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A low-cost method to measure the timing of postfire flash floods and debris flows relative to rainfall

机译:一种低成本的方法,可以测量火灾后山洪和泥石流相对降雨的时间

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摘要

Data on the specific timing of postfire flash floods and debris flows are very limited. We describe a method to measure the response times of small burned watersheds to rainfall using a low-cost pressure transducer, which can be installed quickly after a fire. Although the pressure transducer is not designed for sustained sampling at the fast rates (≤2 s) used at more advanced debris flow monitoring sites, comparisons with high-frequency stage data show that measured spikes in pressure sampled at 1 min intervals are sufficient to detect the passage of most debris flows and floods. Postevent site visits are used to measure the peak stage and identify flow type on the basis of deposit characteristics. The basin response time scale (t_b) to generate flow at each site was determined from an analysis of the cross correlation between time series of flow pressure and 5 min rainfall intensity. This time scale was found to be less than 30 min for 40 postfire floods and 11 postfire debris flows recorded in 15 southern California watersheds (≤1.4 km~2). Including data from 24 other debris flows recorded at 5 more instrumentally advanced monitoring stations, we find there is not a substantial difference in the median t_b for floods and debris flows (11 and 9 min, respectively); however, there are slight, statistically significant differences in the trends of flood and debris flow t_b with basin area, which are presumably related to differences in flow speed between floods and debris flows.
机译:关于大火后山洪和泥石流的特定时间的数据非常有限。我们描述了一种使用低成本的压力传感器来测量小型燃烧流域对降雨的响应时间的方法,该传感器可以在火灾后迅速安装。尽管压力传感器的设计不适合在更先进的泥石流监测站点使用快速采样率(≤2 s)进行持续采样,但与高频阶段数据的比较表明,以1分钟为间隔测量的压力峰值足以检测到大多数泥石流和洪水的通过。事件后现场访问用于测量高峰期并根据沉积物特征识别流量类型。通过分析流量压力和5分钟降雨强度的时间序列之间的相互关系,确定在每个站点产生流量的流域响应时间尺度(t_b)。在加利福尼亚州南部的15个流域(≤1.4km〜2)中,有40次火灾后洪水和11次火灾后泥石流记录,发现该时间尺度小于30分钟。包括在另外5个仪器先进的监测站记录的来自其他24个泥石流的数据,我们发现洪水和泥石流的中值t_b并没有实质性差异(分别为11分钟和9分钟);但是,洪水和泥石流趋势t_b随流域面积的变化在统计上有细微的差异,这大概与洪水和泥石流之间的流速差异有关。

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  • 来源
    《Water resources research》 |2012年第5期|p.W05516.1-W05516.8|共8页
  • 作者单位

    U.S. Geological Survey, Box 25046, Denver Federal Center, Denver, CO 80225, USA;

    U.S. Geological Survey, Box 25046, Denver Federal Center, Denver, CO 80225, USA;

    U.S. Geological Survey, 525 S. Wilson Ave., Pasadena, CA 91106, USA;

    U.S. Geological Survey, 345 Middlefield Rd., Menlo Park, CA 94025, USA;

    U.S. Geological Survey, Box 25046, Denver Federal Center, Denver, CO 80225, USA;

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