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Rainfall thresholds for the occurrence of debris flows in the Jiangjia Gully, Yunnan Province, China

机译:云南省江嘉沟壑区泥石流发生的降雨阈值

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摘要

The Jiangjia Gully (JJG), Yunnan Province, China, is one of several debris flow gullies that characterize the topography of mountainous areas in China. Rainfall-triggered debris flows are frequent in the JJG. In order to model and predict these debris flow occurrences, we analyzed precipitation parameters (including intensity-duration thresholds and rainfall event-duration thresholds) that triggered past debris flow events in the JJG. Since the JJG is unique, any model used for predicting debris flows in this gully must be developed using data from only this gully. Furthermore, the effects of normalized precipitation and antecedent precipitation on debris flows in the JJG were considered. Debris flow data and precipitation data were compiled from 47 debris flow events in 1993, 1994, 1998-2001,2004 and 2006 in JJG. All of these debris flows were triggered following a precipitation event with a duration of 6 h or less, with most of the precipitation events exhibiting a duration of 3 to 6 h. Only three rainfall events with a duration of less than 1 h and average intensity between 1.0 and 42.0 mm/h produced debris flows. The 90%, 70% and 50% probability curves for debris flow events were then constructed. Intensity-duration (I-D) and rainfall event-duration (RE-D) thresholds were then used for debris flow modeling based on preliminary tests and comparisons. Antecedent precipitation was found not to be a significant factor in triggering debris flows in the JJG; however, intraday precipitation played a significant role. Normalized precipitation threshold curves from adjacent areas were not well-correlated with the patterns observed in the JJG. Determination of unique thresholds for each gully is necessary for developing an effective prediction system. Crown Copyright (C) 2015 Published by Elsevier B.V. All rights reserved.
机译:中国云南省的江家沟(JJG)是表征中国山区地形的数种泥石流沟之一。在JJG中,降雨触发的泥石流很频繁。为了对这些泥石流发生进行建模和预测,我们分析了降水参数(包括强度持续时间阈值和降雨事件持续时间阈值),这些参数触发了JJG中过去的泥石流事件。由于JJG是唯一的,因此只能使用来自该沟壑的数据来开发用于预测该沟壑中泥石流的任何模型。此外,还考虑了归一化降水和前期降水对JJG泥石流的影响。泥石流数据和降水数据是根据JJG在1993、1994、1998-2001、2004和2006年发生的47次泥石流事件汇编的。所有这些泥石流都是在持续时间为6小时或更短的降雨事件之后触发的,大多数降水事件的持续时间为3至6小时。仅三个持续时间少于1小时且平均强度在1.0和42.0 mm / h之间的降雨事件产生了泥石流。然后构建泥石流事件的90%,70%和50%概率曲线。然后,根据初步测试和比较,将强度持续时间(I-D)和降雨事件持续时间(RE-D)阈值用于泥石流建模。在JJG,发现前期降水不是触发泥石流的重要因素;然而,日内降水起着重要作用。邻近地区的归一化降水阈值曲线与JJG中观测到的模式没有很好的相关性。为开发有效的预测系统,必须确定每个沟渠的唯一阈值。 Crown版权所有(C)2015,Elsevier B.V.保留所有权利。

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