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000062637 0881_ $$aJuel-4267
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000062637 1001_ $$0P:(DE-Juel1)VDB54359$$aSilva dos Santos, Fabio Henrique$$b0$$eCorresponding author$$uFZJ
000062637 245__ $$aHydratation und Dehydratation in der tropischen Tropopausenschicht
000062637 260__ $$aJülich$$bForschungszentrum Jülich GmbH Zentralbibliothek, Verlag$$c2008
000062637 300__ $$aX, 140 p.
000062637 3367_ $$0PUB:(DE-HGF)11$$2PUB:(DE-HGF)$$aDissertation / PhD Thesis
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000062637 4900_ $$0PERI:(DE-600)2414853-2$$831251$$aBerichte des Forschungszentrums Jülich$$v4267$$x0944-2952
000062637 502__ $$aWuppertal, Univ., Diss., 2008$$bDr. (Univ.)$$cUniv. Wuppertal$$d2008
000062637 500__ $$aRecord converted from VDB: 12.11.2012
000062637 520__ $$aThe topic of this PhD thesis is the abundance of water vapour at the tropical tropopause. For this purpose measurements were made with the hygrometer FISH of ICG-1 from the Research Centre J¨ulich onboard the hight altitude aircraft Geophysica. This experimental work was carried out during two field campaigns in 2005 in Brazil (TROCCINOX) and Australia (SCOUT-O3). Additional data from two other tropical campaigns in Africa (AMMA) and over the Indian Ocean (APE-THESEO) were also analysed. A seasonal cycle of the tropopause height was confirmed by the observed vertical profiles of water vapour (hygropause), saturation over ice and temperature (cold point tropopause). The data collected during the transfer flights show a seasonal motion of the tropical tropopause. The water mixing ratio in the UT/LS region is controlled by two different regimes: local processes below about 410 K potential temperature and large scale processes above this level. A propagation of water vapour in the stratosphere consistent with the tape recorder theory is shown. Particles were measured during the flights at the upper boundary of convection. These particles evaporate before they sediment again below the tropopause. Futhermore the data show that a significant quantity of water — more than previously thought — is transported into the stratosphere by means of convection. Isolated profiles over Africa show increased water vapour in unsaturated air masses in clear sky. Analysis of backward trajectories in conjunction with satellite data show that it originates from areas with overshooting convection. The background of the measured water concentration over Africa during the measurements was affected by asian monsoon regions.
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000062637 655_7 $$aHochschulschrift$$xDissertation (Univ.)
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000062637 9201_ $$0I:(DE-Juel1)VDB790$$d30.09.2010$$gICG$$kICG-1$$lStratosphäre$$x1
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