Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña
A recently identified climate mode called Ningaloo Niño (Niña) is associated with positive (negative) sea surface temperature (SST) anomalies off the west coast of Australia and negative (positive) sea level pressure (SLP) anomalies in the overlying atmosphere. By conducting a series of numerical ex...
Gespeichert in:
| Veröffentlicht in: | Climate dynamics 2014-10, Vol.43 (7-8), p.2197-2205 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 2205 |
|---|---|
| container_issue | 7-8 |
| container_start_page | 2197 |
| container_title | Climate dynamics |
| container_volume | 43 |
| creator | Tozuka, Tomoki Kataoka, Takahito Yamagata, Toshio |
| description | A recently identified climate mode called Ningaloo Niño (Niña) is associated with positive (negative) sea surface temperature (SST) anomalies off the west coast of Australia and negative (positive) sea level pressure (SLP) anomalies in the overlying atmosphere. By conducting a series of numerical experiments with an atmospheric general circulation model, generation mechanisms of the atmospheric circulation anomalies accompanied by Ningaloo Niño/Niña are examined. Even when SST is allowed to vary interannually only in the eastern South Indian Ocean, negative (positive) SLP anomalies are formed off the west coast of Australia in Ningaloo Niño (Niña) years, supporting the existence of local ocean–atmosphere interaction. When the model is forced by SST anomalies outside of the eastern South Indian Ocean, negative (positive) SLP anomalies are also generated in Ningaloo Niño (Niña) years owing to a Matsuno–Gill type response to atmospheric convection anomalies in the tropical Pacific. It is found that the latter impact is stronger in the current atmospheric general circulation model. Regarding climatic impacts, it is shown that Ningaloo Niño (Niña) induces wet (dry) anomalies over the northwestern part of Australia even when SST anomalies outside of the eastern South Indian Ocean are excluded from the SST forcing. |
| doi_str_mv | 10.1007/s00382-013-2044-x |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1611634049</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A386211821</galeid><sourcerecordid>A386211821</sourcerecordid><originalsourceid>FETCH-LOGICAL-c488x-fb39b652d660563e150f570a38ed28a3cc5717b0bf3d4c65f0e2c2be48b484513</originalsourceid><addsrcrecordid>eNp9kdtu1DAQhiMEEkvhAbgiEqKCi7TjY5zLquJQaQUSZa8txxnvukrixU6k7WPxDLwYXqVCXS6w5dP4m9HM_EXxmsAFAagvEwBTtALCKgqcV4cnxYpwli2q4U-LFTQMqlrU4nnxIqU7AMJlTVfFZh2s6fv70oxdGXEIE-aHC9FiV5ppCGm_w-htaX20c28mH8bMhsH0HlMZXPnVj1vTh5Avv3-Fy-NuXhbPnOkTvno4z4rNp48_rr9U62-fb66v1pXlSh0q17KmlYJ2UoKQDIkAJ2owTGFHlWHWiprULbSOddxK4QCppS1y1XLFBWFnxfsl7j6GnzOmSQ8-Wex7M2KYkyaSEMk48Cajb_9B78Icx5ydJkJKAqxRkKmLhcolofajC1M0Ns8OB2_DiM5n-xVTkhKi6DGDDycOmZnwMG3NnJK-uf1-yp4_Yndo-mmXQj8fe5pOQbKANoaUIjq9j34w8V4T0Ee59SK3znLro9z6kH3ePdRnUlbURTNan_46UqWavOrM0YVL-WvcYnzUh_8Ef7M4ORO02cYceHNLIeuVhxKSsj8BCcH6</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1566103980</pqid></control><display><type>article</type><title>Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña</title><source>SpringerLink Journals - AutoHoldings</source><creator>Tozuka, Tomoki ; Kataoka, Takahito ; Yamagata, Toshio</creator><creatorcontrib>Tozuka, Tomoki ; Kataoka, Takahito ; Yamagata, Toshio</creatorcontrib><description>A recently identified climate mode called Ningaloo Niño (Niña) is associated with positive (negative) sea surface temperature (SST) anomalies off the west coast of Australia and negative (positive) sea level pressure (SLP) anomalies in the overlying atmosphere. By conducting a series of numerical experiments with an atmospheric general circulation model, generation mechanisms of the atmospheric circulation anomalies accompanied by Ningaloo Niño/Niña are examined. Even when SST is allowed to vary interannually only in the eastern South Indian Ocean, negative (positive) SLP anomalies are formed off the west coast of Australia in Ningaloo Niño (Niña) years, supporting the existence of local ocean–atmosphere interaction. When the model is forced by SST anomalies outside of the eastern South Indian Ocean, negative (positive) SLP anomalies are also generated in Ningaloo Niño (Niña) years owing to a Matsuno–Gill type response to atmospheric convection anomalies in the tropical Pacific. It is found that the latter impact is stronger in the current atmospheric general circulation model. Regarding climatic impacts, it is shown that Ningaloo Niño (Niña) induces wet (dry) anomalies over the northwestern part of Australia even when SST anomalies outside of the eastern South Indian Ocean are excluded from the SST forcing.