Mean winds of the upper middle atmosphere (∼70–110 km) from the global radar network: Comparisons with CIRA 72, and new rocket and satellite data
Identifieur interne : 001A65 ( Istex/Curation ); précédent : 001A64; suivant : 001A66Mean winds of the upper middle atmosphere (∼70–110 km) from the global radar network: Comparisons with CIRA 72, and new rocket and satellite data
Auteurs : A. H. Manson [Canada] ; C. E. Meek [Canada] ; M. Massebeuf [France] ; J. L. Fellous [France] ; W. G. Elford [France] ; R. A. Vincent [Australie] ; R. L. Craig [Australie] ; R. G. Roper [États-Unis] ; S. Avery [États-Unis] ; B. B. Balsley [États-Unis] ; G. J. Fraser [Nouvelle-Zélande] ; M. J. Smith [Nouvelle-Zélande] ; R. R. Clark [États-Unis] ; S. Kato [Japon] ; T. Tsuda [Japon]Source :
- Advances in Space Research [ 0273-1177 ] ; 1987.
English descriptors
- KwdEn :
- Adelaide, Atmos, December, Early winter, Easterly, Easterly flow, Equatorward, Equatorward flow, Geostrophic, Geostrophic wind, Geostrophic winds, Global radar network, Hanson, July, Last decade, Longitudinal differences, Longitudinal variations, Manson, Meridional, Meridional flow, Meridional wind comparisons, Meridional winds, Meteor radars, Middle atmosphere program, Negative winds, Physica scripta, Planetary waves, Poleward flow, Positive winds, Primrose lake, Radar stations, Radar winds, Saskatoon, Satellite data, Satellite wind comparisons, Scostep secretariat, Scott base, Secular trends, Significant differences, Stratospheric warmings, Strophic winds, Summer flow, Time resolution, Upper middle atmosphere, Westerly flow, Wind data, Wind shears, Zonal, Zonal winds.
- Teeft :
- Adelaide, Atmos, December, Early winter, Easterly, Easterly flow, Equatorward, Equatorward flow, Geostrophic, Geostrophic wind, Geostrophic winds, Global radar network, Hanson, July, Last decade, Longitudinal differences, Longitudinal variations, Manson, Meridional, Meridional flow, Meridional wind comparisons, Meridional winds, Meteor radars, Middle atmosphere program, Negative winds, Physica scripta, Planetary waves, Poleward flow, Positive winds, Primrose lake, Radar stations, Radar winds, Saskatoon, Satellite data, Satellite wind comparisons, Scostep secretariat, Scott base, Secular trends, Significant differences, Stratospheric warmings, Strophic winds, Summer flow, Time resolution, Upper middle atmosphere, Westerly flow, Wind data, Wind shears, Zonal, Zonal winds.
Abstract
Abstract: A substantial quantity of wind data have been assembled from radar systems since CIRA-72 was formed: most of these radars include height ranging, and operate on a regular and even continuous basis. Systems include meteor and MF (medium frequency) Radars: an MST (mesosphere-stratosphere-troposphere) Radar (meteor mode); and an LF (low frequency) drift system. Latitudes represented are near 20° N/S, 35° N/S, 45° N/S, 50°N, 65° N/S. In all cases tidal oscillations were calculated so that corrected mean winds (zonal, meridional) are available - the meridional was not included in CIRA-72. Means for groups of years near 1980 are available, as well as individual recent years (1983, 1984) to allow assessment of secular trends: revised and improved analysis has been completed for several stations.Height-time cross-sections have been formed for each observatory: heights are typically ∼75–110 km, with time resolution of 7–30 days. Such detailed cross-sections were almost unknown before 1972. Comparisons with CIRA-72 are shown, and these emphasize the differences between hemispheres (NH, SH) in the radar winds. Other new winds from rockets and satellite radiances are contrasted with the radar set. There are important differences with the satellite-derived geostrophic winds (1973–78): possible explanations involve secular trends, longitudinal variations, and ageostrophy.
