均温度显示出更复杂的变化,而不是每日的最低和最高温度。在地形和大气圈的控制下,三个温度变量的平均值随经度在空间上减小,尽管四川盆地的平均值比周围地区大,而金沙江流域相对于其他地区变化较小。三个温度变量的变化随时间变小。在1980年代以后,除金沙江流域出现了复杂的温度趋势外,这三个温度变量在YRB的大多数地区都呈上升趋势。在这五十年中,DTR的负值和正值都被检测到,反映了YRB不同区域中每日最低和最高温度的不同上升速度。快速的城市化在2000年代导致武汉和上海城市群的温度和DTR显着上升。综上所述,长江流域的洞庭湖和basin阳湖流域以及长江三角洲对气候变化更为敏感和敏感。

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  • 来源
    《Quaternary International》 |2013年第5期|33-42|共10页
  • 作者单位

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China,Center for Water Resources Research, Chinese Academy of Sciences, Beijing 100101, China;

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China,Center for Water Resources Research, Chinese Academy of Sciences, Beijing 100101, China;

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China,Center for Water Resources Research, Chinese Academy of Sciences, Beijing 100101, China;

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