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Oceanic Residual Topography Agrees With Mantle Flow Predictions at Long Wavelengths

机译：海洋残余地形同意长波长的地幔流预测

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Abstract >Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important prediction made by geodynamic models, but there is an apparent disparity between geodynamic model predictions and estimates of residual topography (total topography minus lithospheric and crustal contributions). We generate synthetic global topography fields with different power spectral slopes and spatial patterns to investigate how well the long‐wavelength (spherical degrees 1 to 3) components can be recovered from a discrete set of samples where residual topography has been recently estimated. An analysis of synthetic topography, along with observed geoid and gravity anomalies, demonstrates the reliability of signal recovery. Appropriate damping factors, which depend on the maximum degree in the spherical harmonic expansion that is used to fit the samples, must be applied to recover the long‐wavelength topography correctly; large damping factors smooth the model excessively and suppress residual topography amplitude and power spectra unrealistically. Recovered long‐wavelength residual topographies based on recent oceanic point‐wise estimates with different spherical expansion degrees agree with each other and with the predicted dynamic topography from mantle flow models. The peak amplitude of the long‐wavelength residual topography from oceanic observations is about 1?km, suggesting an important influence of large‐scale deep mantle flow. </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”> <标题类型=“main”>抽象</ title> >动态地形，由副扫描罩流动引起的表面偏转，是通过地球动力学制作的重要预测模型，但几步模型预测与残余地形的估计之间存在明显的差异（总体地形减去岩石树和地壳贡献）。我们生成具有不同功率谱斜率和空间图案的合成全局地形场，以研究最近估计残留地形的离散样本可以从离散的样本中回收长波长（球面1至3）组分。合成形貌的分析以及观察到的大地形和重力异常，证明了信号恢复的可靠性。必须施加适当的阻尼因子，这取决于用于适合样品的球形谐波膨胀中的最大程度，必须正确施加恢复长波长形貌;大量阻尼因素过度平滑模型，抑制了残余地形幅度和功率光谱。基于最近的近期球形膨胀程度的近期海洋点估计恢复的长波长残余地形彼此同意，并且通过地幔流模型的预测动态地形。来自海洋观测的长波长残余地形的峰值幅度约为1μm，表明大规模深层幔流动的重要影响。</ p> </摘要> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第21期</span><b style="margin: 0 2px;">|</b><span>共11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=Yang Ting&option=202" target="_blank" rel="nofollow">Yang Ting;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moresi Louis&option=202" target="_blank" rel="nofollow">Moresi Louis;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller R. Dietmar&option=202" target="_blank" rel="nofollow">Müller R. Dietmar;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gurnis Michael&option=202" target="_blank" rel="nofollow">Gurnis Michael;</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 Earth SciencesUniversity of MelbourneMelbourne Victoria Australia;</p> <p>School of Earth SciencesUniversity of MelbourneMelbourne Victoria Australia;</p> <p>Earthbyte Group School of GeosciencesUniversity of SydneySydney New South Wales Australia;</p> <p>Seismological LaboratoryCalifornia Institute of TechnologyPasadena CA USA;</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=residual topography&option=203" rel="nofollow">residual topography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dynamic topography&option=203" rel="nofollow">dynamic topography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=long wavelength&option=203" rel="nofollow">long wavelength;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=amplitude&option=203" rel="nofollow">amplitude;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=spatial pattern&option=203" rel="nofollow">spatial pattern;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=damping factors&option=203" rel="nofollow">damping factors;</a> </p> <div class="translation"> 机译：残余地形;动态地形;长波长;幅度;空间模式;阻尼因素; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-19 17:14:12</span> </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/0704019850362.html">Oceanic Residual Topography Agrees With Mantle Flow Predictions at Long Wavelengths</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Ting&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yang Ting,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moresi Louis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Moresi Louis,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller R. 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