</description><identifier>ISSN: 0930-7575</identifier><identifier>EISSN: 1432-0894</identifier><identifier>DOI: 10.1007/s00382-013-2044-x</identifier><identifier>CODEN: CLDYEM</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Atmosphere ; Atmospheric circulation ; Atmospheric convection ; climate ; Climate science ; Climatology ; Climatology. Bioclimatology. Climate change ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; General Circulation Models ; Geophysics/Geodesy ; Meteorological research ; Meteorology ; Ocean-atmosphere interaction ; Oceanography ; Sea level ; Sea surface temperature ; surface water temperature</subject><ispartof>Climate dynamics, 2014-10, Vol.43 (7-8), p.2197-2205</ispartof><rights>Springer-Verlag Berlin Heidelberg 2014</rights><rights>2015 INIST-CNRS</rights><rights>COPYRIGHT 2014 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c488x-fb39b652d660563e150f570a38ed28a3cc5717b0bf3d4c65f0e2c2be48b484513</citedby><cites>FETCH-LOGICAL-c488x-fb39b652d660563e150f570a38ed28a3cc5717b0bf3d4c65f0e2c2be48b484513</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00382-013-2044-x$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00382-013-2044-x$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28892887$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Tozuka, Tomoki</creatorcontrib><creatorcontrib>Kataoka, Takahito</creatorcontrib><creatorcontrib>Yamagata, Toshio</creatorcontrib><title>Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña</title><title>Climate dynamics</title><addtitle>Clim Dyn</addtitle><description>A recently identified climate mode called Ningaloo Niño (Niña) is associated with positive (negative) sea surface temperature (SST) anomalies off the west coast of Australia and negative (positive) sea level pressure (SLP) anomalies in the overlying atmosphere. By conducting a series of numerical experiments with an atmospheric general circulation model, generation mechanisms of the atmospheric circulation anomalies accompanied by Ningaloo Niño/Niña are examined. Even when SST is allowed to vary interannually only in the eastern South Indian Ocean, negative (positive) SLP anomalies are formed off the west coast of Australia in Ningaloo Niño (Niña) years, supporting the existence of local ocean–atmosphere interaction. When the model is forced by SST anomalies outside of the eastern South Indian Ocean, negative (positive) SLP anomalies are also generated in Ningaloo Niño (Niña) years owing to a Matsuno–Gill type response to atmospheric convection anomalies in the tropical Pacific. It is found that the latter impact is stronger in the current atmospheric general circulation model. Regarding climatic impacts, it is shown that Ningaloo Niño (Niña) induces wet (dry) anomalies over the northwestern part of Australia even when SST anomalies outside of the eastern South Indian Ocean are excluded from the SST forcing.</description><subject>Atmosphere</subject><subject>Atmospheric circulation</subject><subject>Atmospheric convection</subject><subject>climate</subject><subject>Climate science</subject><subject>Climatology</subject><subject>Climatology. Bioclimatology. Climate change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>General Circulation Models</subject><subject>Geophysics/Geodesy</subject><subject>Meteorological research</subject><subject>Meteorology</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceanography</subject><subject>Sea level</subject><subject>Sea surface temperature</subject><subject>surface water temperature</subject><issn>0930-7575</issn><issn>1432-0894</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kdtu1DAQhiMEEkvhAbgiEqKCi7TjY5zLquJQaQUSZa8txxnvukrixU6k7WPxDLwYXqVCXS6w5dP4m9HM_EXxmsAFAagvEwBTtALCKgqcV4cnxYpwli2q4U-LFTQMqlrU4nnxIqU7AMJlTVfFZh2s6fv70oxdGXEIE-aHC9FiV5ppCGm_w-htaX20c28mH8bMhsH0HlMZXPnVj1vTh5Avv3-Fy-NuXhbPnOkTvno4z4rNp48_rr9U62-fb66v1pXlSh0q17KmlYJ2UoKQDIkAJ2owTGFHlWHWiprULbSOddxK4QCppS1y1XLFBWFnxfsl7j6GnzOmSQ8-Wex7M2KYkyaSEMk48Cajb_9B78Icx5ydJkJKAqxRkKmLhcolofajC1M0Ns8OB2_DiM5n-xVTkhKi6DGDDycOmZnwMG3NnJK-uf1-yp4_Yndo-mmXQj8fe5pOQbKANoaUIjq9j34w8V4T0Ee59SK3znLro9z6kH3ePdRnUlbURTNan_46UqWavOrM0YVL-WvcYnzUh_8Ef7M4ORO02cYceHNLIeuVhxKSsj8BCcH6</recordid><startdate>20141001</startdate><enddate>20141001</enddate><creator>Tozuka, Tomoki</creator><creator>Kataoka, Takahito</creator><creator>Yamagata, Toshio</creator><general>Springer-Verlag</general><general>Springer