Simulation of Volume and Heat Transport along 26.5°N in the Atlantic
The observed meridional overtuming circula- tion （MOC） and meridional heat transport （MHT） estimated from the Rapid Climate Change/Meridional Circu- lation and Heat Flux Array （RAPID/MOCHA） at 26.5°N are used to evaluate the volume and heat transport in the eddy-resolving model LASG/IAP Climate syst...
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| creator | MO Hui-Er YU Yong-Qiang |
| description | The observed meridional overtuming circula- tion （MOC） and meridional heat transport （MHT） estimated from the Rapid Climate Change/Meridional Circu- lation and Heat Flux Array （RAPID/MOCHA） at 26.5°N are used to evaluate the volume and heat transport in the eddy-resolving model LASG/IAP Climate system Ocean Model （LICOM）. The authors find that the Florida Cur- rent transport and upper mid-ocean transport of the model are underestimated against the observations. The simulated variability of MOC and MHT show a high correlation with the observations, exceeding 0.6. Both the simulated and observed MOC and MHT show a significant seasonal variability. According to the power spectrum analysis, LICOM can represent the mesoscale eddy characteristic of the MOC similar to the observation. The model shows a high correlation of 0.58 for the internal upper mid-ocean transport （MO） and a density difference between the western and eastern boundaries, as noted in previous studies. |
| doi_str_mv | 10.1080/16742834.2012.11447019 |
| format | Article |
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The authors find that the Florida Cur- rent transport and upper mid-ocean transport of the model are underestimated against the observations. The simulated variability of MOC and MHT show a high correlation with the observations, exceeding 0.6. Both the simulated and observed MOC and MHT show a significant seasonal variability. According to the power spectrum analysis, LICOM can represent the mesoscale eddy characteristic of the MOC similar to the observation. The model shows a high correlation of 0.58 for the internal upper mid-ocean transport （MO） and a density difference between the western and eastern boundaries, as noted in previous studies.</description><identifier>ISSN: 1674-2834</identifier><identifier>EISSN: 2376-6123</identifier><identifier>DOI: 10.1080/16742834.2012.11447019</identifier><language>eng</language><publisher>Beijing: Routledge</publisher><subject>Climate change ; Climate system ; Correlation ; eddy-resolving ; Heat transfer ; Heat transport ; meridional heat transport ; meridional overturning circulation ; Ocean circulation ; Seasonal variation ; Seasonal variations ; Temperature ; Transport ; variability ; 中尺度涡 ; 佛罗里达州 ; 大西洋 ; 快速气候变化 ; 模拟量 ; 海洋运输 ; 热量传递 ; 经向环流</subject><ispartof>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2012, Vol.5 (5), p.373-378</ispartof><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences 2012</rights><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences. 2012</rights><rights>Copyright © Wanfang Data Co. 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The authors find that the Florida Cur- rent transport and upper mid-ocean transport of the model are underestimated against the observations. The simulated variability of MOC and MHT show a high correlation with the observations, exceeding 0.6. Both the simulated and observed MOC and MHT show a significant seasonal variability. According to the power spectrum analysis, LICOM can represent the mesoscale eddy characteristic of the MOC similar to the observation. 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variations</subject><subject>Temperature</subject><subject>Transport</subject><subject>variability</subject><subject>中尺度涡</subject><subject>佛罗里达州</subject><subject>大西洋</subject><subject>快速气候变化</subject><subject>模拟量</subject><subject>海洋运输</subject><subject>热量传递</subject><subject>经向环流</subject><issn>1674-2834</issn><issn>2376-6123</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkcFuEzEQhi0EElHpKyAjbkgbZmyvvXuMqkIrVXCgcLWm3nWz7cZOvI5K3opn4MnqVRpxZC6-fPP_ms-MvUdYIjTwGbVRopFqKQDFElEpA9i-Ygshja40CvmaLWaomqm37HyaHgAApdAG5IJd_hg2-5HyEAOPnv-K437Tcwodv-op89tEYdrGlDmNMdxzoZf13z_f-BB4Xvd8lUcKeXDv2BtP49Sfv7xn7OeXy9uLq-rm-9fri9VN5VQNuTIIpFwrgPq7zjunPXg0EpRxnVbUeNGhRyrTSUNtZ7BpXUNOybZutNbyjH065j5R8BTu7UPcp1Aabbdbrw-Pvx_vZg9QA9QF_niEtynu9v2U_9FCYC0UqhYKpY-US3GaUu_tNg0bSgeLYGfF9qTYztH2pLgsro6LQ_AxbegpprGzmQ5jTL5oc8Nk5X8zPryUr4vd3VAuOrUrKZtGlv97BtAJjCg</recordid><startdate>2012</startdate><enddate>2012</enddate><creator>MO 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meridional overtuming circula- tion （MOC） and meridional heat transport （MHT） estimated from the Rapid Climate Change/Meridional Circu- lation and Heat Flux Array （RAPID/MOCHA） at 26.5°N are used to evaluate the volume and heat transport in the eddy-resolving model LASG/IAP Climate system Ocean Model （LICOM）. The authors find that the Florida Cur- rent transport and upper mid-ocean transport of the model are underestimated against the observations. The simulated variability of MOC and MHT show a high correlation with the observations, exceeding 0.6. Both the simulated and observed MOC and MHT show a significant seasonal variability. According to the power spectrum analysis, LICOM can represent the mesoscale eddy characteristic of the MOC similar to the observation. The model shows a high correlation of 0.58 for the internal upper mid-ocean transport （MO） and a density difference between the western and eastern boundaries, as noted in previous studies.</abstract><cop>Beijing</cop><pub>Routledge</pub><doi>10.1080/16742834.2012.11447019</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
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| identifier | ISSN: 1674-2834 |
| ispartof | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2012, Vol.5 (5), p.373-378 |
| issn | 1674-2834 2376-6123 |
| language | eng |
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| source | Taylor & Francis Open Access |
| subjects | Climate change Climate system Correlation eddy-resolving Heat transfer Heat transport meridional heat transport meridional overturning circulation Ocean circulation Seasonal variation Seasonal variations Temperature Transport variability 中尺度涡 佛罗里达州 大西洋 快速气候变化 模拟量 海洋运输 热量传递 经向环流 |
| title | Simulation of Volume and Heat Transport along 26.5°N in the Atlantic |
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