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Spatiotemporal Variation and Abrupt Change Analysis of Temperature from 1960 to 2012 in the Huang-Huai-Hai Plain, China

机译:黄淮海平原1960-2012年气温的时空变化和突变分析

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Based on a monthly dataset of temperature time series (1960–2012) in the Huang-Huai-Hai Plain of China (HHHPC), spatiotemporal variation and abrupt change analysis of temperature were examined by moving average, linear regression, spline interpolation, Mann-Kendall test, and movingt-test. Major conclusions were listed as follows. (1) Annual and seasonal temperature increased with different rates on the process of fluctuating changes during 1960~2012. The upward trend was 0.22°C 10a−1for annual temperature, while it was very significant in winter (0.34°C 10a−1) and spring (0.31°C 10a−1), moderately significant in autumn (0.21°C 10a−1), and nonsignificant in summer (0.05°C 10a−1). (2) The spatial changes of annual and seasonal temperature were similar. The temperature increased significantly in Beijing and its adjacent regions, while it was nonsignificant in the central and southern regions. (3) The spring, autumn, winter, and annual temperature had warm abrupt change. The abrupt change time for winter temperature was in the late 1970s, while it was in the late 1980s and early 1990s for spring, autumn, and annual temperature. (4) Macroscopic effects of global and regional climate warming and human activities were probably responsible for the temperature changes. The climate warming would influence the hydrological cycle and agricultural crops in the study area.
机译:根据中国黄淮海平原(HHHPC)的温度时间序列(1960–2012)的每月数据集,通过移动平均,线性回归,样条插值,Mann-肯德尔测试和移动测试。主要结论如下。 (1)在1960〜2012年期间,年和季节温度在不同的变化过程中以不同的速率上升。全年温度的上升趋势为0.22°C 10a-1,而冬季(0.34°C 10a-1)和春季(0.31°C 10a-1)的上升趋势非常显着,秋季(0.21°C 10a-1的上升趋势则中等)。 ),而夏季(0.05°C 10a-1)则不重要。 (2)年,季节温度的空间变化相似。北京及其附近地区的气温显着升高,而中部和南部地区则没有明显升高。 (3)春季,秋季,冬季和年温度有温暖的突变。冬季温度的突然变化时间是在1970年代末,而春季,秋季和年温度分别在1980年代末和1990年代初。 (4)全球和区域气候变暖和人类活动的宏观影响可能是温度变化的原因。气候变暖将影响研究区域的水文循环和农作物。

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