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          Institute: MPI für Kernphysik     Collection: Physics of Atmospheric Molecular Processes     Display Documents



  history
ID: 29154.0, MPI für Kernphysik / Physics of Atmospheric Molecular Processes
Dehydration in the Arctic stratosphere during the SOLVE/THESEO- 2000 campaigns
Authors:Schiller, C.; Bauer, R.; Cairo, F.; Deshler, T.; Dornbrack, A.; Elkins, J.; Engel, A.; Flentje, H.; Larsen, N.; Levin, I.; Muller, M.; Oltmans, S.; Ovarlez, H.; Ovarlez, J.; Schreiner, J.; Stroh, F.; Voigt, C.; Vomel, H.
Language:English
Date of Publication (YYYY-MM-DD):2002-09
Title of Journal:Journal of Geophysical Research-Atmospheres
Journal Abbrev.:J. Geophys. Res.-Atmos.
Volume:107
Issue / Number:D20
Start Page:8293
End Page:8293
Sequence Number of Article:8293
Review Status:Peer-review
Audience:Experts Only
Abstract / Description:Balloon-borne measurements of H2O, CH4, and H-2 in January and March 2000 show clear evidence for dehydration inside the polar vortex. At 30-50 hPa, total hydrogen is reduced by approximately 0.5 ppmv. This phenomenon is apparent in all five in situ balloon observations of this period; therefore it is probable that dehydration occurred over extended regions and a long period of this winter which was characterized by a well- confined vortex and low stratospheric temperatures. At altitudes below 50 hPa, where dehydration was strongest in previous Arctic observations and in the austral spring, total hydrogen values (2.CH4 +H2O + H-2) were similar to those found in Arctic profiles from other years where there was no dehydration and to those found at midlatitudes. In some of the dehydrated air masses, small solid particles were found whose crystallization might be connected to the earlier formation of ice particles. Back trajectory calculations for the January observations indicate that the probed air masses had experienced temperatures below the ice frost point in a synoptic-scale cold region several days before the observations. Most likely, the air was dehydrated there. In addition, temperatures in these air masses dropped below ice saturation several hours prior to the observations in the lee of the Scandinavian mountain ridge. For the March measurements, no ice saturation was apparent in the recent history of the air masses, again indicating that dehydration in the Arctic winter 1999/2000 was not a local phenomenon.
Free Keywords:water vapor; total hydrogen; Arctic stratosphere; dehydration
External Publication Status:published
Document Type:Article
Affiliations:MPI für Kernphysik/Group K. Mauersberger/Aerosols in Polar Stratospheric Clouds (J. Schreiner)
External Affiliations:KFA Julich GmbH, Forschungszentrum, Inst Chem & Dynam Geosphare 1, D-52425 Julich, Germany; CNR, Inst Fis Atmosfera, I-00133 Rome, Italy; Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA; Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, D-82234 Wessling, Germany; NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80303 USA; Univ Frankfurt, Inst Meteorol & Geophys, D-60054 Frankfurt, Germany; Danish Meteorol Inst, DK-2100 Copenhagen, Denmark; Univ Heidelberg, Inst Umweltphys, D-69120 Heidelberg, Germany; Ecole Polytech, CNRS, Meteorol Dynam Lab, F-91128 Palaiseau, France
Identifiers:ISI:000180466200080 [ID No:1]
ISSN:0747-7309 [ID No:2]
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