Diurnal tides from the troposphere to the lower mesosphere as deduced from TIMED/SABER satellite data and six global reanalysis data sets
We compare and examine diurnal temperature tides including their migrating component (DW1) from the troposphere to the lower mesosphere, using data from Thermosphere‐Ionosphere‐Mesosphere‐Energetics and Dynamics/Sounding of the Atmosphere using Broadband Emission Radiometry (TIMED/SABER) and from si...
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| Veröffentlicht in: | Journal of Geophysical Research: Atmospheres 2012-07, Vol.117 (D13), p.1G-n/a |
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| creator | Sakazaki, T. Fujiwara, M. Zhang, X. Hagan, M. E. Forbes, J. M. |
| description | We compare and examine diurnal temperature tides including their migrating component (DW1) from the troposphere to the lower mesosphere, using data from Thermosphere‐Ionosphere‐Mesosphere‐Energetics and Dynamics/Sounding of the Atmosphere using Broadband Emission Radiometry (TIMED/SABER) and from six different reanalysis data sets: (1) the Modern Era Retrospective analysis for Research and Applications (MERRA), (2) the European Centre for Medium‐range Weather Forecasts (ECMWF) reanalysis (ERA‐Interim) (3) the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR), (4) the Japanese 25‐year reanalysis by Japanese Meteorological Agency (JMA) and the Central Research Institute of Electric Power Industry (CRIEPI) (JRA25), (5) the NCEP/National Center for Atmospheric Research reanalysis (NCEP1), and (6) the NCEP and Department of Energy (DOE) Atmospheric Model Intercomparison Project (AMIP‐II) reanalysis data (NCEP2). The horizontal and vertical structures of the diurnal tides in SABER and reanalyses reasonably agree, although the amplitudes are up to 30–50% smaller in the reanalyses than in the SABER in the upper stratosphere to lower mesosphere. Of all tidal components, the DW1 is dominant while a clear eastward propagating zonal wave number 3 component (DE3) is observed at midlatitudes of the Southern Hemisphere in winter. Among the six reanalyses, MERRA, ERA‐Interim and CFSR are better at reproducing realistic diurnal tides. It is found that the diurnal tides extracted from SABER data in the winter‐hemisphere stratosphere suffer from sampling issues that are caused by short‐term variations of the background temperature. In addition, the GSWM underestimates the amplitude in the midlatitude upper stratosphere by about 50%.
Key Points
Diurnal tides in reanalyses are validated by SABER
Sampling issues about the tidal analysis with SABER data are shown and discussed
Diurnal tides are investigated from the troposphere to the lower mesosphere |
| doi_str_mv | 10.1029/2011JD017117 |
| format | Article |
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Key Points
Diurnal tides in reanalyses are validated by SABER
Sampling issues about the tidal analysis with SABER data are shown and discussed
Diurnal tides are investigated from the troposphere to the lower mesosphere</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2011JD017117</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Atmospheric research ; Climate system ; DE3 ; diurnal tides ; Earth sciences ; Earth, ocean, space ; Electric industries ; Electric power ; Exact sciences and technology ; Geophysics ; Ionosphere ; migrating tides ; reanalysis ; SABER ; sampling issue ; Stratosphere ; Tides ; Troposphere ; Weather forecasting</subject><ispartof>Journal of Geophysical Research: Atmospheres, 2012-07, Vol.117 (D13), p.1G-n/a</ispartof><rights>2012. American Geophysical Union. All Rights Reserved.</rights><rights>2015 INIST-CNRS</rights><rights>Copyright Blackwell Publishing Ltd. 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5231-33b23a19010c9e45ad94b8686deece3fd0d1cc631243497343cb82c5c82456a63</citedby><cites>FETCH-LOGICAL-c5231-33b23a19010c9e45ad94b8686deece3fd0d1cc631243497343cb82c5c82456a63</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%2F2011JD017117$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2011JD017117$$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=26363934$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Sakazaki, T.