Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections: From the East Asian Summer Monsoon Perspective
The East Asian summer monsoon (EASM) may exhibit rather large variability between years characterized by the same ENSO phase. Such inconsistency reduces the EASM predictability based on ENSO. Results in this study show that the Tibetan Plateau snow cover (TPSC) exerts a modulating effect on ENSO tel...
Gespeichert in:
| Veröffentlicht in: | Journal of climate 2012-04, Vol.25 (7), p.2481-2489 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 2489 |
|---|---|
| container_issue | 7 |
| container_start_page | 2481 |
| container_title | Journal of climate |
| container_volume | 25 |
| creator | Wu, Zhiwei Li, Jianping Jiang, Zhihong Ma, Tingting |
| description | The East Asian summer monsoon (EASM) may exhibit rather large variability between years characterized by the same ENSO phase. Such inconsistency reduces the EASM predictability based on ENSO. Results in this study show that the Tibetan Plateau snow cover (TPSC) exerts a modulating effect on ENSO teleconnections and ENSO significantly correlates with the EASM only during the reduced TPSC summers. Three-dimensional circulation structures are examined to manifest that the typical ENSO signals in reduced TPSC summers tend to be stronger than in excessive TPSC summers. Numerical and theoretical evidences indicate that the anomalously reduced TPSC can force positive geopotential height anomalies at the upper troposphere and weaken the jet streams across eastern Asia and northwestern Pacific. Governed by such basic state zonal flows, the extratropical Rossby wave response to the ENSO forcing usually has a larger amplitude and pronounced westward development. In such case, ENSO extends its influences to eastern Asia and enhances its connection with the EASM. |
| doi_str_mv | 10.1175/JCLI-D-11-00135.1 |
| format | Article |
| fullrecord | <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1642326714</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>26191331</jstor_id><sourcerecordid>26191331</sourcerecordid><originalsourceid>FETCH-LOGICAL-c509t-e06c64764a9602705a8eeda75da424b6dcfc0a3c383bd7bfbaa9ca6f1849d1f83</originalsourceid><addsrcrecordid>eNqF0V1rFDEUBuAgFdxWf4AXwmAp9GZqTj4nl7K7tpXVFbpehzOZDM4yndRkpsV_b6ZbFITiVULynHNIXkLeAr0A0PLD5-XmulyVACWlwOUFvCALkIyWVAh2RBa0MqKstJSvyHFK-4yYonRBrr6EZupx7MJQhLYYf_hi19V-xKH4lo89TsXNEB6KZbj3schoFuuvN9ti53vvwjB4Nxen1-Rli33yb57WE_L903q3vCo328vr5cdN6SQ1Y-mpckpoJdAoyjSVWHnfoJYNCiZq1bjWUeSOV7xudN3WiMahaqESpoG24ifk_ND3Loafk0-jve2S832Pgw9TsqAE40xpEP-nAgxXkL8r0_f_0H2Y4pAfYo1hRkkmeEanzyFW5XkVp2yeCgflYkgp-tbexe4W4y8L1M5Z2Tkru8p7-5iVhVxz9tQZk8O-jTi4Lv0pZFIrrY3K7t3B7dMY4t97BQY4B_4bPPGbQQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2814383024</pqid></control><display><type>article</type><title>Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections: From the East Asian Summer Monsoon Perspective</title><source>American Meteorological Society</source><source>Jstor Complete Legacy</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>Wu, Zhiwei ; Li, Jianping ; Jiang, Zhihong ; Ma, Tingting</creator><creatorcontrib>Wu, Zhiwei ; Li, Jianping ; Jiang, Zhihong ; Ma, Tingting</creatorcontrib><description>The East Asian summer monsoon (EASM) may exhibit rather large variability between years characterized by the same ENSO phase. Such inconsistency reduces the EASM predictability based on ENSO. Results in this study show that the Tibetan Plateau snow cover (TPSC) exerts a modulating effect on ENSO teleconnections and ENSO significantly correlates with the EASM only during the reduced TPSC summers. Three-dimensional circulation structures are examined to manifest that the typical ENSO signals in reduced TPSC summers tend to be stronger than in excessive TPSC summers. Numerical and theoretical evidences indicate that the anomalously reduced TPSC can force positive geopotential height anomalies at the upper troposphere and weaken the jet streams across eastern Asia and northwestern Pacific. Governed by such basic state zonal flows, the extratropical Rossby wave response to the ENSO forcing usually has a larger amplitude and pronounced westward development. In such case, ENSO extends its influences to eastern Asia and enhances its connection with the EASM.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/JCLI-D-11-00135.1</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Altitude ; Anomalies ; Asian ; Climate ; Climate change ; Drought ; Dynamic height ; Earth, ocean, space ; East Asian monsoon ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation event ; Exact sciences and technology ; External geophysics ; General circulation models ; Geopotential ; Geopotential height ; Greenhouse gases ; Height anomalies ; Jet stream ; Jet streams (meteorology) ; Joints ; Marine ; Meteorology ; Meteors ; Modulation ; Monsoons ; Planetary waves ; Precipitation ; Rain ; Rossby waves ; Seasons ; Snow ; Snow cover ; Southern Oscillation ; Summer ; Summer circulation ; Summer monsoon ; Teleconnections ; Three dimensional ; Time series ; Troposphere ; Upper troposphere ; Wind ; Zonal flow ; Zonal flow (meteorology)</subject><ispartof>Journal of climate, 2012-04, Vol.25 (7), p.2481-2489</ispartof><rights>2012 American Meteorological Society</rights><rights>2015 INIST-CNRS</rights><rights>Copyright American Meteorological Society 2012</rights><rights>Copyright American Meteorological Society Apr 1, 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c509t-e06c64764a9602705a8eeda75da424b6dcfc0a3c383bd7bfbaa9ca6f1849d1f83</citedby><cites>FETCH-LOGICAL-c509t-e06c64764a9602705a8eeda75da424b6dcfc0a3c383bd7bfbaa9ca6f1849d1f83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26191331$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26191331$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,3681,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25767796$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Wu, Zhiwei</creatorcontrib><creatorcontrib>Li, Jianping</creatorcontrib><creatorcontrib>Jiang, Zhihong</creatorcontrib><creatorcontrib>Ma, Tingting</creatorcontrib><title>Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections: From the East Asian Summer Monsoon Perspective</title><title>Journal of climate</title><description>The East Asian summer monsoon (EASM) may exhibit rather large variability between years characterized by the same ENSO phase. Such inconsistency reduces the EASM predictability based on ENSO. Results in this study show that the Tibetan Plateau snow cover (TPSC) exerts a modulating effect on ENSO teleconnections and ENSO significantly correlates with the EASM only during the reduced TPSC summers. Three-dimensional circulation structures are examined to manifest that the typical ENSO signals in reduced TPSC summers tend to be stronger than in excessive TPSC summers. Numerical and theoretical evidences indicate that the anomalously reduced TPSC can force positive geopotential height anomalies at the upper troposphere and weaken the jet streams across eastern Asia and northwestern Pacific. Governed by such basic state zonal flows, the extratropical Rossby wave response to the ENSO forcing usually has a larger amplitude and pronounced westward development. In such case, ENSO extends its influences to eastern Asia and enhances its connection with the EASM.</description><subject>Altitude</subject><subject>Anomalies</subject><subject>Asian</subject><subject>Climate</subject><subject>Climate change</subject><subject>Drought</subject><subject>Dynamic height</subject><subject>Earth, ocean, space</subject><subject>East Asian monsoon</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation event</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>General circulation models</subject><subject>Geopotential</subject><subject>Geopotential height</subject><subject>Greenhouse gases</subject><subject>Height anomalies</subject><subject>Jet stream</subject><subject>Jet streams (meteorology)</subject><subject>Joints</subject><subject>Marine</subject><subject>Meteorology</subject><subject>Meteors</subject><subject>Modulation</subject><subject>Monsoons</subject><subject>Planetary waves</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Rossby waves</subject><subject>Seasons</subject><subject>Snow</subject><subject>Snow cover</subject><subject>Southern Oscillation</subject><subject>Summer</subject><subject>Summer circulation</subject><subject>Summer monsoon</subject><subject>Teleconnections</subject><subject>Three dimensional</subject><subject>Time series</subject><subject>Troposphere</subject><subject>Upper troposphere</subject><subject>Wind</subject><subject>Zonal flow</subject><subject>Zonal flow (meteorology)</subject><issn>0894-8755</issn><issn>1520-0442</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqF0V1rFDEUBuAgFdxWf4AXwmAp9GZqTj4nl7K7tpXVFbpehzOZDM4yndRkpsV_b6ZbFITiVULynHNIXkLeAr0A0PLD5-XmulyVACWlwOUFvCALkIyWVAh2RBa0MqKstJSvyHFK-4yYonRBrr6EZupx7MJQhLYYf_hi19V-xKH4lo89TsXNEB6KZbj3schoFuuvN9ti53vvwjB4Nxen1-Rli33yb57WE_L903q3vCo328vr5cdN6SQ1Y-mpckpoJdAoyjSVWHnfoJYNCiZq1bjWUeSOV7xudN3WiMahaqESpoG24ifk_ND3Loafk0-jve2S832Pgw9TsqAE40xpEP-nAgxXkL8r0_f_0H2Y4pAfYo1hRkkmeEanzyFW5XkVp2yeCgflYkgp-tbexe4W4y8L1M5Z2Tkru8p7-5iVhVxz9tQZk8O-jTi4Lv0pZFIrrY3K7t3B7dMY4t97BQY4B_4bPPGbQQ</recordid><startdate>20120401</startdate><enddate>20120401</enddate><creator>Wu, Zhiwei</creator><creator>Li, Jianping</creator><creator>Jiang, Zhihong</creator><creator>Ma, Tingting</creator><general>American Meteorological Society</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M0K</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>S0X</scope><scope>7TN</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20120401</creationdate><title>Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections</title><author>Wu, Zhiwei ; Li, Jianping ; Jiang, Zhihong ; Ma, Tingting</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c509t-e06c64764a9602705a8eeda75da424b6dcfc0a3c383bd7bfbaa9ca6f1849d1f83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Altitude</topic><topic>Anomalies</topic><topic>Asian</topic><topic>Climate</topic><topic>Climate change</topic><topic>Drought</topic><topic>Dynamic height</topic><topic>Earth, ocean, space</topic><topic>East