Validation of GOME ozone profiles by means of the ALOMAR ozone lidar

Ozone vertical profiles derived from nadir measurements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the University of Bremen, are validated against measurements with the stratospheric ozone lidar at the ALOMAR facility in North-Norway. A set of 43 measureme...

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Published in:Annales Geophysicae
Main Authors: G. Hansen, K. Bramstedt, V. Rozanov, M. Weber, J. P. Burrows
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2003
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-21-1879-2003
https://doaj.org/article/8f9c7b2f391943b5a5aa3cf9800a12e9
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spelling ftdoajarticles:oai:doaj.org/article:8f9c7b2f391943b5a5aa3cf9800a12e9 2023-05-15T17:39:24+02:00 Validation of GOME ozone profiles by means of the ALOMAR ozone lidar G. Hansen K. Bramstedt V. Rozanov M. Weber J. P. Burrows 2003-08-01T00:00:00Z https://doi.org/10.5194/angeo-21-1879-2003 https://doaj.org/article/8f9c7b2f391943b5a5aa3cf9800a12e9 EN eng Copernicus Publications https://www.ann-geophys.net/21/1879/2003/angeo-21-1879-2003.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-21-1879-2003 0992-7689 1432-0576 https://doaj.org/article/8f9c7b2f391943b5a5aa3cf9800a12e9 Annales Geophysicae, Vol 21, Pp 1879-1886 (2003) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2003 ftdoajarticles https://doi.org/10.5194/angeo-21-1879-2003 2022-12-31T12:06:28Z Ozone vertical profiles derived from nadir measurements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the University of Bremen, are validated against measurements with the stratospheric ozone lidar at the ALOMAR facility in North-Norway. A set of 43 measurements, taken in the period August 1996 to September 1999 with a maximum distance between the ground-based site and the GOME pixel centre of 650 km, is used. The comparison shows a satisfactory agreement within less than ± 7% in the altitude range 15 to 30 km, independent of the season of the year. At lower altitudes, average deviations of the GOME profiles from lidar measurements of up to - 15% occur in spring, the reason for which has to be found in the FURM algorithm, while the agreement is within ± 5% in both winter and summer/autumn months. At altitudes above 30 km, significant seasonally varying discrepancies occur, being largest in winter ( - 40% on average at 40 km altitude) and smallest in summer (less than - 10%). The source of these deviations is most likely related to a radiance and irradiance calibration problem in the GOME data below 300 nm, which are used to derive ozone at the highest altitudes. The validation also shows that it is very important to choose the right ozone climatology for initialisation. Satisfactory results in spring 1997, when the polar stratospheric vortex was very stable, are only achieved, if a winter (vortex) profile is used. Key words. Atmospheric composition and structure (middle atmosphere-composition and chemistry; instruments and techniques; general or miscellaneous) Article in Journal/Newspaper North Norway Directory of Open Access Journals: DOAJ Articles Norway Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Annales Geophysicae 21 8 1879 1886
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
G. Hansen
K. Bramstedt
V. Rozanov
M. Weber
J. P. Burrows
Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description Ozone vertical profiles derived from nadir measurements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the University of Bremen, are validated against measurements with the stratospheric ozone lidar at the ALOMAR facility in North-Norway. A set of 43 measurements, taken in the period August 1996 to September 1999 with a maximum distance between the ground-based site and the GOME pixel centre of 650 km, is used. The comparison shows a satisfactory agreement within less than ± 7% in the altitude range 15 to 30 km, independent of the season of the year. At lower altitudes, average deviations of the GOME profiles from lidar measurements of up to - 15% occur in spring, the reason for which has to be found in the FURM algorithm, while the agreement is within ± 5% in both winter and summer/autumn months. At altitudes above 30 km, significant seasonally varying discrepancies occur, being largest in winter ( - 40% on average at 40 km altitude) and smallest in summer (less than - 10%). The source of these deviations is most likely related to a radiance and irradiance calibration problem in the GOME data below 300 nm, which are used to derive ozone at the highest altitudes. The validation also shows that it is very important to choose the right ozone climatology for initialisation. Satisfactory results in spring 1997, when the polar stratospheric vortex was very stable, are only achieved, if a winter (vortex) profile is used. Key words. Atmospheric composition and structure (middle atmosphere-composition and chemistry; instruments and techniques; general or miscellaneous)
format Article in Journal/Newspaper
author G. Hansen
K. Bramstedt
V. Rozanov
M. Weber
J. P. Burrows
author_facet G. Hansen
K. Bramstedt
V. Rozanov
M. Weber
J. P. Burrows
author_sort G. Hansen
title Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
title_short Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
title_full Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
title_fullStr Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
title_full_unstemmed Validation of GOME ozone profiles by means of the ALOMAR ozone lidar
title_sort validation of gome ozone profiles by means of the alomar ozone lidar
publisher Copernicus Publications
publishDate 2003
url https://doi.org/10.5194/angeo-21-1879-2003
https://doaj.org/article/8f9c7b2f391943b5a5aa3cf9800a12e9
long_lat ENVELOPE(-67.083,-67.083,-68.133,-68.133)
geographic Norway
Alomar
geographic_facet Norway
Alomar
genre North Norway
genre_facet North Norway
op_source Annales Geophysicae, Vol 21, Pp 1879-1886 (2003)
op_relation https://www.ann-geophys.net/21/1879/2003/angeo-21-1879-2003.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-21-1879-2003
0992-7689
1432-0576
https://doaj.org/article/8f9c7b2f391943b5a5aa3cf9800a12e9
op_doi https://doi.org/10.5194/angeo-21-1879-2003
container_title Annales Geophysicae
container_volume 21
container_issue 8
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