The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation
Recent research has suggested that the tropical and extratropical character of the Madden‐Julian oscillation (MJO) depends on the state of the stratospheric quasi‐biennial oscillation (QBO). With this in mind, we use both reanalysis and a global climate model (CESM2‐WACCM) to analyze the global char...
Gespeichert in:
Veröffentlicht in: | Journal of geophysical research. Atmospheres 2020-04, Vol.125 (7), p.n/a |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | n/a |
---|---|
container_issue | 7 |
container_start_page | |
container_title | Journal of geophysical research. Atmospheres |
container_volume | 125 |
creator | Toms, Benjamin A. Barnes, Elizabeth A. Maloney, Eric D. Heever, Susan C. |
description | Recent research has suggested that the tropical and extratropical character of the Madden‐Julian oscillation (MJO) depends on the state of the stratospheric quasi‐biennial oscillation (QBO). With this in mind, we use both reanalysis and a global climate model (CESM2‐WACCM) to analyze the global character of upper tropospheric‐lower stratospheric geopotential height anomalies connected with the MJO and quantify dependencies of these teleconnections on the state of the QBO. We find that the global teleconnection signature of the MJO depends upon the state of the QBO. Globally, within reanalysis the fraction of 20‐ to 90‐day 250‐hPa geopotential height variance linked to the MJO is largest during boreal winter and summer for easterly QBO phases and smallest during westerly QBO phases of boreal winter. The difference between QBO phases is mostly driven by changes in the tropical signature of the MJO, although during boreal winter the Northern Hemispheric teleconnections are particularly more prominent during easterly QBO phases. Otherwise, the QBO modulation of extratropical MJO teleconnections is mainly realized through changes in the locations of the teleconnections. A QBO‐MJO relationship is also apparent within CESM2‐WACCM but is weaker than that observed. This extratropical modulation implies that the regions that benefit from increased subseasonal predictability due to the MJO may also change as a function of the QBO. In a broader sense, these findings emphasize that knowledge of the tropical stratospheric state, particularly as it relates to the QBO, is important for understanding the connections between the MJO and the extratropics.
Key Points
The QBO modulates the locations of MJO teleconnections, mainly through the locations in which they occur
The modulation is greatest during boreal winter but occurs to some extent during all seasons
A modulation also exists within CESM2‐WACCM but is weaker and has a different spatial pattern |
doi_str_mv | 10.1029/2020JD032653 |
format | Article |
fullrecord | <record><control><sourceid>proquest_osti_</sourceid><recordid>TN_cdi_osti_scitechconnect_1607801</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2388902545</sourcerecordid><originalsourceid>FETCH-LOGICAL-c4383-ac1dcecca39fd0a29361f714ed0f844cfbfa9246bca5fc2aeb6c6ca2ca56111e3</originalsourceid><addsrcrecordid>eNp9kctOAjEUhidGEwmy8wEa3Yr2NmVmqaAIgRAVE3dNp9NKydjidCaGhYmP4DP6JBaGGFaezbnk-88lJ4pOEbxEEKdXGGI4HkCCWUwOohZGLO0macoO_-Ley3HU8X4JgyWQ0Ji2os_5QoFh4TJRgLkqlHTWKlkZZ8GTebWiqksFnAZVwKYiz5X9-foe14URFsy8NEUhtrCwORhVHkxdXu9K2XqreqiFN0F0Y5S1JozZk51ER1oUXnV2vh09393O-_fdyWw46l9PupKShHSFRLlUUgqS6hwKnBKGdA9RlUOdUCp1pkWKKcukiLXEQmVMMilwSBlCSJF2dNb0db4yPMyvlFzsTuWIwV4CUYDOG2hVuvda-YovXV3asBfHJElSiGMaB-qioWTpvC-V5qvSvIlyzRHkm0fw_UcEnDT4hynU-l-Wj4ePg83ChPwCFQWNFw</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2388902545</pqid></control><display><type>article</type><title>The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation</title><source>Wiley Free Content</source><source>Wiley Online Library Journals Frontfile Complete</source><source>Alma/SFX Local Collection</source><creator>Toms, Benjamin A. ; Barnes, Elizabeth A. ; Maloney, Eric D. ; Heever, Susan C.</creator><creatorcontrib>Toms, Benjamin A. ; Barnes, Elizabeth A. ; Maloney, Eric D. ; Heever, Susan C.