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Spatio-temporal variation and abrupt changes for major climate variables in the Taihu Basin, China

机译:太湖流域主要气候变量的时空变化和突变

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摘要

Long-term trend and abrupt changes of major climate variables in the Taihu Basin were investigated based on the mean, maximum and minimum air temperature, diurnal temperature range (DTR), precipitation, relative humidity and sunshine duration at six meteorological stations from 1954 to 2006. Results showed that the long-term trend for annual precipitation was not statistically significant during the past 53 years, but a wetter tendency was detected and the increasing centre for annual precipitation was located in the southeast of the study area. Mean air temperature has increased by 1.43°C, similar trends were also identified for maximum and minimum air temperature, which have increased by 1.06 and 1.54°C, respectively, while DTR exhibited a slight decreasing trend with a rate of about —0.09°C/(10 year). The annual mean relative humidity and sunshine duration exhibited a decreasing trend, with Kendall slope values of —0.99%/10 year and —7.797 h/10 year, respectively. Examination of long-range dependence showed that all climate variables exhibited strong persistence at annual scale except minimum air temperature. Detection of abrupt changes using nonpara-metric Mann-Kendall and Pettitt methods showed different results. Abrupt changes occurred in the 1980s and 2000s for annual precipitation using the nonparametric Mann-Kendall method, while no abrupt changes were detected using the Pettitt method. Abrupt changes of temperature and relative humidity took place in the early 1990s using the nonparametric Mann-Kendall method, which occurred in the late and mid 1980s using the Pettitt method, while abrupt changes of sunshine duration and DTR detected by two methods occurred in the similar period. The result will be helpful for local flood control and drought relief in urban planning and construction under future global climate change.
机译:基于1954年至2006年六个气象站的平均,最高和最低气温,日平均温度范围(DTR),降水,相对湿度和日照时数,研究了太湖流域主要气候变量的长期趋势和突变。结果表明,在过去的53年中,年降水量的长期趋势没有统计学意义,但发现有湿润趋势,年降水量的增长中心位于研究区域的东南部。平均气温上升了1.43°C,最高和最低气温也分别出现了类似的趋势,分别上升了1.06和1.54°C,而DTR则以-0.09°C的速率出现了小幅下降的趋势/(10年)。年平均相对湿度和日照时间呈下降趋势,肯德尔坡度值分别为-0.99%/ 10年和-7.797h / 10年。长期依赖性的检验表明,除最低气温外,所有气候变量在年尺度上均表现出较强的持久性。使用非参数Mann-Kendall和Pettitt方法检测突变的结果显示了不同的结果。使用非参数Mann-Kendall方法在1980年代和2000年代出现了年降水量的突变,而使用Pettitt方法则未发现突变。在1990年代初期,使用非参数Mann-Kendall方法发生了温度和相对湿度的突然变化,在1980年代后期和中期,使用了Pettitt方法发生了温度和相对湿度的变化,而通过两种方法检测到的日照持续时间和DTR的突变发生在类似的情况下期。该结果将有助于在未来全球气候变化下的城市规划和建设中进行局部防洪和抗旱。

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    Key Laboratory of Water and Sediment Sciences, Ministry of Education, College of Water Sciences, Beijing Normal University, Beijing 100875, P.R. China;

    Key Laboratory of Water and Sediment Sciences, Ministry of Education, College of Water Sciences, Beijing Normal University, Beijing 100875, P.R. China;

    Key Laboratory of Water and Sediment Sciences, Ministry of Education, College of Water Sciences, Beijing Normal University, Beijing 100875, P.R. China,Beijing Hydraulic Research Institute, Beijing 100048, China;

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  • 正文语种 eng
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  • 关键词

    climate change; trend; abrupt change; precipitation; air temperature; taihu;

    机译:气候变化;趋势;突变沉淀;气温;太湖;

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