Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument

This paper presents the spatio-temporal distribution of NO y species at altitudes between 14 and 31 km as measured with the MIPAS-B instrument on the morning of 21 March 2003 in northern Scandinavia. At lower altitudes (below about 22 km), temperature variations, the distribution of ClONO 2 , and th...

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Main Authors: G. Maucher, H. Nordmeyer, A. Lengel, F. Friedl-Vallon, G. Wetzel, H. Oelhaf, R. Ruhnke, A. Kleinert, A. Wiegele, H. Fischer
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doaj.org/article/229e62038432411c948c9607cecb4ac7
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spelling ftdoajarticles:oai:doaj.org/article:229e62038432411c948c9607cecb4ac7 2023-05-15T15:06:12+02:00 Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument G. Maucher H. Nordmeyer A. Lengel F. Friedl-Vallon G. Wetzel H. Oelhaf R. Ruhnke A. Kleinert A. Wiegele H. Fischer 2009-02-01T00:00:00Z https://doaj.org/article/229e62038432411c948c9607cecb4ac7 EN eng Copernicus Publications http://www.atmos-chem-phys.net/9/1151/2009/acp-9-1151-2009.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 1680-7316 1680-7324 https://doaj.org/article/229e62038432411c948c9607cecb4ac7 Atmospheric Chemistry and Physics, Vol 9, Iss 4, Pp 1151-1163 (2009) Physics QC1-999 Chemistry QD1-999 article 2009 ftdoajarticles 2023-01-08T01:31:59Z This paper presents the spatio-temporal distribution of NO y species at altitudes between 14 and 31 km as measured with the MIPAS-B instrument on the morning of 21 March 2003 in northern Scandinavia. At lower altitudes (below about 22 km), temperature variations, the distribution of ClONO 2 , and the tracer N 2 O reveal the dynamics through the edge of the late arctic polar vortex. At higher altitudes, continuous measurement before, during, and after sunrise provides information about photochemistry illustrating the evolution of the photochemically active gases NO 2 and N 2 O 5 around sunrise. The measured temporal evolution of NO 2 and N 2 O 5 is compared to box modelling that is run along backward calculated trajectories. While the comparison of measured and modelled N 2 O 5 reveals significant differences, there is a good agreement between the model and observations for NO 2 in terms of volume mixing ratios but the simulated decrease shortly after sunrise is underestimated compared to the measurements. The differences are attributed to the photolysis rates used in the box model calculations. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
G. Maucher
H. Nordmeyer
A. Lengel
F. Friedl-Vallon
G. Wetzel
H. Oelhaf
R. Ruhnke
A. Kleinert
A. Wiegele
H. Fischer
Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
topic_facet Physics
QC1-999
Chemistry
QD1-999
description This paper presents the spatio-temporal distribution of NO y species at altitudes between 14 and 31 km as measured with the MIPAS-B instrument on the morning of 21 March 2003 in northern Scandinavia. At lower altitudes (below about 22 km), temperature variations, the distribution of ClONO 2 , and the tracer N 2 O reveal the dynamics through the edge of the late arctic polar vortex. At higher altitudes, continuous measurement before, during, and after sunrise provides information about photochemistry illustrating the evolution of the photochemically active gases NO 2 and N 2 O 5 around sunrise. The measured temporal evolution of NO 2 and N 2 O 5 is compared to box modelling that is run along backward calculated trajectories. While the comparison of measured and modelled N 2 O 5 reveals significant differences, there is a good agreement between the model and observations for NO 2 in terms of volume mixing ratios but the simulated decrease shortly after sunrise is underestimated compared to the measurements. The differences are attributed to the photolysis rates used in the box model calculations.
format Article in Journal/Newspaper
author G. Maucher
H. Nordmeyer
A. Lengel
F. Friedl-Vallon
G. Wetzel
H. Oelhaf
R. Ruhnke
A. Kleinert
A. Wiegele
H. Fischer
author_facet G. Maucher
H. Nordmeyer
A. Lengel
F. Friedl-Vallon
G. Wetzel
H. Oelhaf
R. Ruhnke
A. Kleinert
A. Wiegele
H. Fischer
author_sort G. Maucher
title Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
title_short Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
title_full Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
title_fullStr Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
title_full_unstemmed Spatio-temporal variations of NO y species in the northern latitudes stratosphere measured with the balloon-borne MIPAS instrument
title_sort spatio-temporal variations of no y species in the northern latitudes stratosphere measured with the balloon-borne mipas instrument
publisher Copernicus Publications
publishDate 2009
url https://doaj.org/article/229e62038432411c948c9607cecb4ac7
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmospheric Chemistry and Physics, Vol 9, Iss 4, Pp 1151-1163 (2009)
op_relation http://www.atmos-chem-phys.net/9/1151/2009/acp-9-1151-2009.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
1680-7316
1680-7324
https://doaj.org/article/229e62038432411c948c9607cecb4ac7
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