Time Variations in Ocean Bottom Pressure from a Few Hours to Many Years: In Situ Data, Numerical Models, and GRACE Satellite Gravimetry

Poropat L.; Dobslaw H.; Zhang L.; Macrander A.; Boebel O.; Thomas M.

摘要

Abstract >In situ ocean bottom pressure (OBP) obtained from 154 different locations irregularly scattered over the globe is carefully processed to isolate signals related to the ocean general circulation and large‐scale sea level changes. Comparison against a global numerical ocean model experiment indicates poor correspondence for periods below 24?hr, possibly related to residual tidal signals and small timing errors in the atmospheric forcing applied to the ocean model. Correspondence increases rapidly for periods between 3?and 10?days, where wind‐driven dynamics are already well understood and consequently well implemented into numerical models. Coherence decreases again for periods around 30?days and longer, where processes not implemented into ocean general circulation models as barystatic sea level changes become more important. Correspondence between in situ data and satellite‐based OBP as obtained from the Gravity Recovery and Climate Experiment (GRACE) German Research Centre for Geosciences RL05a gravity fields critically depends on the postprocessing of Level‐2 Stokes coefficients that also includes the selection of appropriate averaging regions for the GRACE‐based mass anomalies. The assessment of other available GRACE Level‐2 products indicates even better fit of more recent solutions as ITSG‐Grace2016 and the Center for Space Research and Jet Propulsion Laboratory RL05 mascons. In view of the strong high‐frequency component of OBP, however, a higher temporal resolution of the oceanic GRACE products would be rather advantageous. </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 =“JGRC23031-Abs-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> >原位海底压力（OBP）从154个不同的位置获得，不规则地分散在全球上，被仔细加工以隔离与海洋一般循环和大规模海平面变化有关的信号。针对全局数值海洋模型实验的比较表明，在24小时以下的时期对应不良，可能与残留的潮汐信号相关和应用于海洋模型的大气强制中的小定时误差。通信在3°之间的时间内迅速增加？和10个？天，其中风力驱动的动态已经很好地理解并因此充分利用到数值模型中。连贯性再次减少30个？天和更长的时间，其中未实施到海洋一般循环模型中的过程，随着尺态的海平面变化变得更加重要。从重力恢复和气候实验（Grace）Geosciences Geosciences RL05A重力场获得的原位数据和卫星基于卫星的OBP之间的对应关系尺寸重视尺寸依赖于第2级斯托克斯系数的后处理，其还包括适当平均区域的选择对于基于恩典的质量异常。评估其他可用的恩惠第2级产品表示甚至更好地适合最近的解决方案作为ITSG-Grace2016，以及空间研究和喷射推进实验室RL05吉祥物中心。然而，鉴于OBP的强高频分量，海洋恩典产品的较高时间分辨率将是相当优势的。</ 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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR 》</a> <b style="margin: 0 2px;">|</b><span>2018年第8期</span><b style="margin: 0 2px;">|</b> <span>共12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=Poropat L.&option=202" target="_blank" rel="nofollow">Poropat L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dobslaw H.&option=202" target="_blank" rel="nofollow">Dobslaw H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang L.&option=202" target="_blank" rel="nofollow">Zhang L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Macrander A.&option=202" target="_blank" rel="nofollow">Macrander A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boebel O.&option=202" target="_blank" rel="nofollow">Boebel O.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thomas M.&option=202" target="_blank" rel="nofollow">Thomas M.;</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 1: GeodesyGFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Department 1: GeodesyGFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Department 1: GeodesyGFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Marine and Freshwater Research InstituteReykjavík Iceland;</p> <p>Alfred Wegener Institute for Polar und Marine ResearchBremerhaven Germany;</p> <p>Department 1: GeodesyGFZ German Research Centre for GeosciencesPotsdam 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;"> </p> </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/0704025579715.html">Time Variations in Ocean Bottom Pressure from a Few Hours to Many Years: In Situ Data, Numerical Models, and GRACE Satellite Gravimetry</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Poropat L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Poropat L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dobslaw H.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dobslaw H.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang L.,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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