A case study on the formation and evolution of ice supersaturation in the vicinity of a warm conveyor belt\'s outflow region
dc.contributor.author
Spichtinger, Peter
dc.contributor.author
Gierens, Klaus
dc.contributor.author
Wernli, Heini
dc.date.accessioned
2019-08-30T10:18:21Z
dc.date.available
2017-06-09T21:35:26Z
dc.date.available
2018-11-05T12:05:23Z
dc.date.available
2019-08-30T10:18:21Z
dc.date.issued
2005
dc.identifier.issn
1680-7324
dc.identifier.issn
1680-7375
dc.identifier.other
10.5194/acp-5-973-2005
en_US
dc.identifier.uri
http://hdl.handle.net/20.500.11850/48173
dc.identifier.doi
10.3929/ethz-b-000048173
dc.description.abstract
A case study is presented on the formation and evolution of an ice-supersaturated region (ISSR) that was detected by a radiosonde in NE Germany at 06:00 UTC 29 November 2000. The ISSR was situated in the vicinity of the outflow region of a warm conveyor belt associated with an intense event of cyclogenesis in the eastern North Atlantic. Using ECMWF analyses and trajectory calculations it is determined when the air parcels became supersaturated and later subsaturated again. In the case considered, the state of air parcel supersaturation can last for longer than 24h. The ISSR was unusually thick: while the mean vertical extension of ISSRs in NE Germany is about 500m, the one investigated here reached 3km. The ice-supersaturated region investigated was bordered both vertically and horizontally by strongly subsaturated air. Near the path of the radiosonde the ISSR was probably cloud free, as inferred from METEOSAT infrared images. However, at other locations within the ISSR it is probable that there were cirrus clouds. Relative humidity measurements obtained by the Lindenberg radiosonde are used to correct the negative bias of the ECMWF humidity and to construct two-dimensional maps of ice supersaturation over Europe during the considered period. A systematic backward trajectory analysis for the ISSRs on these maps shows that the ISSR air masses themselves experienced only a moderate upward motion during the previous days, whereas parts of the ISSRs were located just above strongly ascending air masses from the boundary layer. This indicates qualitatively that warm conveyor belts associated with mid-latitude cyclogenesis are disturbances that can induce the formation of ISSRs in the upper troposphere. The ISSR maps also lead us to a new perception of ISSRs as large dynamic regions of supersaturated air where cirrus clouds can be embedded at some locations while there is clear air at others.
en_US
dc.format
application/pdf
en_US
dc.language.iso
en
en_US
dc.publisher
Copernicus
en_US
dc.rights.uri
http://creativecommons.org/licenses/by-nc-sa/2.5/
dc.title
A case study on the formation and evolution of ice supersaturation in the vicinity of a warm conveyor belt\'s outflow region
en_US
dc.type
Journal Article
dc.rights.license
Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic
dc.date.published
2005-03-22
ethz.journal.title
Atmospheric Chemistry and Physics
ethz.journal.volume
5
en_US
ethz.journal.issue
4
en_US
ethz.journal.abbreviated
Atmos. Chem. Phys.
ethz.pages.start
973
en_US
ethz.pages.end
987
en_US
ethz.version.deposit
publishedVersion
en_US
ethz.identifier.nebis
004294181
ethz.publication.status
published
en_US
ethz.leitzahl
ETH Zürich::00002 - ETH Zürich::00012 - Lehre und Forschung::00007 - Departemente::02350 - Dep. Umweltsystemwissenschaften / Dep. of Environmental Systems Science::02717 - Institut für Atmosphäre und Klima / Inst. Atmospheric and Climate Science::03690 - Lohmann, Ulrike / Lohmann, Ulrike
en_US
ethz.leitzahl.certified
ETH Zürich::00002 - ETH Zürich::00012 - Lehre und Forschung::00007 - Departemente::02350 - Dep. Umweltsystemwissenschaften / Dep. of Environmental Systems Science::02717 - Institut für Atmosphäre und Klima / Inst. Atmospheric and Climate Science::03690 - Lohmann, Ulrike / Lohmann, Ulrike
ethz.date.deposited
2017-06-09T21:35:50Z
ethz.source
ECIT
ethz.identifier.importid
imp59364f23b31df62352
ethz.ecitpid
pub:79136
ethz.eth
yes
en_US
ethz.availability
Open access
en_US
ethz.rosetta.installDate
2017-07-18T10:09:49Z
ethz.rosetta.lastUpdated
2025-02-13T19:21:57Z
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true
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true
ethz.COinS
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