Berlin Heidelberg</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M1Q</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20141001</creationdate><title>Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña</title><author>Tozuka, Tomoki ; Kataoka, Takahito ; Yamagata, Toshio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c488x-fb39b652d660563e150f570a38ed28a3cc5717b0bf3d4c65f0e2c2be48b484513</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Atmosphere</topic><topic>Atmospheric circulation</topic><topic>Atmospheric convection</topic><topic>climate</topic><topic>Climate science</topic><topic>Climatology</topic><topic>Climatology. Bioclimatology. Climate change</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>General Circulation Models</topic><topic>Geophysics/Geodesy</topic><topic>Meteorological research</topic><topic>Meteorology</topic><topic>Ocean-atmosphere interaction</topic><topic>Oceanography</topic><topic>Sea level</topic><topic>Sea surface temperature</topic><topic>surface water temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tozuka, Tomoki</creatorcontrib><creatorcontrib>Kataoka, Takahito</creatorcontrib><creatorcontrib>Yamagata, Toshio</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Military Database</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Climate dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tozuka, Tomoki</au><au>Kataoka, Takahito</au><au>Yamagata, Toshio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña</atitle><jtitle>Climate dynamics</jtitle><stitle>Clim Dyn</stitle><date>2014-10-01</date><risdate>2014</risdate><volume>43</volume><issue>7-8</issue><spage>2197</spage><epage>2205</epage><pages>2197-2205</pages><issn>0930-7575</issn><eissn>1432-0894</eissn><coden>CLDYEM</coden><abstract>A recently identified climate mode called Ningaloo Niño (Niña) is associated with positive (negative) sea surface temperature (SST) anomalies off the west coast of Australia and negative (positive) sea level pressure (SLP) anomalies in the overlying atmosphere. By conducting a series of numerical experiments with an atmospheric general circulation model, generation mechanisms of the atmospheric circulation anomalies accompanied by Ningaloo Niño/Niña are examined. Even when SST is allowed to vary interannually only in the eastern South Indian Ocean, negative (positive) SLP anomalies are formed off the west coast of Australia in Ningaloo Niño (Niña) years, supporting the existence of local ocean–atmosphere interaction. When the model is forced by SST anomalies outside of the eastern South Indian Ocean, negative (positive) SLP anomalies are also generated in Ningaloo Niño (Niña) years owing to a Matsuno–Gill type response to atmospheric convection anomalies in the tropical Pacific. It is found that the latter impact is stronger in the current atmospheric general circulation model. Regarding climatic impacts, it is shown that Ningaloo Niño (Niña) induces wet (dry) anomalies over the northwestern part of Australia even when SST anomalies outside of the eastern South Indian Ocean are excluded from the SST forcing.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s00382-013-2044-x</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0930-7575 |
| ispartof | Climate dynamics, 2014-10, Vol.43 (7-8), p.2197-2205 |
| issn | 0930-7575 1432-0894 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1611634049 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Atmosphere Atmospheric circulation Atmospheric convection climate Climate science Climatology Climatology. Bioclimatology. Climate change Earth and Environmental Science Earth Sciences Earth, ocean, space Exact sciences and technology External geophysics General Circulation Models Geophysics/Geodesy Meteorological research Meteorology Ocean-atmosphere interaction Oceanography Sea level Sea surface temperature surface water temperature |
| title | Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T17%3A51%3A17IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Locally%20and%20remotely%20forced%20atmospheric%20circulation%20anomalies%20of%20Ningaloo%20Ni%C3%B1o/Ni%C3%B1a&rft.jtitle=Climate%20dynamics&rft.au=Tozuka,%20Tomoki&rft.date=2014-10-01&rft.volume=43&rft.issue=7-8&rft.spage=2197&rft.epage=2205&rft.pages=2197-2205&rft.issn=0930-7575&rft.eissn=1432-0894&rft.coden=CLDYEM&rft_id=info:doi/10.1007/s00382-013-2044-x&rft_dat=%3Cgale_proqu%3EA386211821%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1566103980&rft_id=info:pmid/&rft_galeid=A386211821&rfr_iscdi=true |