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On the role of extratropical air‐sea interaction in the persistence of the Southern Annular Mode
Using the daily atmosphere and ocean reanalysis data, this study highlights the role of extratropical air‐sea interaction in the variability of the Southern Annular Mode (SAM). Our analysis shows that the SAM‐induced meridional dipolar sea surface temperature (SST) anomalies, through surface heat fl...
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Published in: | Geophysical research letters 2016-08, Vol.43 (16), p.8806-8814 |
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creator | Xiao, Bei Zhang, Yang Yang, Xiu‐Qun Nie, Yu |
description | Using the daily atmosphere and ocean reanalysis data, this study highlights the role of extratropical air‐sea interaction in the variability of the Southern Annular Mode (SAM). Our analysis shows that the SAM‐induced meridional dipolar sea surface temperature (SST) anomalies, through surface heat fluxes, can maintain persistent lower tropospheric temperature anomalies, which further results in anomalous eddy momentum forcing enhancing the persistence of the SAM. With the Finite Amplitude Wave Activity diagnosis, we illustrate that response of the eddy momentum forcing to SST anomalies can be attributed to changes in both baroclinic processes as baroclinic eddy generation and barotropic processes as wave breaking thus resultant diffusive eddy mixing, with the former confined at high latitudes and the latter strongest at midlatitudes. Spectral analysis further suggests that the above air‐sea interactions are important for bimonthly and longer time scale SAM variations. The dipolar SST pattern may be an indicator for predicting subseasonal and interseasonal variabilities of the SAM.
Key Points
Daily reanalysis data show evidence that air‐sea interactions enhance the persistence of SAM
Ocean feeds back to SAM via both barotropic mechanism at midlatitude and baroclinic mechanism at high latitude
Air‐sea interactions are suggested to be important for the bimonthly and longer time scale variabilities of the SAM |
doi_str_mv | 10.1002/2016GL070255 |
format | article |
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Key Points
Daily reanalysis data show evidence that air‐sea interactions enhance the persistence of SAM
Ocean feeds back to SAM via both barotropic mechanism at midlatitude and baroclinic mechanism at high latitude
Air‐sea interactions are suggested to be important for the bimonthly and longer time scale variabilities of the SAM</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/2016GL070255</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Annular ; Anomalies ; Eddies ; eddy‐mean flow interaction ; extratropical air‐sea interaction ; Geophysics ; Latitude ; Marine ; Meteorology ; Ocean-atmosphere interaction ; Oceans ; Sea surface temperature ; Southern Annular Mode ; Spectral analysis ; Time</subject><ispartof>Geophysical research letters, 2016-08, Vol.43 (16), p.8806-8814</ispartof><rights>2016. The Authors.</rights><rights>2016. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4766-a34e98c65891c4fd16b0ff9e5d7f0042f439ab75f3e84ee9bc6bf877fbd383b93</citedby><cites>FETCH-LOGICAL-c4766-a34e98c65891c4fd16b0ff9e5d7f0042f439ab75f3e84ee9bc6bf877fbd383b93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2016GL070255$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2016GL070255$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,11505,27915,27916,46459,46883</link.rule.ids></links><search><creatorcontrib>Xiao, Bei</creatorcontrib><creatorcontrib>Zhang, Yang</creatorcontrib><creatorcontrib>Yang, Xiu‐Qun</creatorcontrib><creatorcontrib>Nie, Yu</creatorcontrib><title>On the role of extratropical air‐sea interaction in the persistence of the Southern Annular Mode</title><title>Geophysical research letters</title><description>Using the daily atmosphere and ocean reanalysis data, this study highlights the role of extratropical air‐sea interaction in the variability of the Southern Annular Mode (SAM). Our analysis shows that the SAM‐induced meridional dipolar sea surface temperature (SST) anomalies, through surface heat fluxes, can maintain persistent lower tropospheric temperature anomalies, which further results in anomalous eddy momentum forcing enhancing the persistence of the SAM. With the Finite Amplitude Wave Activity diagnosis, we illustrate that response of the eddy momentum forcing to SST anomalies can be attributed to changes in both baroclinic processes as baroclinic eddy generation and barotropic processes as wave breaking thus resultant diffusive eddy mixing, with the former confined at high latitudes and the latter strongest at midlatitudes. Spectral analysis further suggests that the above air‐sea interactions are important for bimonthly and longer time scale SAM variations. The dipolar SST pattern may be an indicator for predicting subseasonal and interseasonal variabilities of the SAM.