Url:
DOI: 10.1016/0273-1177(87)90086-X
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H." last="Manson">A. H. Manson</name><affiliation wicri:level="1"><mods:affiliation>I.S.A.S., University of Saskatchewan, Canada</mods:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>I.S.A.S., University of Saskatchewan</wicri:regionArea></affiliation></author><author><name sortKey="Meek, C E" sort="Meek, C E" uniqKey="Meek C" first="C. E." last="Meek">C. E. Meek</name><affiliation wicri:level="1"><mods:affiliation>I.S.A.S., University of Saskatchewan, Canada</mods:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>I.S.A.S., University of Saskatchewan</wicri:regionArea></affiliation></author><author><name sortKey="Massebeuf, M" sort="Massebeuf, M" uniqKey="Massebeuf M" first="M." last="Massebeuf">M. 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A. Vincent</name><affiliation wicri:level="1"><mods:affiliation>University of Adelaide, Australia</mods:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>University of Adelaide</wicri:regionArea></affiliation></author><author><name sortKey="Craig, R L" sort="Craig, R L" uniqKey="Craig R" first="R. L." last="Craig">R. L. Craig</name><affiliation wicri:level="1"><mods:affiliation>University of Adelaide, Australia</mods:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>University of Adelaide</wicri:regionArea></affiliation></author><author><name sortKey="Roper, R G" sort="Roper, R G" uniqKey="Roper R" first="R. G." last="Roper">R. G. Roper</name><affiliation wicri:level="1"><mods:affiliation>Georgia Institute of Technology, U.S.A.</mods:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>Georgia Institute of Technology</wicri:regionArea></affiliation></author><author><name sortKey="Avery, S" sort="Avery, S" uniqKey="Avery S" first="S." last="Avery">S. Avery</name><affiliation wicri:level="1"><mods:affiliation>CIRES and NOAA, Boulder, U.S.A.</mods:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>CIRES and NOAA, Boulder</wicri:regionArea></affiliation></author><author><name sortKey="Balsley, B B" sort="Balsley, B B" uniqKey="Balsley B" first="B. B." last="Balsley">B. B. Balsley</name><affiliation wicri:level="1"><mods:affiliation>CIRES and NOAA, Boulder, U.S.A.</mods:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>CIRES and NOAA, Boulder</wicri:regionArea></affiliation></author><author><name sortKey="Fraser, G J" sort="Fraser, G J" uniqKey="Fraser G" first="G. J." last="Fraser">G. J. Fraser</name><affiliation wicri:level="1"><mods:affiliation>University of Canterbury, New Zealand</mods:affiliation><country xml:lang="fr">Nouvelle-Zélande</country><wicri:regionArea>University of Canterbury</wicri:regionArea></affiliation></author><author><name sortKey="Smith, M J" sort="Smith, M J" uniqKey="Smith M" first="M. J." last="Smith">M. J. Smith</name><affiliation wicri:level="1"><mods:affiliation>University of Canterbury, New Zealand</mods:affiliation><country xml:lang="fr">Nouvelle-Zélande</country><wicri:regionArea>University of Canterbury</wicri:regionArea></affiliation></author><author><name sortKey="Clark, R R" sort="Clark, R R" uniqKey="Clark R" first="R. R." last="Clark">R. R. Clark</name><affiliation wicri:level="1"><mods:affiliation>University of New Hampshire, U.S.A.</mods:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>University of New Hampshire</wicri:regionArea></affiliation></author><author><name sortKey="Kato, S" sort="Kato, S" uniqKey="Kato S" first="S." last="Kato">S. Kato</name><affiliation wicri:level="1"><mods:affiliation>Kyoto University, Japan</mods:affiliation><country xml:lang="fr">Japon</country><wicri:regionArea>Kyoto University</wicri:regionArea></affiliation></author><author><name sortKey="Tsuda, T" sort="Tsuda, T" uniqKey="Tsuda T" first="T." last="Tsuda">T. Tsuda</name><affiliation wicri:level="1"><mods:affiliation>Kyoto University, Japan</mods:affiliation><country xml:lang="fr">Japon</country><wicri:regionArea>Kyoto University</wicri:regionArea></affiliation></author></analytic><monogr></monogr><series><title level="j">Advances in Space Research</title><title level="j" type="abbrev">JASR</title><idno type="ISSN">0273-1177</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1987">1987</date><biblScope unit="volume">7</biblScope><biblScope unit="issue">10</biblScope><biblScope unit="page" from="143">143</biblScope><biblScope