A regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes

机译：加利福尼亚州潮湿冬季沿海流域的沉积物出口制度转变：对横向反应潮流性极端的景观反应的影响

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Abstract >Small, steep watersheds are prolific sediment sources from which sediment flux is highly sensitive to climatic changes. Storm intensity and frequency are widely expected to increase during the 21st century, and so assessing the response of small, steep watersheds to extreme rainfall is essential to understanding landscape response to climate change. During record winter rainfall in 2016–2017, the San Lorenzo River, coastal California, had nine flow peaks representing 2–10‐year flood magnitudes. By the third flood, fluvial suspended sediment showed a regime shift to greater and coarser sediment supply, coincident with numerous landslides in the watershed. Even with no singular catastrophic flood, these flows exported more than half as much sediment as had a 100‐year flood 35?years earlier, substantially enlarging the nearshore delta. Annual sediment load in 2017 was an order of magnitude greater than during an average‐rainfall year, and 500‐fold greater than in a recent drought. These anomalous sediment inputs are critical to the coastal littoral system, delivering enough sediment, sometimes over only a few days, to maintain beaches for several years. Future projections of megadroughts punctuated by major atmospheric‐river storm activity suggest that interannual sediment‐yield variations will become more extreme than today in the western USA, with potential consequences for coastal management, ecosystems, and water‐storage capacity. The occurrence of two years with major sediment export over the past 35?years that were not associated with extremes of the El Ni?o Southern Oscillation or Pacific Decadal Oscillation suggests caution in interpreting climatic signals from marine sedimentary deposits derived from small, steep, coastal watersheds, to avoid misinterpreting the frequencies of those cycles. Published 2018. This articl </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> > small，陡峭的流域是沉积物通量对气候变化高度敏感的多产沉积物来源。风暴强度和频率在21世纪中普遍预期增加，因此评估小，陡峭的流域对极端降雨的反应对于了解气候变化的景观应对至关重要。在2016 - 2017年冬季降雨期间，沿海加利福尼亚州圣洛伦佐河有九个流量峰值，代表2-10年的洪水峰值。通过第三次洪水，河流悬浮沉积物显示出更大且粗糙的沉积物供应的制度转变，与流域中的许多山体滑坡一致。即使没有奇异的灾难性洪水，这些流量也会出口超过一半的沉积物，因为100年前的洪水35次？年前，大幅扩大了近岸三角洲。 2017年度沉积物负荷大于平均降雨年龄的数量级，比最近的干旱在500倍。这些异常沉积物输入对沿海沿海系统至关重要，提供足够的沉积物，有时只超过几天，以保持海滩几年。主要大气河河风暴活动标点的未来预测表明，持续沉积物 - 产量变化比今天在美国西部的终际沉积物变化会变得更加极端，对沿海管理，生态系统和储水能力进行潜在后果。在过去的35年中，两年的主要沉积物出口发生了两年？南部振荡或太平洋二等振荡的极端与极端有关的年份表明，在解释来自小型，陡峭，沿海的海洋沉积沉积物的气候信号中提出了谨慎流域，避免误解这些周期的频率。 2018年出版。这个articl </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12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=East Amy E.&option=202" target="_blank" rel="nofollow">East Amy E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stevens Andrew W.&option=202" target="_blank" rel="nofollow">Stevens Andrew W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ritchie Andrew C.&option=202" target="_blank" rel="nofollow">Ritchie Andrew C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barnard Patrick L.&option=202" target="_blank" rel="nofollow">Barnard Patrick L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Campbell‐Swarzenski Pamela&option=202" target="_blank" rel="nofollow">Campbell‐Swarzenski Pamela;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Collins Brian D.&option=202" target="_blank" rel="nofollow">Collins Brian D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Conaway Christopher H.&option=202" target="_blank" rel="nofollow">Conaway Christopher 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>US Geological Survey Pacific Coastal and Marine Science CenterSanta Cruz CA 95060 USA;</p> <p>US Geological Survey Pacific Coastal and Marine Science CenterSanta Cruz CA 95060 USA;</p> <p>US Geological Survey Pacific Coastal and Marine Science CenterSanta Cruz CA 95060 USA;</p> <p>US Geological Survey Pacific Coastal and Marine Science CenterSanta Cruz CA 95060 USA;</p> <p>US Geological Survey Pacific Coastal and Marine Science CenterSanta Cruz CA 95060 USA;</p> <p>US Geological Survey Geology Minerals Energy &</p> <p>Geophysics Science CenterMenlo Park CA 94025 USA;</p> <p>US Geological Survey National Research ProgramMenlo Park CA 94025 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=natural hazards&option=203" rel="nofollow">natural hazards;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=suspended sediment&option=203" rel="nofollow">suspended sediment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment load&option=203" rel="nofollow">sediment load;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=floods&option=203" rel="nofollow">floods;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=coastal watershed&option=203" rel="nofollow">coastal watershed;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=climate change&option=203" rel="nofollow">climate change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=extreme events&option=203" rel="nofollow">extreme events;</a> </p> <div class="translation"> 机译：自然灾害;悬浮沉积物;沉积物负荷;洪水;沿海流域;气候变化;极端事件; </div> </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023138776.html">A regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=East Amy E.&option=202" 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