Thermal structure of the mesopause region during the WADIS-2 rocket campaign

dc.bibliographicCitation.firstPage77eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
dc.bibliographicCitation.volume19eng
dc.contributor.authorWörl, R.
dc.contributor.authorStrelnikov, B.
dc.contributor.authorViehl, T.P.
dc.contributor.authorHöffner, J.
dc.contributor.authorPautet, P.-D.
dc.contributor.authorTaylor, M.J.
dc.contributor.authorZhao, Y.
dc.contributor.authorLöbken, F.-J.
dc.date.accessioned2020-11-25T14:52:42Z
dc.date.available2020-11-25T14:52:42Z
dc.date.issued2019
dc.description.abstractThis paper presents simultaneous temperature measurements by three independent instruments during the WADIS-2 rocket campaign in northern Norway (69° N, 14° E) on 5 March 2015. Vertical profiles were measured in situ with the CONE instrument. Continuous mobile IAP Fe lidar (Fe lidar) measurements during a period of 24 h, as well as horizontally resolved temperature maps by the Utah State University (USU) Advanced Mesospheric Temperature Mapper (AMTM) in the mesopause region, are analysed. Vertical and horizontal temperature profiles by all three instruments are in good agreement. A harmonic analysis of the Fe lidar measurements shows the presence of waves with periods of 24, 12, 8, and 6 h. Strong waves with amplitudes of up to 10K at 8 and 6 h are found. The 24 and 12 h components play only a minor role during these observations. In contrast only a few short periodic gravity waves are found. Horizontally resolved temperatures measured with the AMTM in the hydroxyl (OH) layer are used to connect the vertical temperature profiles. In the field of view of 200km×160km only small deviations from the horizontal mean of the order of 5K are found. Therefore only weak gravity wave signatures occurred. This suggests horizontal structures of more than 200 km. A comparison of Fe lidar, rocket-borne measurements, and AMTM temperatures indicates an OH centroid altitude of about 85 km. © 2019 Copernicus GmbH. All rights reserved.eng
dc.description.fondsLeibniz_Fonds
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://doi.org/10.34657/4631
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6002
dc.language.isoengeng
dc.publisherGöttingen : Copernicus GmbHeng
dc.relation.doihttps://doi.org/10.5194/acp-19-77-2019
dc.relation.issn1680-7316
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.othergravity waveeng
dc.subject.othermesopauseeng
dc.subject.othertemperature profileeng
dc.subject.otherthermal structureeng
dc.subject.othervertical profileeng
dc.subject.otherNorwayeng
dc.titleThermal structure of the mesopause region during the WADIS-2 rocket campaigneng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorIAPeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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