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TanDEM‐X Time Series Analysis Reveals Lava Flow Volume and Effusion Rates of the 2012–2013 Tolbachik, Kamchatka Fissure Eruption

机译：tandem-x时间序列分析显示2012-2013 Tolbachik，堪察加裂爆发的熔岩流量和积液率

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Abstract > Assessing eruption volumes is one of the major challenges in volcano research but provides valuable insights into the dynamics of an eruption and the associated hazard. One way to estimate this important parameter is the generation and differencing of digital elevation models (DEMs) acquired before, during, and after an eruption. The satellite mission TanDEM‐X enables generation of time series of DEMs using synthetic aperture radar satellite imagery. We use these data to study the 2012–2013 eruption of Tolbachik in Kamchatka. We developed a processing scheme for generation of 18 DEMs from TanDEM‐X imagery that relies on the generation of a preeruption DEM which is used to process the syneruption and posteruption data pairs. Differencing each DEM with the preeruption DEM enables mapping the lava flows and measuring lava flow volume over time and to estimate lava extrusion rates. We find a final lava flow volume of 0.53?km 3 covering an area of 36?km 2 by the end of the eruption. An uncertainty analysis is performed while analyzing the DEM differences in areas where no topographic change is expected, leading to an error of ±0.01?km 3 for the final lava flow volume. The lava effusion was with 247.92?m 3 /s very high in the first days of the eruption and rapidly decayed toward its end. While many basaltic eruptions follow an exponentially decaying flow model, the extrusion rates at Tolbachik are more compatible with a 1/ t model. This special characteristic might be useful to gain further insight into the eruption process at Tolbachik. </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 Type =“Main”XML：ID =“JGRB52345-Abs-Abs-0001”XML：Lang =“en”> <标题类型=“main”> Abstract </ title> >评估爆发卷是主要的火山研究中的挑战，但为爆发和相关危害的动态提供了有价值的见解。估计这一重要参数的一种方法是在爆发之前，期间和之后获得的数字高度模型（DEM）的生成和差异。使用合成孔径雷达卫星图像，卫星任务TANDEM-X能够产生时间序列的DEMS。我们使用这些数据来研究2012-2013在堪察加的ToLbachik爆发。我们开发了一种从Tandem-X图像生成18个DEM的处理方案，它依赖于生成用于处理增效和后后数据对的预先发生的。差异与预培解DEM的每个DEM使熔岩流动和测量熔岩流量随着时间的推移和估计熔岩挤出率。我们发现最终的熔岩流量为0.53 km 3 </ sup>在喷发结束时覆盖36 km 2 2 </ sup>的区域。在不预期地形变化的区域分析DEM差异的同时执行不确定性分析，导致最终熔岩流量的±0.01 km 3 </ sup>的误差。熔岩积液在火山喷发的第一天且非常高的247.92？m 3 </ sup> / s非常高。虽然许多玄武岩爆发遵循指数衰减的流动模型，但托巴奇克的挤出速率与1 / 模型更加兼容。这种特色可能有助于进一步了解托巴奇克的喷发过程。 </ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第10期</span><b style="margin: 0 2px;">|</b><span>共21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=Kubanek Julia&option=202" target="_blank" rel="nofollow">Kubanek Julia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Westerhaus Malte&option=202" target="_blank" rel="nofollow">Westerhaus Malte;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heck Bernhard&option=202" target="_blank" rel="nofollow">Heck Bernhard;</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 Planetary SciencesMcGill UniversityMontreal Quebec Canada;</p> <p>Geodetic InstituteKarlsruhe Institute of TechnologyKarlsruhe Germany;</p> <p>Geodetic InstituteKarlsruhe Institute of TechnologyKarlsruhe Germany;</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=Tolbachik&option=203" rel="nofollow">Tolbachik;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kamchatka&option=203" rel="nofollow">Kamchatka;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=TanDEM‐X&option=203" rel="nofollow">TanDEM‐X;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=topographic change&option=203" rel="nofollow">topographic change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=2012–2013 fissure eruption&option=203" rel="nofollow">2012–2013 fissure eruption;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=digital elevation model&option=203" rel="nofollow">digital elevation model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lava flow volume&option=203" rel="nofollow">lava flow volume;</a> </p> <div class="translation"> 机译：TOTBACHIK;KAMCHATKA;TANDEM-X;地形变化;2012-2013裂缝爆发;数字高度模型;熔岩流量; </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> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704020652095.html">TanDEM-X Time Series Analysis Reveals Lava Flow Volume and Effusion Rates of the 2012-2013 Tolbachik, Kamchatka Fissure Eruption</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kubanek Julia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kubanek Julia,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Westerhaus Malte&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Westerhaus Malte,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heck Bernhard&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Heck Bernhard </a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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