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dc.contributor.authorHauchecorne, A.
dc.contributor.authorBertaux, J.L.
dc.contributor.authorDalaudier, F.
dc.contributor.authorKeckhut, P.
dc.contributor.authorLemennais, P.
dc.contributor.authorBekki, S.
dc.contributor.authorMarchand, M.
dc.contributor.authorLebrun, J.C.
dc.contributor.authorKyrölä, E.
dc.contributor.authorTamminen, J.
dc.contributor.authorSofieva, V.
dc.contributor.authorFussen, D.
dc.contributor.authorVanhellemont, F.
dc.contributor.authorFanton d'Andon, O.
dc.contributor.authorBarrot, G.
dc.contributor.authorBlanot, L.
dc.contributor.authorFehr, T.
dc.contributor.authorSaavedra de Miguel, L.
dc.date2010
dc.date.accessioned2016-03-31T12:16:17Z
dc.date.available2016-03-31T12:16:17Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/3225
dc.languageeng
dc.titleResponse of tropical stratospheric O3, NO2 and NO3 to the equatorial Quasi-Biennial Oscillation and to temperature as seen from GOMOS/ENVISAT
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titleAtmospheric Chemistry and Physics
dc.source.volume10
dc.source.issue18
dc.source.page8873-8879
Orfeo.peerreviewedYes
dc.identifier.doi10.5194/acp-10-8873-2010


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