</creatorcontrib><creatorcontrib>Fujiwara, M.</creatorcontrib><creatorcontrib>Zhang, X.</creatorcontrib><creatorcontrib>Hagan, M. E.</creatorcontrib><creatorcontrib>Forbes, J. M.</creatorcontrib><title>Diurnal tides from the troposphere to the lower mesosphere as deduced from TIMED/SABER satellite data and six global reanalysis data sets</title><title>Journal of Geophysical Research: Atmospheres</title><addtitle>J. Geophys. Res</addtitle><description>We compare and examine diurnal temperature tides including their migrating component (DW1) from the troposphere to the lower mesosphere, using data from Thermosphere‐Ionosphere‐Mesosphere‐Energetics and Dynamics/Sounding of the Atmosphere using Broadband Emission Radiometry (TIMED/SABER) and from six different reanalysis data sets: (1) the Modern Era Retrospective analysis for Research and Applications (MERRA), (2) the European Centre for Medium‐range Weather Forecasts (ECMWF) reanalysis (ERA‐Interim) (3) the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR), (4) the Japanese 25‐year reanalysis by Japanese Meteorological Agency (JMA) and the Central Research Institute of Electric Power Industry (CRIEPI) (JRA25), (5) the NCEP/National Center for Atmospheric Research reanalysis (NCEP1), and (6) the NCEP and Department of Energy (DOE) Atmospheric Model Intercomparison Project (AMIP‐II) reanalysis data (NCEP2). The horizontal and vertical structures of the diurnal tides in SABER and reanalyses reasonably agree, although the amplitudes are up to 30–50% smaller in the reanalyses than in the SABER in the upper stratosphere to lower mesosphere. Of all tidal components, the DW1 is dominant while a clear eastward propagating zonal wave number 3 component (DE3) is observed at midlatitudes of the Southern Hemisphere in winter. Among the six reanalyses, MERRA, ERA‐Interim and CFSR are better at reproducing realistic diurnal tides. It is found that the diurnal tides extracted from SABER data in the winter‐hemisphere stratosphere suffer from sampling issues that are caused by short‐term variations of the background temperature. In addition, the GSWM underestimates the amplitude in the midlatitude upper stratosphere by about 50%.
Key Points
Diurnal tides in reanalyses are validated by SABER
Sampling issues about the tidal analysis with SABER data are shown and discussed
Diurnal tides are investigated from the troposphere to the lower mesosphere</description><subject>Atmospheric research</subject><subject>Climate system</subject><subject>DE3</subject><subject>diurnal tides</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Electric industries</subject><subject>Electric power</subject><subject>Exact sciences and technology</subject><subject>Geophysics</subject><subject>Ionosphere</subject><subject>migrating tides</subject><subject>reanalysis</subject><subject>SABER</subject><subject>sampling issue</subject><subject>Stratosphere</subject><subject>Tides</subject><subject>Troposphere</subject><subject>Weather forecasting</subject><issn>0148-0227</issn><issn>2169-897X</issn><issn>2156-2202</issn><issn>2169-8996</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>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kM9O3DAQxq2qlVhRbjyApaq3pnhsx0mOlGy3INpK_BGrXiyvPSmm2c3iyQr2EXhrAqGop_oy1sz3-0bzMbYP4jMIWR1IAXBSCygAijdsIiE3mZRCvmUTAbrMhJTFDtsjuhHD07nRAibsoY6btHIt72NA4k3qlry_Rt6nbt3R-hrT8O-eW213h4kvkf72HfGAYeMxjNzF8fdpfXB--GV6xsn12LaxRx5c77hbBU7xnv9uu8WwLKEbdm4p0jgm7Ok9e9e4lnDvpe6yy6_Ti6Nv2enP2fHR4Wnmc6kgU2ohlYNKgPAV6tyFSi9KU5qA6FE1QQTw3iiQWumqUFr5RSl97ks53OyM2mUfRt916m43SL296Z4jIAtG5qoqS60H1adR5VNHlLCx6xSXLm0tCPuUt_0370H-8cXUkXdtk9zKR3plpFFGVerJVo26u9ji9r-e9mR2VkNRChiobKQi9Xj_Srn0x5pCFbm9-jGzczmfV790ba_UI8rXnNI</recordid><startdate>20120716</startdate><enddate>20120716</enddate><creator>Sakazaki, T.</creator><creator>Fujiwara, M.</creator><creator>Zhang, X.</creator><creator>Hagan, M. E.</creator><creator>Forbes, J. M.