首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Spatial and temporal variations in rainfall erosivity and erosivity density in South Korea
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Spatial and temporal variations in rainfall erosivity and erosivity density in South Korea

机译:韩国降雨侵蚀性和侵蚀性密度的空间和时间变化

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Rainfall erosivity is one of the key parameters in Universal Soil Loss Equation (USLE), which has been used to predict the amount of soil loss by water for 50 years. Investigating spatial and temporal trends in rainfall erosivity is important for soil and water conservation planning. Rainfall erosivity (the R factors) in many regions is expected to be altered due to changes in rainfall patterns related to rainfall intensity and the frequency and spatial distribution of storm events that may occur with climate change. In South Korea, some researchers have studied temporal variation in meteorological and hydrologic phenomena with climate change, particularly temperature and precipitation trends. The purpose of this study is to investigate spatial and temporal variations in rainfall erosivity and erosivity density and to improve our understanding of the evolution of rainfall erosivity in South Korea. First, we calculated rainfall erosivity at 46 stations for 1961-2015 using 5-min precipitation data. Second, we examined spatial and temporal variability in the rainfall erosivity; trends and change points of R factor time series and analyzed the relationships between rainfall erosivity and climate indices (such as the precipitation amount, number of effective events, and duration). Four trend tests such as the t-test, MK test, modified version of the MK test, and BBS-MK test, were used to detect trends in the annual R factor, total duration, number of effective events, total depth, mean maximum 30-min intensity, and total kinetic energy time series for all employed stations. The results provide insights into the evolution of rainfall erosivity and the effects of large-scale climatic circulation on rainfall erosivity.
机译:降雨侵蚀是通用土壤损失方程(USLE)的关键参数之一,已被用于预测水50年的土壤损失量。调查降雨侵蚀性的空间和时间趋势对于水土保持计划很重要。由于与降雨强度有关的降雨模式的变化以及气候变化可能发生的风暴事件的频率和空间分布,预计许多地区的降雨侵蚀性(R因子)预计会发生变化。在韩国,一些研究人员研究了气候变化,特别是温度和降水趋势的气象和水文现象的时间变化。本研究的目的是调查降雨侵蚀性和侵蚀性密度的空间和时间变化,并改善我们对韩国降雨侵蚀性演变的理解。首先,我们使用5分钟降水数据计算了1961 - 2015年的46站的降雨侵蚀性。其次,我们检查了降雨侵蚀性的空间和时间变异; R因子时间序列的趋势和变化点,分析了降雨侵蚀性与气候指标之间的关系(如降水量,有效事件数量和持续时间)。四个趋势测试,如T检验,MK测试,修改版本的MK测试和BBS-MK测试,用于检测年度R因子,总持续时间,有效事件数量,总深度,平均值的趋势适用于所有使用的车站的30分钟强度和总动能时间序列。结果提供了进入降雨侵蚀性的演变和大规模气候循环对降雨侵蚀性的影响的见解。

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