Key Points
Daily reanalysis data show evidence that air‐sea interactions enhance the persistence of SAM
Ocean feeds back to SAM via both barotropic mechanism at midlatitude and baroclinic mechanism at high latitude
Air‐sea interactions are suggested to be important for the bimonthly and longer time scale variabilities of the SAM</description><subject>Annular</subject><subject>Anomalies</subject><subject>Eddies</subject><subject>eddy‐mean flow interaction</subject><subject>extratropical air‐sea interaction</subject><subject>Geophysics</subject><subject>Latitude</subject><subject>Marine</subject><subject>Meteorology</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceans</subject><subject>Sea surface temperature</subject><subject>Southern Annular Mode</subject><subject>Spectral analysis</subject><subject>Time</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNqN0c1KxDAQB_AgCq6rNx-g4MWD1Unz1RwX0VVYWfDjXNLsBCs1WZMW9eYj-Iw-iV3Xg3gQTzMMv__AMITsUzimAMVJAVROZ6CgEGKDjKjmPC8B1CYZAeihL5TcJjspPQAAA0ZHpJ77rLvHLIYWs-AyfOmi6WJYNta0mWnix9t7QpM1vsNobNcEP_RfkSXG1KQOvf1KrkY3oR9K9NnE-741MbsKC9wlW860Cfe-65jcnZ_dnl7ks_n08nQyyy1XUuaGcdSllaLU1HK3oLIG5zSKhXIAvHCcaVMr4RiWHFHXVtauVMrVC1ayWrMxOVzvXcbw1GPqqscmWWxb4zH0qaIlExK0EP-hhdKg9BAZk4Nf9CH00Q-HDIpqSqVgbFBHa2VjSCmiq5axeTTxtaJQrX5T_fzNwIs1f25afP3TVtPrmeClkuwTwM2QCA</recordid><startdate>20160828</startdate><enddate>20160828</enddate><creator>Xiao, Bei</creator><creator>Zhang, Yang</creator><creator>Yang, Xiu‐Qun</creator><creator>Nie, Yu</creator><general>John Wiley & Sons, Inc</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>20160828</creationdate><title>On the role of extratropical air‐sea interaction in the persistence of the Southern Annular Mode</title><author>Xiao, Bei ; Zhang, Yang ; Yang, Xiu‐Qun ; Nie, Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4766-a34e98c65891c4fd16b0ff9e5d7f0042f439ab75f3e84ee9bc6bf877fbd383b93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Annular</topic><topic>Anomalies</topic><topic>Eddies</topic><topic>eddy‐mean flow interaction</topic><topic>extratropical air‐sea interaction</topic><topic>Geophysics</topic><topic>Latitude</topic><topic>Marine</topic><topic>Meteorology</topic><topic>Ocean-atmosphere interaction</topic><topic>Oceans</topic><topic>Sea surface temperature</topic><topic>Southern Annular Mode</topic><topic>Spectral analysis</topic><topic>Time</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Xiao, Bei</creatorcontrib><creatorcontrib>Zhang, Yang</creatorcontrib><creatorcontrib>Yang, Xiu‐Qun</creatorcontrib><creatorcontrib>Nie, Yu</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>Wiley Online Library Free Content</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Xiao, Bei</au><au>Zhang, Yang</au><au>Yang, Xiu‐Qun</au><au>Nie, Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>On the role of extratropical air‐sea interaction in the persistence of the Southern Annular Mode</atitle><jtitle>Geophysical research letters</jtitle><date>2016-08-28</date><risdate>2016</risdate><volume>43</volume><issue>16</issue><spage>8806</spage><epage>8814</epage><pages>8806-8814</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>Using the daily atmosphere and ocean reanalysis data, this study highlights the role of extratropical air‐sea interaction in the variability of the Southern Annular Mode (SAM). Our analysis shows that the SAM‐induced meridional dipolar sea surface temperature (SST) anomalies, through surface heat fluxes, can maintain persistent lower tropospheric temperature anomalies, which further results in anomalous eddy momentum forcing enhancing the persistence of the SAM. With the Finite Amplitude Wave Activity diagnosis, we illustrate that response of the eddy momentum forcing to SST anomalies can be attributed to changes in both baroclinic processes as baroclinic eddy generation and barotropic processes as wave breaking thus resultant diffusive eddy mixing, with the former confined at high latitudes and the latter strongest at midlatitudes. Spectral analysis further suggests that the above air‐sea interactions are important for bimonthly and longer time scale SAM variations. The dipolar SST pattern may be an indicator for predicting subseasonal and interseasonal variabilities of the SAM.
Key Points
Daily reanalysis data show evidence that air‐sea interactions enhance the persistence of SAM
Ocean feeds back to SAM via both barotropic mechanism at midlatitude and baroclinic mechanism at high latitude
Air‐sea interactions are suggested to be important for the bimonthly and longer time scale variabilities of the SAM</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1002/2016GL070255</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Annular Anomalies Eddies eddy‐mean flow interaction extratropical air‐sea interaction Geophysics Latitude Marine Meteorology Ocean-atmosphere interaction Oceans Sea surface temperature Southern Annular Mode Spectral analysis Time |
title | On the role of extratropical air‐sea interaction in the persistence of the Southern Annular Mode |
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