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dc.contributor.authorShepherd, M.G.
dc.contributor.authorWu, D.L.
dc.contributor.authorFedulina, I.N.
dc.contributor.authorGurubaran, S.
dc.contributor.authorRussell, J.M.
dc.contributor.authorMlynczak, M.G.
dc.contributor.authorShepherd, G.G.
dc.date.accessioned2015-09-11T09:18:24Z
dc.date.accessioned2021-02-12T09:28:45Z-
dc.date.available2015-09-11T09:18:24Z
dc.date.available2021-02-12T09:28:45Z-
dc.date.issued2007
dc.identifier.citationJournal of Atmospheric and Solar-Terrestrial Physics, v.69/17-18, p.2309-2337, 2007, doi: 10.1016/j.jastp.2007.04.009en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/384-
dc.description.abstractTemperature observations at 20–90 km height and 5–15°N during the winter of 1992–1993, 1993–1994 and 2003–2004, from the Wind Imaging Interferometer (WINDII) and Microwave Limb Sounder (MLS) experiments on the Upper Atmosphere Research Satellite (UARS) satellite and the Sounding the Atmosphere using Broadband Emission Radiometry (SABER) experiment on the Thermosphere, Ionosphere, Mesosphere Energetics and Dynamics (TIMED) satellite are analyzed together with MF radar winds and UK Meteorological Office (UKMO) assimilated fields. Mesospheric cooling is observed at the time of stratospheric warming at the tropics correlative with stratospheric warming events at middle and high latitudes. Planetary waves m=1 with periods of 4–5, 6–8, 10 and 12–18 days are found to dominate the period. Westward 7- and 16-day waves at the tropics appear enhanced by stationary planetary waves during sudden stratospheric warming events.en_US
dc.language.isoenen_US
dc.subjectTropical mesosphereen_US
dc.subjectTemperaturesen_US
dc.subjectStratospheric warmingen_US
dc.subjectSatellitesen_US
dc.subjectSSWen_US
dc.titleStratospheric warming effects on the tropical mesospheric temperature fielden_US
dc.typeArticleen_US
dc.identifier.accession090877
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