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Trends analysis of rainfall and rainfall extremes in Sarawak, Malaysia using modified Mann-Kendall test

机译:马来西亚利用改进的MANN-KENDALL测试,马来西亚降雨与降雨降雨及降雨趋势分析

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This study assesses the spatial pattern of changes in rainfall extremes of Sarawak in recent years (1980-2014). The Mann-Kendall (MK) test along with modified Mann-Kendall (m-MK) test, which can discriminate multi-scale variability of unidirectional trend, was used to analyze the changes at 31 stations. Taking account of the scaling effect through eliminating the effect of autocorrelation, m-MK was employed to discriminate multi-scale variability of the unidirectional trends of the annual rainfall in Sarawak. It can confirm the significance of the MK test. The annual rainfall trend from MK test showed significant changes at 95% confidence level at five stations. The seasonal trends from MK test indicate an increasing rate of rainfall during the Northeast monsoon and a decreasing trend during the Southwest monsoon in some region of Sarawak. However, the m-MK test detected an increasing trend in annual rainfall only at one station and no significant trend in seasonal rainfall at any stations. The significant increasing trends of the 1-h maximum rainfall from the MK test are detected mainly at the stations located in the urban area giving concern to the occurrence of the flash flood. On the other hand, the m-MK test detected no significant trend in 1- and 3-h maximum rainfalls at any location. On the contrary, it detected significant trends in 6- and 72-h maximum rainfalls at a station located in the Lower Rajang basin area which is an extensive low-lying agricultural area and prone to stagnant flood. These results indicate that the trends in rainfall and rainfall extremes reported in Malaysia and surrounding region should be verified with m-MK test as most of the trends may result from scaling effect.
机译:本研究评估了近年来沙捞越降雨极端变化的空间模式(1980-2014)。 Mann-Kendall(MK)测试以及改进的Mann-Kendall(M-MK)测试,可以辨别单向趋势的多规模变化,分析31站的变化。考虑到通过消除自相关的效果来考虑到缩放效果,M-MK被用来区分砂拉越年降雨量的单尺度变化。它可以确认MK测试的重要性。来自MK测试的年降雨趋势显示出5个站点的95%置信水平的显着变化。 MK试验中的季节性趋势表明了东北季风期间的降雨率越来越高,在沙捞越的某些地区西南季风期间的趋势降低。然而,M-MK检测检测到每年降雨量的趋势越来越大,在任何站点都没有明显的季节降雨趋势。从MK测试中的1-H最大降雨的显着提高趋势主要在位于城市地区的车站,以令潮流洪水发生的关注。另一方面,M-MK测试在任何位置检测到1-和3-H的最大降雨中没有显着趋势。相反,它检测到位于Rajang盆地下方的车站的6-和72-H和72-H最大降雨中的重大趋势,这是一个广泛的低洼农业区,易于停滞不前。这些结果表明,在马来西亚和周边地区报道的降雨和降雨极端的趋势应通过M-MK测试来验证,因为大多数趋势可能是由缩放效应产生的。

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