</creatorcontrib><description>Recent research has suggested that the tropical and extratropical character of the Madden‐Julian oscillation (MJO) depends on the state of the stratospheric quasi‐biennial oscillation (QBO). With this in mind, we use both reanalysis and a global climate model (CESM2‐WACCM) to analyze the global character of upper tropospheric‐lower stratospheric geopotential height anomalies connected with the MJO and quantify dependencies of these teleconnections on the state of the QBO. We find that the global teleconnection signature of the MJO depends upon the state of the QBO. Globally, within reanalysis the fraction of 20‐ to 90‐day 250‐hPa geopotential height variance linked to the MJO is largest during boreal winter and summer for easterly QBO phases and smallest during westerly QBO phases of boreal winter. The difference between QBO phases is mostly driven by changes in the tropical signature of the MJO, although during boreal winter the Northern Hemispheric teleconnections are particularly more prominent during easterly QBO phases. Otherwise, the QBO modulation of extratropical MJO teleconnections is mainly realized through changes in the locations of the teleconnections. A QBO‐MJO relationship is also apparent within CESM2‐WACCM but is weaker than that observed. This extratropical modulation implies that the regions that benefit from increased subseasonal predictability due to the MJO may also change as a function of the QBO. In a broader sense, these findings emphasize that knowledge of the tropical stratospheric state, particularly as it relates to the QBO, is important for understanding the connections between the MJO and the extratropics.
Key Points
The QBO modulates the locations of MJO teleconnections, mainly through the locations in which they occur
The modulation is greatest during boreal winter but occurs to some extent during all seasons
A modulation also exists within CESM2‐WACCM but is weaker and has a different spatial pattern</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2020JD032653</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Anomalies ; Climate models ; Cyclones ; Dynamic height ; Geophysics ; Geopotential ; Geopotential height ; Global climate ; Global climate models ; Height ; Height anomalies ; Madden-Julian oscillation ; Modulation ; Phases ; Quasi-biennial oscillation ; spectral analysis ; Teleconnections ; Tropical climate ; tropical‐extratropical coupling ; tropospheric‐stratospheric coupling ; Winter</subject><ispartof>Journal of geophysical research. Atmospheres, 2020-04, Vol.125 (7), p.n/a</ispartof><rights>2020. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4383-ac1dcecca39fd0a29361f714ed0f844cfbfa9246bca5fc2aeb6c6ca2ca56111e3</citedby><cites>FETCH-LOGICAL-c4383-ac1dcecca39fd0a29361f714ed0f844cfbfa9246bca5fc2aeb6c6ca2ca56111e3</cites><orcidid>0000-0002-2660-2611 ; 0000-0003-4284-9320 ; 0000-0001-9843-3864 ; 0000-0001-7982-5491 ; 0000000342849320 ; 0000000226602611 ; 0000000179825491 ; 0000000198433864</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2020JD032653$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2020JD032653$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,1427,27901,27902,45550,45551,46384,46808</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/1607801$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Toms, Benjamin A.</creatorcontrib><creatorcontrib>Barnes, Elizabeth A.</creatorcontrib><creatorcontrib>Maloney, Eric D.</creatorcontrib><creatorcontrib>Heever, Susan C.</creatorcontrib><title>The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation</title><title>Journal of geophysical research. Atmospheres</title><description>Recent research has suggested that the tropical and extratropical character of the Madden‐Julian oscillation (MJO) depends on the state of the stratospheric quasi‐biennial oscillation (QBO). With this in mind, we use both reanalysis and a global climate model (CESM2‐WACCM) to analyze the global character of upper tropospheric‐lower stratospheric geopotential height anomalies connected with the MJO and quantify dependencies of these teleconnections on the state of the QBO. We find that the global teleconnection signature of the MJO depends upon the state of the QBO. Globally, within reanalysis the fraction of 20‐ to 90‐day 250‐hPa geopotential height variance linked to the MJO is largest during boreal winter and summer for easterly QBO phases and smallest during westerly QBO phases of boreal winter. The difference between QBO phases is mostly driven by changes in the tropical signature of the MJO, although during boreal winter the Northern Hemispheric teleconnections are particularly more prominent during easterly QBO phases. Otherwise, the QBO modulation of extratropical MJO teleconnections is mainly realized through changes in the locations of the teleconnections. A QBO‐MJO relationship is also apparent within CESM2‐WACCM but is weaker than that observed. This extratropical modulation implies that the regions that benefit from increased subseasonal predictability due to the MJO may also change as a function of the QBO. In a broader sense, these findings emphasize that knowledge of the tropical stratospheric state, particularly as it relates to the QBO, is important for understanding the connections between the MJO and the extratropics.
