Comparison of geomorphological field mapping and 2D‐InSAR mapping of periglacial landscape activity at Nordnesfjellet, northern Norway

机译：挪威北部北部近翼景观活动的地貌景观活动与2D-Insar映射的比较

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Abstract >The ability to continuously monitor the dynamic response of periglacial landforms in a climate change context is of increasing scientific interest. Satellite radar interferometry provides information on surface displacement that can be related to periglacial processes. Here we present a comparison of two‐dimensional (2D) surface displacement rates and geomorphological mapping at periglacial landform and sediment scale from the mountain Nordnesfjellet in northern Norway. Hence, 2D Interferometric Synthetic Aperture Radar (InSAR) results stem from a 2009–2014 TerraSAR‐X dataset from ascending and descending orbits, decomposed into horizontal displacement vectors along an east–west plane, vertical displacement vectors and combined displacement velocity. Geomorphological mapping was carried out on aerial imagery and validated in the field. This detailed landform and sediment type mapping revealed an altitudinal distribution dominated by, weathered bedrock blockfields, surrounded primarily by slightly, to non‐vegetated solifluction landforms at the mountain tops. Below, an active rockslide and associated rockfall deposits are located on the steep east‐facing side of the study area, whereas glacial sediments dominate on the gentler western side. We show that 2D InSAR correctly depicts displacement rates that can be associated with typical deformation patterns for flat‐lying or inclined landforms, within and below the regional permafrost limit, for both wet and dry areas. A net lowering of the entire landscape caused by general denudation of the periglacial landforms and sediments is here quantified for the first time using radar remote sensing. Copyright ? 2018 John Wiley & Sons, Ltd. </abstract> </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”> <标题类型=“main”>抽象</ title> >的能力为了不断监测气候变化中褶皱地貌的动态响应，环境越来越大。卫星雷达干涉测量提供有关表面位移的信息，这些信息可能与褶皱过程有关。在这里，我们展示了二维（2D）表面位移率和地貌映射在挪威北部山上山峰山峰的褶皱地貌和沉积物等级的比较。因此，2D干涉式合成孔径雷达（INSAR）结果由2009-2014 Terrasar-X数据集源于上升和下降轨道，沿着东西飞机，垂直位移向量和组合的位移速度分解成水平位移向量。地貌映射在空中图像上进行并在现场验证。这种详细的地貌和沉积物型映射显示了一个由风化的基岩块底座主导的高度分配，主要由略微略微包围，在山顶上的非植被求扎地貌。下面，一个活跃的摇滚滑坡和相关的岩石矿床位于研究区的陡峭东侧侧，而冰川沉积物在温门特的西方占主导地位。我们表明，2D Insar正确地描绘了可以与用于潮湿和干燥区域的扁平躺线或倾斜地形，内部和低于区域永久区域的典型变形模式相关联的位移率。通过雷达遥感首次定量由褶皱地貌和沉积物的一般剥蚀引起的整个景观的净降低。版权？ 2018年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </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10期</span><b style="margin: 0 2px;">|</b><span>共10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=Eckerstorfer Markus&option=202" target="_blank" rel="nofollow">Eckerstorfer Markus;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eriksen Harald ?verli&option=202" target="_blank" rel="nofollow">Eriksen Harald ?verli;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rouyet Line&option=202" target="_blank" rel="nofollow">Rouyet Line;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Christiansen Hanne H.&option=202" target="_blank" rel="nofollow">Christiansen Hanne H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lauknes Tom Rune&option=202" target="_blank" rel="nofollow">Lauknes Tom Rune;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Blikra Lars Harald&option=202" target="_blank" rel="nofollow">Blikra Lars Harald;</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>NorutTroms? Norway;</p> <p>NorutTroms? Norway;</p> <p>NorutTroms? Norway;</p> <p>Arctic Geology DepartmentThe University Centre in Svalbard UNISLongyearbyen Norway;</p> <p>NorutTroms? Norway;</p> <p>Norwegian Water Resources and Energy DirectorateNVEOslo Norway;</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=2D InSAR&option=203" rel="nofollow">2D InSAR;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=periglacial landforms&option=203" rel="nofollow">periglacial landforms;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geomorphological mapping&option=203" rel="nofollow">geomorphological mapping;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=remote sensing&option=203" rel="nofollow">remote sensing;</a> </p> <div class="translation"> 机译：2D INSAR;褶皱地貌;地貌映射;遥感; 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