Supersaturation, Dehydration, and Denitrification in Arctic Cirrus

A polar cirrus case study is discussed with the help of a one-dimensional model with explicit aerosol and ice microphysics. It is demonstrated that continuous cooling of air in regions with small amounts of ice and slow ice deposition rates of water vapor drives significant in-cloud supersaturations...

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Main Author: Kärcher, B.
Format: Other Non-Article Part of Journal/Newspaper
Language:English
Published: Copernicus Publications 2005
Subjects:
Online Access:https://elib.dlr.de/18853/
https://elib.dlr.de/18853/1/acp-5-1757-2005.pdf
http://www.atmos-chem-phys.org/acp/5/1757/
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spelling ftdlr:oai:elib.dlr.de:18853 2023-05-15T14:23:20+02:00 Supersaturation, Dehydration, and Denitrification in Arctic Cirrus Kärcher, B. 2005 application/pdf https://elib.dlr.de/18853/ https://elib.dlr.de/18853/1/acp-5-1757-2005.pdf http://www.atmos-chem-phys.org/acp/5/1757/ en eng Copernicus Publications https://elib.dlr.de/18853/1/acp-5-1757-2005.pdf Kärcher, B. (2005) Supersaturation, Dehydration, and Denitrification in Arctic Cirrus. Atmospheric Chemistry and Physics, 5, Seiten 1757-1772. Copernicus Publications. Atmosphärische Spurenstoffe Zeitschriftenbeitrag PeerReviewed 2005 ftdlr 2019-05-05T22:52:51Z A polar cirrus case study is discussed with the help of a one-dimensional model with explicit aerosol and ice microphysics. It is demonstrated that continuous cooling of air in regions with small amounts of ice and slow ice deposition rates of water vapor drives significant in-cloud supersaturations over ice, with potentially important consequences for heterogeneous halogen activation. Radiatively important cloud properties such as ice crystal size distributions are investigated, showing the presence of high number concentrations of small crystals in the cloud top region at the tropopause, broad but highly variable size spectra in the cloud interior, and mostly large crystals at the cloud base. It is found that weakly forced Arctic cirrostratus are highly efficient at dehydrating upper tropospheric air. Estimating nitric acid uptake in cirrus with an unprecedented treatment of diffusion-limited trapping in growing ice crystals suggests that such clouds could also denitrify upper tropospheric air masses efficiently, but a closer comparison to suitable observations is needed to draw a definite conclusion on this point. It is also shown that low temperatures, high ice supersaturations, and the absence of ice above but close to the cloud top region cause efficient uptake of nitric acid in background aerosol particles. Other Non-Article Part of Journal/Newspaper Arctic Arctic German Aerospace Center: elib - DLR electronic library Arctic
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language English
topic Atmosphärische Spurenstoffe
spellingShingle Atmosphärische Spurenstoffe
Kärcher, B.
Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
topic_facet Atmosphärische Spurenstoffe
description A polar cirrus case study is discussed with the help of a one-dimensional model with explicit aerosol and ice microphysics. It is demonstrated that continuous cooling of air in regions with small amounts of ice and slow ice deposition rates of water vapor drives significant in-cloud supersaturations over ice, with potentially important consequences for heterogeneous halogen activation. Radiatively important cloud properties such as ice crystal size distributions are investigated, showing the presence of high number concentrations of small crystals in the cloud top region at the tropopause, broad but highly variable size spectra in the cloud interior, and mostly large crystals at the cloud base. It is found that weakly forced Arctic cirrostratus are highly efficient at dehydrating upper tropospheric air. Estimating nitric acid uptake in cirrus with an unprecedented treatment of diffusion-limited trapping in growing ice crystals suggests that such clouds could also denitrify upper tropospheric air masses efficiently, but a closer comparison to suitable observations is needed to draw a definite conclusion on this point. It is also shown that low temperatures, high ice supersaturations, and the absence of ice above but close to the cloud top region cause efficient uptake of nitric acid in background aerosol particles.
format Other Non-Article Part of Journal/Newspaper
author Kärcher, B.
author_facet Kärcher, B.
author_sort Kärcher, B.
title Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
title_short Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
title_full Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
title_fullStr Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
title_full_unstemmed Supersaturation, Dehydration, and Denitrification in Arctic Cirrus
title_sort supersaturation, dehydration, and denitrification in arctic cirrus
publisher Copernicus Publications
publishDate 2005
url https://elib.dlr.de/18853/
https://elib.dlr.de/18853/1/acp-5-1757-2005.pdf
http://www.atmos-chem-phys.org/acp/5/1757/
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_relation https://elib.dlr.de/18853/1/acp-5-1757-2005.pdf
Kärcher, B. (2005) Supersaturation, Dehydration, and Denitrification in Arctic Cirrus. Atmospheric Chemistry and Physics, 5, Seiten 1757-1772. Copernicus Publications.
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