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Spatial Analysis of Rainfall Erosivity Trends in South Korea

机译:韩国降雨侵蚀力趋势的空间分析

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Rainfall erosive factor is one of the most important factors in RUSLE(Revised Universal Soil Loss Equation), the empirical method to estimate the amount of annual mean soil loss in certain areas. The purpose of this study is focused on the analysis of the spatial and temporal variability of rainfall erosivity in South Korea. The Mann-Kendall test were conducted to analyze linear and temporal trends of 33 weather stations for 1973~1999. 5 stations(middle-westem region) out of 33 stations had a significant positive trend, but 4 stations(east-coast, south-coast region) had a significant negative trend with a 90% confidence limit respectively. And rest of the regions had no significant trend. The results of Moran's I and Geary's C showed rainfall erosivity in South Korea had statistically weak positive spatial autocorrelations (clustered pattern) in the 1980s ~ 1990s and annual extreme values for 31 stations with a 90% confidence limit. Coefficient variance of rainfall erosivity in the 1990s also increased about 10% more than in the 1970s. This trend could be correlated with the increase of the local heavy storms.
机译:降雨侵蚀因子是RUSLE(修订的通用土壤流失方程)中最重要的因素之一,RUSLE是估算某些地区年平均土壤流失量的一种经验方法。本研究的重点是分析韩国降雨侵蚀力的时空变化。通过Mann-Kendall检验对33个气象站1973〜1999年的线性和时间趋势进行了分析。 33个站点中的5个站点(中西部地区)具有明显的正趋势,而4个站点(东海岸,南海岸区域)具有显着的负趋势,分别具有90%的置信限。其他地区则没有明显趋势。 Moran's I和Geary's C的结果表明,韩国的降雨侵蚀力在1980〜1990年代具有统计上较弱的正空间自相关(成簇模式),并且31个观测站的年极值均具有90%的置信度极限。 1990年代降雨侵蚀力的系数方差也比1970年代增加了约10%。这种趋势可能与当地暴风雨的增加有关。

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