Landslides control the spatial and temporal variation of channel width in southern Taiwan: Implications for landscape evolution and cascading hazards in steep, tectonically active landscapes

机译：滑坡控制台湾南部沟道宽度的空间和时间变化：对景观进化和级联灾害的影响，构造的强大景观

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Abstract >Intense precipitation or seismic events can generate clustered mass movement processes across a landscape. These rare events have significant impacts on the landscape, however, the rarity of such events leads to uncertainty in how they impact the entire geomorphic system over a range of timescales. Taiwan is steep, tectonically active, and prone to landslide and debris flows, especially when exposed to heavy rainfall events. Typhoon Morakot made landfall in Taiwan in August of 2009, causing widespread landslides in southern Taiwan. The south to north trend in valley relief in southern Taiwan leads to spatial variability in landslide susceptibility providing an opportunity to infer the long‐term impact of such landslide events on channel morphology. We use pre‐ and post‐typhoon imagery to quantify the propagating impact of this event on channel width as the debris is routed through the landscape. The results show the importance of cascading hazards from landslides on landscape evolution based on patterns of channel width (both pre‐ and post‐typhoon) and hillslope gradients in 20 basins along strike in southern Taiwan. Prior to Typhoon Morakot, the river channels in the central part of the study area were about 3–10 times wider than the channels in the south. Following the typhoon, aggradation and widening was also a maximum in these central to northern basins where hillslope gradients and channel steepness is high, accentuating the pre‐typhoon pattern. The results further show that the narrowest channels are located where channel steepness is the lowest, an observation inconsistent with a detachment‐limited model for river evolution. We infer this pattern is indicative of a strong role of sediment supply, and associated landslide events, on long‐term channel evolution. These findings have implications across a range of spati </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> >激烈的降水或地震事件可以在景观中产生聚类批量移动过程。这些罕见的事件对景观产生了重大影响，然而，这些事件的罕见性导致它们如何影响整个几何系统在一系列时间尺度上的不确定性。台湾是陡峭的，根本上活跃，并且容易出现滑坡和碎片流动，特别是在暴露于大雨事件时。 2009年8月，台湾台湾台湾莫拉科特在台湾造成了广泛的滑坡。台湾南部山谷救济的南方趋势导致滑坡易感性的空间可变性，为推断这种滑坡事件对信道形态的长期影响提供了机会。我们使用预先和音风电影图像来量化此事件在频道宽度上的传播影响，因为碎片通过横向路由。结果表明，基于通道宽度（下台风的横向和下部和台风前后）和山坡梯度沿着台湾剧中的山坡梯度的山坡横向进化的景观演变的横向发展的重要性。在台风莫拉科特之前，研究区域的中央部分的河流渠道比南方的频道宽约3-10倍。在台风之后，这些中央山坡梯度和通道陡度高的北部盆地中的北部盆地的巨大，加强了，加强了大量，突出了前风前图案。结果进一步表明，最窄的通道位于信道陡度是最低的地方，观察与河流进化的分离有限的模型不一致。我们推断这种模式表明沉积物供应的强大作用以及长期渠道进化的沉积物供应和相关的滑坡事件。这些调查结果对一系列斯鲜利有影响 </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>2018年第9期</span><b style="margin: 0 2px;">|</b><span>共16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=Yanites Brian J.&option=202" target="_blank" rel="nofollow">Yanites Brian J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mitchell Nate A.&option=202" target="_blank" rel="nofollow">Mitchell Nate A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bregy Joshua C.&option=202" target="_blank" rel="nofollow">Bregy Joshua C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carlson Grace A.&option=202" target="_blank" rel="nofollow">Carlson Grace A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cataldo Kirstyn&option=202" target="_blank" rel="nofollow">Cataldo Kirstyn;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holahan Margaret&option=202" target="_blank" rel="nofollow">Holahan Margaret;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Johnston Graham H.&option=202" target="_blank" rel="nofollow">Johnston Graham H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nelson Amelia&option=202" target="_blank" rel="nofollow">Nelson Amelia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valenza Jeffery&option=202" target="_blank" rel="nofollow">Valenza Jeffery;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wanker Matthew&option=202" target="_blank" rel="nofollow">Wanker Matthew;</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 Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of GeographyIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN;</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=landslides&option=203" rel="nofollow">landslides;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluvial geomorphology&option=203" rel="nofollow">fluvial geomorphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=channel width&option=203" rel="nofollow">channel width;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tectonic geomorphology&option=203" rel="nofollow">tectonic geomorphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hazards&option=203" rel="nofollow">hazards;</a> </p> <div class="translation"> 机译：山体滑坡;河流般的地貌;频道宽度;构造地貌;危险; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 02:29:57</span> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" 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