Key Points
The QBO modulates the locations of MJO teleconnections, mainly through the locations in which they occur
The modulation is greatest during boreal winter but occurs to some extent during all seasons
A modulation also exists within CESM2‐WACCM but is weaker and has a different spatial pattern</description><subject>Anomalies</subject><subject>Climate models</subject><subject>Cyclones</subject><subject>Dynamic height</subject><subject>Geophysics</subject><subject>Geopotential</subject><subject>Geopotential height</subject><subject>Global climate</subject><subject>Global climate models</subject><subject>Height</subject><subject>Height anomalies</subject><subject>Madden-Julian oscillation</subject><subject>Modulation</subject><subject>Phases</subject><subject>Quasi-biennial oscillation</subject><subject>spectral analysis</subject><subject>Teleconnections</subject><subject>Tropical climate</subject><subject>tropical‐extratropical coupling</subject><subject>tropospheric‐stratospheric coupling</subject><subject>Winter</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kctOAjEUhidGEwmy8wEa3Yr2NmVmqaAIgRAVE3dNp9NKydjidCaGhYmP4DP6JBaGGFaezbnk-88lJ4pOEbxEEKdXGGI4HkCCWUwOohZGLO0macoO_-Ley3HU8X4JgyWQ0Ji2os_5QoFh4TJRgLkqlHTWKlkZZ8GTebWiqksFnAZVwKYiz5X9-foe14URFsy8NEUhtrCwORhVHkxdXu9K2XqreqiFN0F0Y5S1JozZk51ER1oUXnV2vh09393O-_fdyWw46l9PupKShHSFRLlUUgqS6hwKnBKGdA9RlUOdUCp1pkWKKcukiLXEQmVMMilwSBlCSJF2dNb0db4yPMyvlFzsTuWIwV4CUYDOG2hVuvda-YovXV3asBfHJElSiGMaB-qioWTpvC-V5qvSvIlyzRHkm0fw_UcEnDT4hynU-l-Wj4ePg83ChPwCFQWNFw</recordid><startdate>20200416</startdate><enddate>20200416</enddate><creator>Toms, Benjamin A.</creator><creator>Barnes, Elizabeth A.</creator><creator>Maloney, Eric D.</creator><creator>Heever, Susan C.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union (AGU)</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</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><scope>OTOTI</scope><orcidid>https://orcid.org/0000-0002-2660-2611</orcidid><orcidid>https://orcid.org/0000-0003-4284-9320</orcidid><orcidid>https://orcid.org/0000-0001-9843-3864</orcidid><orcidid>https://orcid.org/0000-0001-7982-5491</orcidid><orcidid>https://orcid.org/0000000342849320</orcidid><orcidid>https://orcid.org/0000000226602611</orcidid><orcidid>https://orcid.org/0000000179825491</orcidid><orcidid>https://orcid.org/0000000198433864</orcidid></search><sort><creationdate>20200416</creationdate><title>The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation</title><author>Toms, Benjamin A. ; Barnes, Elizabeth A. ; Maloney, Eric D. ; Heever, Susan C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4383-ac1dcecca39fd0a29361f714ed0f844cfbfa9246bca5fc2aeb6c6ca2ca56111e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Anomalies</topic><topic>Climate models</topic><topic>Cyclones</topic><topic>Dynamic height</topic><topic>Geophysics</topic><topic>Geopotential</topic><topic>Geopotential height</topic><topic>Global climate</topic><topic>Global climate models</topic><topic>Height</topic><topic>Height anomalies</topic><topic>Madden-Julian oscillation</topic><topic>Modulation</topic><topic>Phases</topic><topic>Quasi-biennial oscillation</topic><topic>spectral analysis</topic><topic>Teleconnections</topic><topic>Tropical climate</topic><topic>tropical‐extratropical coupling</topic><topic>tropospheric‐stratospheric coupling</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Toms, Benjamin A.</creatorcontrib><creatorcontrib>Barnes, Elizabeth A.</creatorcontrib><creatorcontrib>Maloney, Eric D.</creatorcontrib><creatorcontrib>Heever, Susan C.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</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><collection>OSTI.GOV</collection><jtitle>Journal of geophysical research. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Toms, Benjamin A.</au><au>Barnes, Elizabeth A.</au><au>Maloney, Eric D.