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Modelling the relative dominance of wave erosion and weathering processes in shore platform development in micro‐ to mega‐tidal settings

机译:在微量到大型潮汐环境中建模波浪侵蚀和风化过程的相对主导地位

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Abstract >In this paper we use a numerical model to explore the relative dominance of two main processes in shore platform development: wave erosion; weathering due to wetting and drying. The modelling approach differs from previous work in several aspects, including: the way that it accounts for weathering arising from gradual surficial intertidal rock degradation; subtidal profile shape development; and the consideration of a broad erosion parameter space in which, at either end of the erosion spectrum, shore platform profiles are produced by waves or weathering alone. Results show that in micro‐tidal settings, wave erosion dominates the evolution of (i) shore platforms that become largely subtidal and (ii) sub‐horizontal shore platforms that have a receding seaward edge. Weathering processes dominate the evolution of sub‐horizontal shore platforms with a stable seaward edge. In contrast, sloping shore platforms in mega‐tidal settings are produced across the full range of the process‐dominance spectrum depending on the how the erosional efficacy of wave erosion and weathering are parameterized. Morphological feedbacks control the process‐dominance. In small tidal environments wave processes are strongly controlled by the presence/absence of an abrupt seaward edge, but this influence is much smaller in large tidal environments due to larger water depths particularly at high tides. In large tidal environments, similar shore platform profile geometries can be produced by either wave‐dominant or weathering‐dominant process regimes. Equifinality in shore platform development has been noted in other studies, but mainly in the context of smaller‐scale (centimetre to metre) erosion features. Here we draw attention to geomorphic equifinality at the scale of the shore platform itself. Progress requires a greater understanding of the actual m </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> >纸张我们使用数字模型来探索岸上平台开发中的两个主要过程的相对主导地位:波浪侵蚀;由于润湿和干燥而耐候。建模方法与以前的工作不同,包括:它占渐进思维岩石降解所产生的风化的方式;阴影型材形状开发;并且考虑了广泛的侵蚀参数空间,其中在侵蚀光谱的任一端,岸平台轮廓由波或耐候仅产生。结果表明,在微潮汐环境中,波浪侵蚀主导了(i)岸平台的演变,这些平台变得基本上是对倒退的海边的副水平岸平台。风化过程主导了稳定的海边缘的亚水平岸平台的演变。相反,根据波浪侵蚀和风化的侵蚀功效如何,在整个过程优势频谱中产生普通潮汐设置中的坡度平台。形态反馈控制过程优势。在小潮汐环境中,波浪过程受到突然的海边的存在/不存在的强烈控制,但由于较大的水深特别是在高潮中,这种影响在大的潮汐环境中大得多。在大型潮汐环境中,类似的岸平台轮廓几何形状可以通过波导或风化的主导过程制度来生产。在其他研究中已经注意到岸上平台开发的平等性,但主要是在较小尺度(厘米到仪表)侵蚀特征的背景下。在这里,我们注意到岸平台本身的规模上的地貌正平。进展需要更好地了解实际的m </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12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=Matsumoto Hironori&option=202" target="_blank" rel="nofollow">Matsumoto Hironori;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dickson Mark E.&option=202" target="_blank" rel="nofollow">Dickson Mark E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kench Paul S.&option=202" target="_blank" rel="nofollow">Kench Paul S.;</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>School of EnvironmentThe University of AucklandAuckland New Zealand;</p> <p>School of EnvironmentThe University of AucklandAuckland New Zealand;</p> <p>School of EnvironmentThe University of AucklandAuckland New Zealand;</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=shore platform&option=203" rel="nofollow">shore platform;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=process dominance&option=203" rel="nofollow">process dominance;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=theoretical model&option=203" rel="nofollow">theoretical model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=equifinality&option=203" rel="nofollow">equifinality;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tidal range&option=203" rel="nofollow">tidal range;</a> </p> <div class="translation"> 机译:岸上平台;过程优势;理论模型;平等;潮汐范围; 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