The influence of climate and microclimate (aspect) on soil creep efficiency: Cinder cone morphology and evolution along the eastern Mediterranean Golan Heights

机译：气候和微气密（方面）对土壤蠕变效率的影响：粉碎地中海戈兰高地的煤粉锥形态和进化

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Abstract > Although hillslope evolution has been subject to much investigation for more than a century, the effect of climate on the morphology of soil‐mantled hillslopes remains poorly constrained. In this study, we perform numerical simulations of volcanic cinder cones in the Golan Heights (eastern Mediterranean) to estimate soil transport efficiency across a significant north–south gradient in mean annual precipitation (1100 to 500?mm). We use the initial cinder cone morphology (constrained by stratigraphy), the modern hillslope form (surveyed with sub‐meter accuracy) and the eruption age (based on 40 Ar– 39 Ar chronology) to predict the best‐fit value of the soil transport coefficient (‘diffusivity’) based on a nonlinear transport model. Our results indicate that the best‐fit diffusivity ( <fi>K</fi> ) varies from 1 to 6?m 2 ?ka ?1 among the five cinder cones in our field area. Diffusivity ( <fi>K</fi> ) values vary systematically with precipitation and hillslope aspect; specifically, <fi>K</fi> is higher on south‐facing (drier) hillslopes and decreases with mean annual precipitation. We interpret this climate dependency to reflect vegetation‐driven variations in apparent soil cohesion, which increases with root network density, and attenuation of rain splash and overland flow erosion, which increases with vegetative ground cover. To assess how vegetative root mass and ground cover vary with precipitation and aspect, we quantified the spatial distribution of NDVI (normalized difference vegetation index) from ASTER satellite images and observed spatial variations that correlate with our calibrated values of <fi>K</fi> . Analysis of prev </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> >虽然是hillslope进化已经受到多个世纪以来的大量调查的影响，气候对土着山坡的形态的影响仍然受到严重的影响。在这项研究中，我们在戈兰高地（东部地中海）中对火山煤渣锥体进行了数值模拟，以估计在平均年降水量（1100至500？mm）中估算在一个重要的南北梯度上的土壤运输效率。我们使用初始煤渣形态（由地层限制），现代山坡形式（用亚米精度调查）和喷发年龄（基于 40 </ sup> ar- 39 </ sup>基于非线性传输模型，AR时间顺序）预测土壤输送系数（'扩散率'）的最佳拟合值。我们的结果表明，最佳拟合扩散率（<fi> k </ fi>）在五个煤粉锥中的1至6Ωm 2 </ sup>中变化。在我们的领域。扩散性（<fi> k </ fi>）值随着沉淀和山坡方面系统地系统地变化;具体而言，朝南（干燥器）山坡上的<fi> k </ fi>与平均年降水量减少。我们解释这种气候依赖，反映明显的土壤凝聚力的植被驱动的变化，随着根网络密度增加，雨水和陆上流动侵蚀的衰减增加了植物地面覆盖。为了评估植物生根质量和地面覆盖如何随沉淀和方面而变化，我们量化了来自紫迹卫星图像的NDVI（归一化差异植被指数）的空间分布，并观察到与我们校准的<fi> k </ fi的校准值相关的空间变化>。普遍分析 </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14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=Ben‐Asher Matan&option=202" target="_blank" rel="nofollow">Ben‐Asher Matan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haviv Itai&option=202" target="_blank" rel="nofollow">Haviv Itai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Roering Joshua J.&option=202" target="_blank" rel="nofollow">Roering Joshua J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Crouvi Onn&option=202" target="_blank" rel="nofollow">Crouvi Onn;</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 Geological and Environmental SciencesBen Gurion University of the NegevBeer‐Sheva Israel;</p> <p>Department of Geological and Environmental SciencesBen Gurion University of the NegevBeer‐Sheva Israel;</p> <p>Department of Geological SciencesUniversity of OregonEugene OR 97403 USA;</p> <p>Geological Survey of IsraelJerusalem Israel;</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=hillslope evolution&option=203" rel="nofollow">hillslope evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soil creep&option=203" rel="nofollow">soil creep;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=nonlinear diffusion&option=203" rel="nofollow">nonlinear diffusion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=landscape evolution&option=203" rel="nofollow">landscape evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=aspect asymmetry&option=203" rel="nofollow">aspect asymmetry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cinder cones&option=203" rel="nofollow">cinder cones;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=NDVI&option=203" rel="nofollow">NDVI;</a> </p> <div class="translation"> 机译：Hillslope Evolution;土壤蠕变;非线性扩散;景观进化;突出不对称;煤渣锥;NDVI; </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/0704023139148.html">The influence of climate and microclimate (aspect) on soil creep 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