Agreement of CMIP5 Simulated and Observed Ocean Anthropogenic CO        <sub >2</sub>2        Uptake

Bronselaer Benjamin; Winton Michael; Russell Joellen; Sabine Christopher L.; Khatiwala Samar

摘要

Abstract >Previous studies found large biases between individual observational and model estimates of historical ocean anthropogenic carbon uptake. We show that the largest bias between the Coupled Model Intercomparison Project phase 5 (CMIP5) ensemble mean and between two observational estimates of ocean anthropogenic carbon is due to a difference in start date. After adjusting the CMIP5 and observational estimates to the 1791–1995 period, all three carbon uptake estimates agree to within 3?Pg of C, about 4% of the total. The CMIP5 ensemble mean spatial bias compared to the observations is generally smaller than the observational error, apart from a negative bias in the Southern Ocean and a positive bias in the Southern Indian and Pacific Oceans compensating each other in the global mean. This dipole pattern is likely due to an equatorward and weak bias in the position of Southern Hemisphere westerlies and lack of mode and intermediate water ventilation. </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><抽象类型= “主要” 的xml：LANG = “en” 的XML：ID = “grl56674-ABS-0001”> <标题类型= “主”>抽象</ TITLE> <P>先前的研究发现，较大的个体的观察之间的偏差历史海洋人为碳吸收的模型估计。我们表明，耦合模型相互比较项目阶段5（CMIP5）集合均值和海洋人为碳的两个观察估计之间的最大偏差是由于开始日期的差异。在调整CMIP5和观察估计到1791-1995期后，所有三种碳摄取估计值都在3？PG的C中同意，约占总量的4％。相比观测CMIP5集合平均的空间偏差一般比观测误差较小，除了在南大洋负偏置，并在南印度洋和太平洋正偏置于全球平均补偿对方。这种偶极模式可能是由于南半球威斯利普的位置和缺乏模式和中间水通风的赤道和弱偏差。</ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第24期</span><b style="margin: 0 2px;">|</b><span>共8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=Bronselaer Benjamin&option=202" target="_blank" rel="nofollow">Bronselaer Benjamin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Winton Michael&option=202" target="_blank" rel="nofollow">Winton Michael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Russell Joellen&option=202" target="_blank" rel="nofollow">Russell Joellen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sabine Christopher L.&option=202" target="_blank" rel="nofollow">Sabine Christopher L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Khatiwala Samar&option=202" target="_blank" rel="nofollow">Khatiwala Samar;</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>Geophysical Fluid Dynamics LaboratoryPrinceton NJ USA;</p> <p>Geophysical Fluid Dynamics LaboratoryPrinceton NJ USA;</p> <p>Department of GeosciencesUniversity of ArizonaTucson AZ USA;</p> <p>NOAA Pacific Marine Environmental LaboratorySeattle WA USA;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</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=ocean carbon&option=203" rel="nofollow">ocean carbon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CMIP5&option=203" rel="nofollow">CMIP5;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=anthropogenic carbon&option=203" rel="nofollow">anthropogenic carbon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=impulse response function&option=203" rel="nofollow">impulse response function;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=observations&option=203" rel="nofollow">observations;</a> </p> <div class="translation"> 机译：海洋碳;CMIP5;人为碳;脉冲响应函数;观察; 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Agreement of CMIP5 Simulated and Observed Ocean Anthropogenic CO 22 Uptake

摘要

Agreement of CMIP5 Simulated and Observed Ocean Anthropogenic CO ₂2 Uptake