2000年和2001年发生在蒙大拿州的野火引发的洪水和泥石流

C. Parrett, S. Cannon, K. Pierce
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引用次数: 29

摘要

继2000年夏季大规模野火之后,蒙大拿州在三个不同的烧伤区域经历了洪水和泥石流:(1)蒙大拿州西南部的比特鲁特地区,(2)海伦娜附近的峡谷渡口地区,(3)蒙大拿州东南部的阿什兰地区。2000年9月至10月,比特鲁特研究区域的洪水和泥石流开始于一场大的锋面风暴。在被烧地区没有降水资料。在比特根烧伤区附近的一个国家气象站,日降水量的复发间隔约为10年。风暴导致了泥石流和小睡童河的洪峰,其复发间隔约为100年。7月
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Wildfire-related floods and debris flows in Montana in 2000 and 2001
Following extensive wildfires in summer 2000, Montana experienced flooding and debris flows in three different burned areas: (1) the Bitterroot area in southwestern Montana, (2) the Canyon Ferry area near Helena, and (3) the Ashland area in southeastern Montana. Flooding and debris flows in the Bitterroot study area began with a large, frontal storm in September-October 2000. No precipitation data were available at sites in the burned area. Daily precipitation at one National Weather Service station near the Bitterroot burn area had a recurrence interval of about 10 years. The storm resulted in debris flows and a peak flood discharge on Little Sleeping Child Creek that had a recurrence interval of about 100 years. July
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