Reconstructing the quasi-biennial oscillation back to the early 1900s
The quasi‐biennial oscillation (QBO) is important for understanding the dynamical and chemical variability of the global stratosphere. Currently available wind data from the equatorial stratosphere extend back to 1953. Here we present reconstructions of the QBO extending back to 1900 that can be use...
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| Veröffentlicht in: | Geophysical research letters 2007-11, Vol.34 (22), p.n/a |
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| container_title | Geophysical research letters |
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| creator | Brönnimann, Stefan Annis, Jeffrey L. Vogler, Christian Jones, Phil D. |
| description | The quasi‐biennial oscillation (QBO) is important for understanding the dynamical and chemical variability of the global stratosphere. Currently available wind data from the equatorial stratosphere extend back to 1953. Here we present reconstructions of the QBO extending back to 1900 that can be used to constrain climate model simulations. The reconstructions are based on historical pilot balloon data as well as hourly sea‐level pressure (SLP) data from Jakarta, Indonesia. The latter were used to extract the signal of the solar semi‐diurnal tide in the middle atmosphere, which is modulated by the QBO. The reconstructions are in good agreement with the QBO signal extracted from historical total ozone data extending back to 1924. Further analyses suggest that the maximum phases of the QBO are captured relatively well after about 1910. |
| doi_str_mv | 10.1029/2007GL031354 |
| format | Article |
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Currently available wind data from the equatorial stratosphere extend back to 1953. Here we present reconstructions of the QBO extending back to 1900 that can be used to constrain climate model simulations. The reconstructions are based on historical pilot balloon data as well as hourly sea‐level pressure (SLP) data from Jakarta, Indonesia. The latter were used to extract the signal of the solar semi‐diurnal tide in the middle atmosphere, which is modulated by the QBO. The reconstructions are in good agreement with the QBO signal extracted from historical total ozone data extending back to 1924. Further analyses suggest that the maximum phases of the QBO are captured relatively well after about 1910.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2007GL031354</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; quasi-biennial oscillation ; stratosphere ; total ozone</subject><ispartof>Geophysical research letters, 2007-11, Vol.34 (22), p.n/a</ispartof><rights>Copyright 2007 by the American Geophysical Union.</rights><rights>2008 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5099-ced63a2710d4e45f715c80871344ad8489e9834c43a6bf403056b99eb41951813</citedby><cites>FETCH-LOGICAL-a5099-ced63a2710d4e45f715c80871344ad8489e9834c43a6bf403056b99eb41951813</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2007GL031354$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2007GL031354$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=19954751$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Brönnimann, Stefan</creatorcontrib><creatorcontrib>Annis, Jeffrey L.</creatorcontrib><creatorcontrib>Vogler, Christian</creatorcontrib><creatorcontrib>Jones, Phil D.</creatorcontrib><title>Reconstructing the quasi-biennial oscillation back to the early 1900s</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>The quasi‐biennial oscillation (QBO) is important for understanding the dynamical and chemical variability of the global stratosphere. Currently available wind data from the equatorial stratosphere extend back to 1953. Here we present reconstructions of the QBO extending back to 1900 that can be used to constrain climate model simulations. The reconstructions are based on historical pilot balloon data as well as hourly sea‐level pressure (SLP) data from Jakarta, Indonesia. The latter were used to extract the signal of the solar semi‐diurnal tide in the middle atmosphere, which is modulated by the QBO. The reconstructions are in good agreement with the QBO signal extracted from historical total ozone data extending back to 1924. Further analyses suggest that the maximum phases of the QBO are captured relatively well after about 1910.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>quasi-biennial oscillation</subject><subject>stratosphere</subject><subject>total ozone</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNp9kMFOwzAQRC0EEqVw4wNygROBdWzH8RFVNCACVAXE0XJcB0zTpLUTQf-elFTAidOuVm9mR4PQMYZzDJG4iAB4mgHBhNEdNMCC0jDpbrtoACC6PeLxPjrw_h0ASMcN0NXU6LryjWt1Y6vXoHkzwapV3oa5NVVlVRnUXtuyVI2tqyBXeh409TdmlCvXARYA_hDtFar05mg7h-h5fPU0ug6zh_RmdJmFioEQoTazmKiIY5hRQ1nBMdMJJBwTStUsoYkwIiFUU6LivKBdRBbnQpicYsFwgskQnfa-S1evWuMbubBemy5dZerWywgYA8qSDjzrQe1q750p5NLZhXJriUFuupJ_u-rwk62v8lqVhVOVtv5XIwSjnG3-Rz33YUuz_tdTptMsIhyLThT2Iusb8_kjUm4uY044ky_3qcwmtxN69ziVY_IFtC2ETg</recordid><startdate>200711</startdate><enddate>200711</enddate><creator>Brönnimann, Stefan</creator><creator>Annis, Jeffrey L.</creator><creator>Vogler, Christian</creator><creator>Jones, Phil D.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>200711</creationdate><title>Reconstructing the quasi-biennial oscillation back to the early 1900s</title><author>Brönnimann, Stefan ; Annis, Jeffrey L. ; Vogler, Christian ; Jones, Phil D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5099-ced63a2710d4e45f715c80871344ad8489e9834c43a6bf403056b99eb41951813</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>quasi-biennial oscillation</topic><topic>stratosphere</topic><topic>total ozone</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Brönnimann, Stefan</creatorcontrib><creatorcontrib>Annis, Jeffrey L.</creatorcontrib><creatorcontrib>Vogler, Christian</creatorcontrib><creatorcontrib>Jones, Phil D.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Brönnimann, Stefan</au><au>Annis, Jeffrey L.</au><au>Vogler, Christian</au><au>Jones, Phil D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reconstructing the quasi-biennial oscillation back to the early 1900s</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2007-11</date><risdate>2007</risdate><volume>34</volume><issue>22</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The quasi‐biennial oscillation (QBO) is important for understanding the dynamical and chemical variability of the global stratosphere. Currently available wind data from the equatorial stratosphere extend back to 1953. Here we present reconstructions of the QBO extending back to 1900 that can be used to constrain climate model simulations. The reconstructions are based on historical pilot balloon data as well as hourly sea‐level pressure (SLP) data from Jakarta, Indonesia. The latter were used to extract the signal of the solar semi‐diurnal tide in the middle atmosphere, which is modulated by the QBO. The reconstructions are in good agreement with the QBO signal extracted from historical total ozone data extending back to 1924. 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| subjects | Earth sciences Earth, ocean, space Exact sciences and technology quasi-biennial oscillation stratosphere total ozone |
| title | Reconstructing the quasi-biennial oscillation back to the early 1900s |
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