Reconstructing extreme post‐wildfire floods: a comparison of convective and mesoscale events

机译：重建极端野火洪水：对流和迈空活动的比较

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Abstract > In much of western United States destructive floods after wildfire are frequently caused by localized, short‐duration convective thunderstorms; however, little is known about post‐fire flooding from longer‐duration, low‐intensity mesoscale storms. In this study we estimate and compare peak flows from convective and mesoscale floods following the 2012 High Park Fire in the ungaged 15.5?km 2 Skin Gulch basin in the northcentral Colorado Front Range. The convective storm on 6 July 2012 came just days after the wildfire was contained. Radar data indicated that the total rainfall was 20–47?mm, and the maximum rainfall intensities (upwards of 50?mm h ?1 ) were concentrated over portions of the watershed that burned at high severity. The mesoscale storm on 9–15 September 2013 produced 220–240?mm of rain but had maximum 15‐min intensities of only 25–32?mm h ?1 . > Peak flows for each flood were estimated using three independent techniques. Our best estimate using a 2D hydraulic model was 28?m 3 ?s ?1 ?km ?2 for the flood following the convective storm, placing it among the largest rainfall‐runoff floods per unit area in the United States. In contrast, the flood associated with the mesoscale flood was only 6?m 3 ?s ?1 ?km ?2 , but the long‐duration flood caused extensive channel incision and widening, indicating that this storm was much more geomorphically effective. The peak flow estimates for the 2013 flood had a higher relative uncertainty and this stemmed from whether we used pre‐ or post‐flood channel topography. The results doc </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> >美国西部的破坏性洪水经常由本地化，短期对流雷暴引起;然而，对于从更长持续时间，低强度的Mescle Storms的火灾后洪水知之甚少。在这项研究中，我们在2012年在Nortgaged 15.5？Km <Sup> 2 </ Sup>皮肤遮阳篷中估算和比较和Mesoscale洪水从对流和Mesoscale洪水中的峰值流动的峰值流动在NorthCentral Colorado前方范围内。 2012年7月6日的对流风暴仅次于野火的几天内。雷达数据表明，总降雨量为20-47Ωmm，最大的降雨强度（向上的50？mm H 1）集中在高度严重程度下燃烧的分水物的部分上。 2013年9月9日至15日的Mesoscale Storm制作了220-240毫米的雨，但最多15分钟的强度仅为25-32？mm h ？1 </ sup>。使用三种独立技术估计每个洪水的峰值。我们使用2D液压模型的最佳估计为28？m 3 </ sup>？s 1 </ sup>？mm 2 </ sup>在对流风暴之后的洪水，将它放在美国每单位面积的最大降雨洪水中。相比之下，与mesoscale洪水相关的洪水仅为6？m 3 </ sup>？s ？1 </ sup>？Km 2 </ sup>，但长 - 持续洪水引起了广泛的沟道切口和扩大，表明这场风暴更加良好。 2013洪水的峰值流估计具有更高的相对不确定性，并且这源于我们是否使用过洪水后通道地形。结果Doc. </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第15期</span><b style="margin: 0 2px;">|</b><span>共18页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brogan Daniel J.&option=202" target="_blank" rel="nofollow">Brogan Daniel J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nelson Peter A.&option=202" target="_blank" rel="nofollow">Nelson Peter A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=MacDonald Lee H.&option=202" target="_blank" rel="nofollow">MacDonald Lee H.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Civil and Environmental EngineeringColorado State UniversityFort Collins CO 80523‐1372 USA;</p> <p>Department of Civil and Environmental EngineeringColorado State UniversityFort Collins CO 80523‐1372 USA;</p> <p>Department of Ecosystem Science and SustainabilityColorado State UniversityFort Collins CO 80523‐1476 USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=extreme flooding&option=203" rel="nofollow">extreme flooding;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geomorphology&option=203" rel="nofollow">geomorphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wildfire&option=203" rel="nofollow">wildfire;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydraulics&option=203" rel="nofollow">hydraulics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrology&option=203" rel="nofollow">hydrology;</a> </p> <div class="translation"> 机译：极端洪水;地貌;野火;液压;水文; 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