unit="page" to="153">153</biblScope></imprint><idno type="ISSN">0273-1177</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0273-1177</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Adelaide</term><term>Atmos</term><term>December</term><term>Early winter</term><term>Easterly</term><term>Easterly flow</term><term>Equatorward</term><term>Equatorward flow</term><term>Geostrophic</term><term>Geostrophic wind</term><term>Geostrophic winds</term><term>Global radar network</term><term>Hanson</term><term>July</term><term>Last decade</term><term>Longitudinal differences</term><term>Longitudinal variations</term><term>Manson</term><term>Meridional</term><term>Meridional flow</term><term>Meridional wind comparisons</term><term>Meridional winds</term><term>Meteor radars</term><term>Middle atmosphere program</term><term>Negative winds</term><term>Physica scripta</term><term>Planetary waves</term><term>Poleward flow</term><term>Positive winds</term><term>Primrose lake</term><term>Radar stations</term><term>Radar winds</term><term>Saskatoon</term><term>Satellite data</term><term>Satellite wind comparisons</term><term>Scostep secretariat</term><term>Scott base</term><term>Secular trends</term><term>Significant differences</term><term>Stratospheric warmings</term><term>Strophic winds</term><term>Summer flow</term><term>Time resolution</term><term>Upper middle atmosphere</term><term>Westerly flow</term><term>Wind data</term><term>Wind shears</term><term>Zonal</term><term>Zonal winds</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Adelaide</term><term>Atmos</term><term>December</term><term>Early winter</term><term>Easterly</term><term>Easterly flow</term><term>Equatorward</term><term>Equatorward flow</term><term>Geostrophic</term><term>Geostrophic wind</term><term>Geostrophic winds</term><term>Global radar network</term><term>Hanson</term><term>July</term><term>Last decade</term><term>Longitudinal differences</term><term>Longitudinal variations</term><term>Manson</term><term>Meridional</term><term>Meridional flow</term><term>Meridional wind comparisons</term><term>Meridional winds</term><term>Meteor radars</term><term>Middle atmosphere program</term><term>Negative winds</term><term>Physica scripta</term><term>Planetary waves</term><term>Poleward flow</term><term>Positive winds</term><term>Primrose lake</term><term>Radar stations</term><term>Radar winds</term><term>Saskatoon</term><term>Satellite data</term><term>Satellite wind comparisons</term><term>Scostep secretariat</term><term>Scott base</term><term>Secular trends</term><term>Significant differences</term><term>Stratospheric warmings</term><term>Strophic winds</term><term>Summer flow</term><term>Time resolution</term><term>Upper middle atmosphere</term><term>Westerly flow</term><term>Wind data</term><term>Wind shears</term><term>Zonal</term><term>Zonal winds</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: A substantial quantity of wind data have been assembled from radar systems since CIRA-72 was formed: most of these radars include height ranging, and operate on a regular and even continuous basis. Systems include meteor and MF (medium frequency) Radars: an MST (mesosphere-stratosphere-troposphere) Radar (meteor mode); and an LF (low frequency) drift system. Latitudes represented are near 20° N/S, 35° N/S, 45° N/S, 50°N, 65° N/S. In all cases tidal oscillations were calculated so that corrected mean winds (zonal, meridional) are available - the meridional was not included in CIRA-72. Means for groups of years near 1980 are available, as well as individual recent years (1983, 1984) to allow assessment of secular trends: revised and improved analysis has been completed for several stations.Height-time cross-sections have been formed for each observatory: heights are typically ∼75–110 km, with time resolution of 7–30 days. Such detailed cross-sections were almost unknown before 1972. Comparisons with CIRA-72 are shown, and these emphasize the differences between hemispheres (NH, SH) in the radar winds. Other new winds from rockets and satellite radiances are contrasted with the radar set. There are important differences with the satellite-derived geostrophic winds (1973–78): possible explanations involve secular trends, longitudinal variations, and ageostrophy.</div></front></TEI></record>Pour manipuler ce document sous Unix (Dilib)
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