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</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>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M7S</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>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20120716</creationdate><title>Diurnal tides from the troposphere to the lower mesosphere as deduced from TIMED/SABER satellite data and six global reanalysis data sets</title><author>Sakazaki, T. ; Fujiwara, M. ; Zhang, X. ; Hagan, M. 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M.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</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>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>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</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>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Engineering 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>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Journal of Geophysical Research: Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sakazaki, T.</au><au>Fujiwara, M.</au><au>Zhang, X.</au><au>Hagan, M. E.</au><au>Forbes, J. M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Diurnal tides from the troposphere to the lower mesosphere as deduced from TIMED/SABER satellite data and six global reanalysis data sets</atitle><jtitle>Journal of Geophysical Research: Atmospheres</jtitle><addtitle>J. Geophys. Res</addtitle><date>2012-07-16</date><risdate>2012</risdate><volume>117</volume><issue>D13</issue><spage>1G</spage><epage>n/a</epage><pages>1G-n/a</pages><issn>0148-0227</issn><issn>2169-897X</issn><eissn>2156-2202</eissn><eissn>2169-8996</eissn><abstract>We compare and examine diurnal temperature tides including their migrating component (DW1) from the troposphere to the lower mesosphere, using data from Thermosphere‐Ionosphere‐Mesosphere‐Energetics and Dynamics/Sounding of the Atmosphere using Broadband Emission Radiometry (TIMED/SABER) and from six different reanalysis data sets: (1) the Modern Era Retrospective analysis for Research and Applications (MERRA), (2) the European Centre for Medium‐range Weather Forecasts (ECMWF) reanalysis (ERA‐Interim) (3) the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR), (4) the Japanese 25‐year reanalysis by Japanese Meteorological Agency (JMA) and the Central Research Institute of Electric Power Industry (CRIEPI) (JRA25), (5) the NCEP/National Center for Atmospheric Research reanalysis (NCEP1), and (6) the NCEP and Department of Energy (DOE) Atmospheric Model Intercomparison Project (AMIP‐II) reanalysis data (NCEP2). The horizontal and vertical structures of the diurnal tides in SABER and reanalyses reasonably agree, although the amplitudes are up to 30–50% smaller in the reanalyses than in the SABER in the upper stratosphere to lower mesosphere. Of all tidal components, the DW1 is dominant while a clear eastward propagating zonal wave number 3 component (DE3) is observed at midlatitudes of the Southern Hemisphere in winter. Among the six reanalyses, MERRA, ERA‐Interim and CFSR are better at reproducing realistic diurnal tides. It is found that the diurnal tides extracted from SABER data in the winter‐hemisphere stratosphere suffer from sampling issues that are caused by short‐term variations of the background temperature. In addition, the GSWM underestimates the amplitude in the midlatitude upper stratosphere by about 50%.
Key Points
Diurnal tides in reanalyses are validated by SABER
Sampling issues about the tidal analysis with SABER data are shown and discussed
Diurnal tides are investigated from the troposphere to the lower mesosphere</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2011JD017117</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Atmospheric research Climate system DE3 diurnal tides Earth sciences Earth, ocean, space Electric industries Electric power Exact sciences and technology Geophysics Ionosphere migrating tides reanalysis SABER sampling issue Stratosphere Tides Troposphere Weather forecasting |
| title | Diurnal tides from the troposphere to the lower mesosphere as deduced from TIMED/SABER satellite data and six global reanalysis data sets |
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