</au><au>Heever, Susan C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation</atitle><jtitle>Journal of geophysical research. Atmospheres</jtitle><date>2020-04-16</date><risdate>2020</risdate><volume>125</volume><issue>7</issue><epage>n/a</epage><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>Recent research has suggested that the tropical and extratropical character of the Madden‐Julian oscillation (MJO) depends on the state of the stratospheric quasi‐biennial oscillation (QBO). With this in mind, we use both reanalysis and a global climate model (CESM2‐WACCM) to analyze the global character of upper tropospheric‐lower stratospheric geopotential height anomalies connected with the MJO and quantify dependencies of these teleconnections on the state of the QBO. We find that the global teleconnection signature of the MJO depends upon the state of the QBO. Globally, within reanalysis the fraction of 20‐ to 90‐day 250‐hPa geopotential height variance linked to the MJO is largest during boreal winter and summer for easterly QBO phases and smallest during westerly QBO phases of boreal winter. The difference between QBO phases is mostly driven by changes in the tropical signature of the MJO, although during boreal winter the Northern Hemispheric teleconnections are particularly more prominent during easterly QBO phases. Otherwise, the QBO modulation of extratropical MJO teleconnections is mainly realized through changes in the locations of the teleconnections. A QBO‐MJO relationship is also apparent within CESM2‐WACCM but is weaker than that observed. This extratropical modulation implies that the regions that benefit from increased subseasonal predictability due to the MJO may also change as a function of the QBO. In a broader sense, these findings emphasize that knowledge of the tropical stratospheric state, particularly as it relates to the QBO, is important for understanding the connections between the MJO and the extratropics.
Key Points
The QBO modulates the locations of MJO teleconnections, mainly through the locations in which they occur
The modulation is greatest during boreal winter but occurs to some extent during all seasons
A modulation also exists within CESM2‐WACCM but is weaker and has a different spatial pattern</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2020JD032653</doi><tpages>23</tpages><orcidid>https://orcid.org/0000-0002-2660-2611</orcidid><orcidid>https://orcid.org/0000-0003-4284-9320</orcidid><orcidid>https://orcid.org/0000-0001-9843-3864</orcidid><orcidid>https://orcid.org/0000-0001-7982-5491</orcidid><orcidid>https://orcid.org/0000000342849320</orcidid><orcidid>https://orcid.org/0000000226602611</orcidid><orcidid>https://orcid.org/0000000179825491</orcidid><orcidid>https://orcid.org/0000000198433864</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 2169-897X |
ispartof | Journal of geophysical research. Atmospheres, 2020-04, Vol.125 (7), p.n/a |
issn | 2169-897X 2169-8996 |
language | eng |
recordid | cdi_osti_scitechconnect_1607801 |
source | Wiley Free Content; Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection |
subjects | Anomalies Climate models Cyclones Dynamic height Geophysics Geopotential Geopotential height Global climate Global climate models Height Height anomalies Madden-Julian oscillation Modulation Phases Quasi-biennial oscillation spectral analysis Teleconnections Tropical climate tropical‐extratropical coupling tropospheric‐stratospheric coupling Winter |
title | The Global Teleconnection Signature of the Madden‐Julian Oscillation and Its Modulation by the Quasi‐Biennial Oscillation |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-09T17%3A57%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_osti_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20Global%20Teleconnection%20Signature%20of%20the%20Madden%E2%80%90Julian%20Oscillation%20and%20Its%20Modulation%20by%20the%20Quasi%E2%80%90Biennial%20Oscillation&rft.jtitle=Journal%20of%20geophysical%20research.%20Atmospheres&rft.au=Toms,%20Benjamin%20A.&rft.date=2020-04-16&rft.volume=125&rft.issue=7&rft.epage=n/a&rft.issn=2169-897X&rft.eissn=2169-8996&rft_id=info:doi/10.1029/2020JD032653&rft_dat=%3Cproquest_osti_%3E2388902545%3C/proquest_osti_%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2388902545&rft_id=info:pmid/&rfr_iscdi=true |