Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM
Observations of the mesosphere and lower thermosphere winds obtained by the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) during 1991 to 1995 reveal a semiannual variation in the amplitude of the (1, 1) diurnal tide. The global‐scale wave model (GSWM) repres...
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Veröffentlicht in: | Geophysical research letters 1995-10, Vol.22 (19), p.2641-2644 |
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description | Observations of the mesosphere and lower thermosphere winds obtained by the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) during 1991 to 1995 reveal a semiannual variation in the amplitude of the (1, 1) diurnal tide. The global‐scale wave model (GSWM) represents the first numerical modeling attempt at simulating this seasonal variability, and a preliminary comparison of the GSWM tidal results with HRDI measurements is presented. The results of the comparison and of numerical tests point to some vital and unresolved questions regarding tidal dissipation and tropospheric forcing. In addition to the seasonal variability, HRDI has revealed a strong interannual modulation of the diurnal tide with amplitudes observed to change by nearly a factor of 2 from 1992 to 1994. |
doi_str_mv | 10.1029/95GL02635 |
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The results of the comparison and of numerical tests point to some vital and unresolved questions regarding tidal dissipation and tropospheric forcing. In addition to the seasonal variability, HRDI has revealed a strong interannual modulation of the diurnal tide with amplitudes observed to change by nearly a factor of 2 from 1992 to 1994.</description><subject>Amplitudes</subject><subject>Doppler</subject><subject>Doppler effect</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Marine</subject><subject>Mathematical models</subject><subject>Mesosphere</subject><subject>Modulation</subject><subject>Physics of the high neutral atmosphere</subject><subject>Seasonal variations</subject><subject>Tides</subject><subject>Tides, waves, convection, winds, turbulence</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><recordid>eNqFkU1v1DAQhi0EEkvhwD_wASE4pPgj448jKjStlAJtQZW4WI7tgMGbFDvbsv-ejVLtDe1pRqPnfTUzL0IvKTmmhOl3GpqWMMHhEVpRXdeVIkQ-RitC9K5nUjxFz0r5RQjhhNMV-t6Ow49qCnmN72yOtospTlscBzz9DLiMyWbs4yYPNuEp-oDHroR8Fzzutvjs6sM5toPHJa43yU7LdBY21zcXz9GT3qYSXjzUI_Tt9OPXk7Oq_dycn7xvKweCqYozy6mVxHoLQnEH0jvnXfAAlHsOqtPQ0V4oIlktOqc0SBd6vjtGKUolP0KvF9_bPP7ZhDKZdSwupGSHMG6KoYoKDUodBoXWgnLYgW8OgDVjmtZaH0aB1TUFBfOebxfU5bGUHHpzm-Pa5q2hxMzhmX14O_bVg60tzqY-28HFshdwoSjw2fJ4we5jCtv_-5nmqlUC5hdUiyCWKfzdC2z-bYTkEszNp8YQcXF5_UVLc8n_ASB8srU</recordid><startdate>19951001</startdate><enddate>19951001</enddate><creator>Burrage, M. 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B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5628-32a31a70ada5683c57dccdced5513d358b95b1f6807246bc8957cef3827881173</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1995</creationdate><topic>Amplitudes</topic><topic>Doppler</topic><topic>Doppler effect</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Marine</topic><topic>Mathematical models</topic><topic>Mesosphere</topic><topic>Modulation</topic><topic>Physics of the high neutral atmosphere</topic><topic>Seasonal variations</topic><topic>Tides</topic><topic>Tides, waves, convection, winds, turbulence</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Burrage, M. D.</creatorcontrib><creatorcontrib>Hagan, M. E.</creatorcontrib><creatorcontrib>Skinner, W. R.</creatorcontrib><creatorcontrib>Wu, D. 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B.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic 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><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Burrage, M. D.</au><au>Hagan, M. E.</au><au>Skinner, W. R.</au><au>Wu, D. L.</au><au>Hays, P. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1995-10-01</date><risdate>1995</risdate><volume>22</volume><issue>19</issue><spage>2641</spage><epage>2644</epage><pages>2641-2644</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Observations of the mesosphere and lower thermosphere winds obtained by the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) during 1991 to 1995 reveal a semiannual variation in the amplitude of the (1, 1) diurnal tide. The global‐scale wave model (GSWM) represents the first numerical modeling attempt at simulating this seasonal variability, and a preliminary comparison of the GSWM tidal results with HRDI measurements is presented. The results of the comparison and of numerical tests point to some vital and unresolved questions regarding tidal dissipation and tropospheric forcing. In addition to the seasonal variability, HRDI has revealed a strong interannual modulation of the diurnal tide with amplitudes observed to change by nearly a factor of 2 from 1992 to 1994.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/95GL02635</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Amplitudes Doppler Doppler effect Earth, ocean, space Exact sciences and technology External geophysics Marine Mathematical models Mesosphere Modulation Physics of the high neutral atmosphere Seasonal variations Tides Tides, waves, convection, winds, turbulence |
title | Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM |
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