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Climate change detection and annual extreme temperature analysis of the Irtysh Basin

机译:额尔齐斯河流域的气候变化探测和年度极端温度分析

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摘要

As the largest tributary of the Ob River, the Irtysh River is an international river partially joining the territories of China, Kazakhstan, and Russia. Four meteorological stations in the Irtysh Basin were selected and the long-term observed daily temperature data were collected. The extreme temperature change was analyzed considering climate change. Detected by the heuristic segmentation by histogram comparison approach, climate was changed during the first half of the 1970s in terms of the increased mean value and decreased standard deviation of the daily temperature series. The noticeable change of the monthly mean temperature was the warmer winter. After climate change, the annual maximum temperature was little changed and its series was not segmented. However, the annual minimum temperature was significantly changed in terms of the increased mean value by more than 2℃, so its series was segmented to the pre- and post-change point subseries. The generalized extreme value distribution was fitted to the annual extreme temperature and the parameters were estimated by the maximum likelihood method. The return levels for 10/50/100-year return periods estimated by the profile likelihood method were obtained for the annual extreme temperature. The probability of occurrence of the cold extremes was decreased after 1970s.
机译:作为鄂毕河的最大支流,额尔齐斯河是一条国际河流,部分连接了中国,哈萨克斯坦和俄罗斯。选择了额尔齐斯盆地的四个气象站,并收集了长期观察到的每日温度数据。分析了考虑气候变化的极端温度变化。通过直方图比较法进行启发式分割检测,在1970年代上半叶,由于每日温度序列的平均值增加和标准偏差减小,气候发生了变化。每月平均温度的明显变化是冬天变暖。气候变化后,年度最高温度几乎没有变化,其序列没有分段。但是,年度最低温度在增加平均值超过2℃方面发生了显着变化,因此将其序列划分为变化前和变化后的子序列。将广义极值分布拟合到年度极端温度,并通过最大似然法估算参数。通过廓线似然法估算的10/50/100年回报期的回报水平是针对年度极端温度得出的。 1970年代后发生极端寒冷的可能性降低。

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  • 来源
    《Theoretical and applied climatology》 |2013年第4期|465-470|共6页
  • 作者单位

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China,College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China,College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China,College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China,College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;

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