首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Reply to Comment by W. R. Peltier, D. F. Argus, and R. Drummond on “An Assessment of the ICE6G_C (VM5a) Glacial Isostatic Adjustment Model”

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Reply to Comment by W. R. Peltier, D. F. Argus, and R. Drummond on “An Assessment of the ICE6G_C (VM5a) Glacial Isostatic Adjustment Model”

机译：回复W. R. Peltier，D.F.Farus和R. Drummond的评论评估“ICE6G_C（VM5A）冰川等静态调整模型的评估”

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Abstract > The empirical approximation of Purcell et al. (2011, https://doi.org/10.1029/2011GL048624) has been validated by Peltier et al. (2018, https://doi.org/10.1002/2016JB013844). In their Comment they introduced new results derived from the same ice/rheology models of ICE6G_C (VM5a) but using a different model for Antarctic bathymetry. This has greatly reduced the differences in predicted Antarctic uplift rates relative to those of Purcell et al. (2016, https://doi.org/10.1002/2015JB012742). In fact, with a ～50% reduction in uplift rate in the Weddell Sea, the results of Peltier et al. (2018, https://doi.org/10.1002/2016JB013844) now agree more closely with the predictions of Purcell et al. (2016, https://doi.org/10.1002/2015JB012742) than with the original ICE6G_C values. Peltier et al. (2018, https://doi.org/10.1002/2016JB013844) state that the high power in their high‐frequency spherical harmonic coefficients remains in their new calculations. They also claim that Purcell et al. (2016, https://doi.org/10.1002/2015JB012742) used an inaccurate loading history in deriving their velocity field. In fact, the ice load history was unchanged; to remove any ambiguity, the ice and water load histories used in the CALSEA calculations are provided in the href="#jgrb52445-supinf-0001">supporting information</link> . </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：Lang =“en”XML：ID =“JGRB52445-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> > Purcell等人的经验逼近。（2011年，HTTPS://Doi.org/10.1029/2011GL048624）已由Peltier等人验证。（2018，https://doi.org/10.1002/2016JB013844）。在评论中，他们引入了来自ICE6G_C（VM5A）的相同冰/流变模型的新结果，但使用不同的南极浴型模型。这极大地降低了相对于purcell等人的预测南极提升速率的差异。（2016，https://doi.org/10.1002/2015JB012742）。事实上，在韦德尔海中的提升速率降低了〜50％，Peltier等人的结果。（2018年，https://doi.org/10.1002/2016jb013844）现在与Purcell等人的预测更密切。（2016，https://doi.org/10.1002/2015JB012742）与原始ICE6G_C值相比。 Peltier等。（2018年，HTTPS://Doi.org/10.1002/2016JB013844）状态下，其高频球形谐波系数的高功率仍然处于新的计算中。他们还声称purcell等。（2016，https://doi.org/10.1002/2015JB012742）使用了导出其速度字段的不准确的加载历史记录。事实上，冰负荷历史没有变化;为了消除任何模糊性，在<链路Href =“#jgrb52445-supinf-0001”>支持信息</ link>中提供了CALSEA计算中使用的冰和水负荷历史。 </ 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>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共4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=Purcell A.&option=202" target="_blank" rel="nofollow">Purcell A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tregoning P.&option=202" target="_blank" rel="nofollow">Tregoning P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dehecq A.&option=202" target="_blank" rel="nofollow">Dehecq A.;</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>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</p> <p>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</p> <p>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</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=glacio‐isostatic modeling&option=203" rel="nofollow">glacio‐isostatic modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Antarctic uplift rates&option=203" rel="nofollow">Antarctic uplift rates;</a> </p> <div class="translation"> 机译：Glacio-iSostatic建模;南极提升速率; </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/0704025592803.html">Reply to Comment by W. 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