Asian monsoon</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>El Nino-Southern Oscillation event</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>General circulation models</topic><topic>Geopotential</topic><topic>Geopotential height</topic><topic>Greenhouse gases</topic><topic>Height anomalies</topic><topic>Jet stream</topic><topic>Jet streams (meteorology)</topic><topic>Joints</topic><topic>Marine</topic><topic>Meteorology</topic><topic>Meteors</topic><topic>Modulation</topic><topic>Monsoons</topic><topic>Planetary waves</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Rossby waves</topic><topic>Seasons</topic><topic>Snow</topic><topic>Snow cover</topic><topic>Southern Oscillation</topic><topic>Summer</topic><topic>Summer circulation</topic><topic>Summer monsoon</topic><topic>Teleconnections</topic><topic>Three dimensional</topic><topic>Time series</topic><topic>Troposphere</topic><topic>Upper troposphere</topic><topic>Wind</topic><topic>Zonal flow</topic><topic>Zonal flow (meteorology)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wu, Zhiwei</creatorcontrib><creatorcontrib>Li, Jianping</creatorcontrib><creatorcontrib>Jiang, Zhihong</creatorcontrib><creatorcontrib>Ma, Tingting</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Technology Collection</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>Research Library Prep</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>Agricultural Science Database</collection><collection>Military Database</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</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><collection>SIRS Editorial</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of climate</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wu, Zhiwei</au><au>Li, Jianping</au><au>Jiang, Zhihong</au><au>Ma, Tingting</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections: From the East Asian Summer Monsoon Perspective</atitle><jtitle>Journal of climate</jtitle><date>2012-04-01</date><risdate>2012</risdate><volume>25</volume><issue>7</issue><spage>2481</spage><epage>2489</epage><pages>2481-2489</pages><issn>0894-8755</issn><eissn>1520-0442</eissn><abstract>The East Asian summer monsoon (EASM) may exhibit rather large variability between years characterized by the same ENSO phase. Such inconsistency reduces the EASM predictability based on ENSO. Results in this study show that the Tibetan Plateau snow cover (TPSC) exerts a modulating effect on ENSO teleconnections and ENSO significantly correlates with the EASM only during the reduced TPSC summers. Three-dimensional circulation structures are examined to manifest that the typical ENSO signals in reduced TPSC summers tend to be stronger than in excessive TPSC summers. Numerical and theoretical evidences indicate that the anomalously reduced TPSC can force positive geopotential height anomalies at the upper troposphere and weaken the jet streams across eastern Asia and northwestern Pacific. Governed by such basic state zonal flows, the extratropical Rossby wave response to the ENSO forcing usually has a larger amplitude and pronounced westward development. In such case, ENSO extends its influences to eastern Asia and enhances its connection with the EASM.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/JCLI-D-11-00135.1</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0894-8755 |
| ispartof | Journal of climate, 2012-04, Vol.25 (7), p.2481-2489 |
| issn | 0894-8755 1520-0442 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1642326714 |
| source | American Meteorological Society; Jstor Complete Legacy; EZB-FREE-00999 freely available EZB journals |
| subjects | Altitude Anomalies Asian Climate Climate change Drought Dynamic height Earth, ocean, space East Asian monsoon El Nino El Nino phenomena El Nino-Southern Oscillation event Exact sciences and technology External geophysics General circulation models Geopotential Geopotential height Greenhouse gases Height anomalies Jet stream Jet streams (meteorology) Joints Marine Meteorology Meteors Modulation Monsoons Planetary waves Precipitation Rain Rossby waves Seasons Snow Snow cover Southern Oscillation Summer Summer circulation Summer monsoon Teleconnections Three dimensional Time series Troposphere Upper troposphere Wind Zonal flow Zonal flow (meteorology) |
| title | Modulation of the Tibetan Plateau Snow Cover on the ENSO Teleconnections: From the East Asian Summer Monsoon Perspective |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-27T17%3A04%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Modulation%20of%20the%20Tibetan%20Plateau%20Snow%20Cover%20on%20the%20ENSO%20Teleconnections:%20From%20the%20East%20Asian%20Summer%20Monsoon%20Perspective&rft.jtitle=Journal%20of%20climate&rft.au=Wu,%20Zhiwei&rft.date=2012-04-01&rft.volume=25&rft.issue=7&rft.spage=2481&rft.epage=2489&rft.pages=2481-2489&rft.issn=0894-8755&rft.eissn=1520-0442&rft_id=info:doi/10.1175/JCLI-D-11-00135.1&rft_dat=%3Cjstor_proqu%3E26191331%3C/jstor_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2814383024&rft_id=info:pmid/&rft_jstor_id=26191331&rfr_iscdi=true |