Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland

A polar stratospheric ice cloud (PSC type II) was observed by airborne lidar above Greenland on 14 January 2000. It was the unique observation of an ice cloud over Greenland during the SOLVE/THESEO 2000 campaign. Mesoscale simulations with the hydrostatic HRM model are presented which, in contrast t...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Buss, S., Hertzog, A., Hostettler, C., Bui, T. B., Lüthi, D., Wernli, H.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
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Online Access:https://doi.org/10.5194/acp-4-1183-2004
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00049252 2023-05-15T16:25:53+02:00 Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland Buss, S. Hertzog, A. Hostettler, C. Bui, T. B. Lüthi, D. Wernli, H. 2004-08 electronic https://doi.org/10.5194/acp-4-1183-2004 https://noa.gwlb.de/receive/cop_mods_00049252 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00048872/acp-4-1183-2004.pdf https://acp.copernicus.org/articles/4/1183/2004/acp-4-1183-2004.pdf eng eng Copernicus Publications Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324 https://doi.org/10.5194/acp-4-1183-2004 https://noa.gwlb.de/receive/cop_mods_00049252 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00048872/acp-4-1183-2004.pdf https://acp.copernicus.org/articles/4/1183/2004/acp-4-1183-2004.pdf https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2004 ftnonlinearchiv https://doi.org/10.5194/acp-4-1183-2004 2022-02-08T22:37:36Z A polar stratospheric ice cloud (PSC type II) was observed by airborne lidar above Greenland on 14 January 2000. It was the unique observation of an ice cloud over Greenland during the SOLVE/THESEO 2000 campaign. Mesoscale simulations with the hydrostatic HRM model are presented which, in contrast to global analyses, are capable to produce a vertically propagating gravity wave that induces the low temperatures at the level of the PSC afforded for the ice formation. The simulated minimum temperature is ~8 K below the driving analyses and ~4.5 K below the frost point, exactly coinciding with the location of the observed ice cloud. Despite the high elevations of the Greenland orography the simulated gravity wave is not a mountain wave. Analyses of the horizontal wind divergence, of the background wind profiles, of backward gravity wave ray-tracing trajectories, of HRM experiments with reduced Greenland topography and of several diagnostics near the tropopause level provide evidence that the wave is emitted from an intense, rapidly evolving, anticyclonically curved jet stream. The precise physical process responsible for the wave emission could not be identified definitely, but geostrophic adjustment and shear instability are likely candidates. In order to evaluate the potential frequency of such non-orographic polar stratospheric cloud events, the non-linear balance equation diagnostic is performed for the winter 1999/2000. It indicates that ice-PSCs are only occasionally generated by gravity waves emanating from spontaneous adjustment. Article in Journal/Newspaper Greenland Niedersächsisches Online-Archiv NOA Greenland Atmospheric Chemistry and Physics 4 5 1183 1200
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Buss, S.
Hertzog, A.
Hostettler, C.
Bui, T. B.
Lüthi, D.
Wernli, H.
Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
topic_facet article
Verlagsveröffentlichung
description A polar stratospheric ice cloud (PSC type II) was observed by airborne lidar above Greenland on 14 January 2000. It was the unique observation of an ice cloud over Greenland during the SOLVE/THESEO 2000 campaign. Mesoscale simulations with the hydrostatic HRM model are presented which, in contrast to global analyses, are capable to produce a vertically propagating gravity wave that induces the low temperatures at the level of the PSC afforded for the ice formation. The simulated minimum temperature is ~8 K below the driving analyses and ~4.5 K below the frost point, exactly coinciding with the location of the observed ice cloud. Despite the high elevations of the Greenland orography the simulated gravity wave is not a mountain wave. Analyses of the horizontal wind divergence, of the background wind profiles, of backward gravity wave ray-tracing trajectories, of HRM experiments with reduced Greenland topography and of several diagnostics near the tropopause level provide evidence that the wave is emitted from an intense, rapidly evolving, anticyclonically curved jet stream. The precise physical process responsible for the wave emission could not be identified definitely, but geostrophic adjustment and shear instability are likely candidates. In order to evaluate the potential frequency of such non-orographic polar stratospheric cloud events, the non-linear balance equation diagnostic is performed for the winter 1999/2000. It indicates that ice-PSCs are only occasionally generated by gravity waves emanating from spontaneous adjustment.
format Article in Journal/Newspaper
author Buss, S.
Hertzog, A.
Hostettler, C.
Bui, T. B.
Lüthi, D.
Wernli, H.
author_facet Buss, S.
Hertzog, A.
Hostettler, C.
Bui, T. B.
Lüthi, D.
Wernli, H.
author_sort Buss, S.
title Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
title_short Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
title_full Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
title_fullStr Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
title_full_unstemmed Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland
title_sort analysis of a jet stream induced gravity wave associated with an observed ice cloud over greenland
publisher Copernicus Publications
publishDate 2004
url https://doi.org/10.5194/acp-4-1183-2004
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https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00048872/acp-4-1183-2004.pdf
https://acp.copernicus.org/articles/4/1183/2004/acp-4-1183-2004.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_relation Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324
https://doi.org/10.5194/acp-4-1183-2004
https://noa.gwlb.de/receive/cop_mods_00049252
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00048872/acp-4-1183-2004.pdf
https://acp.copernicus.org/articles/4/1183/2004/acp-4-1183-2004.pdf
op_rights https://open-access.net/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/acp-4-1183-2004
container_title Atmospheric Chemistry and Physics
container_volume 4
container_issue 5
container_start_page 1183
op_container_end_page 1200
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