Validation of GOME total ozone by means of the Norwegian ozone monitoring network

The Global Ozone Monitoring Experiment (GOME) onboard the ERS-2 satellite has been in operation since July 1995. The Norwegian ground-based total ozone network has played an important role both in the main validation during the commissioning phase and in the validation of upgraded versions of the an...

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Published in:Annales Geophysicae
Main Authors: G. Hansen, A. Dahlback, F. Tønnessen, T. Svenøe
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 1999
Subjects:
Online Access:https://doi.org/10.1007/s00585-999-0430-9
https://doaj.org/article/83e9a53fb4684890915b21b60897b57e
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author G. Hansen
A. Dahlback
F. Tønnessen
T. Svenøe
author_facet G. Hansen
A. Dahlback
F. Tønnessen
T. Svenøe
author_sort G. Hansen
collection Directory of Open Access Journals: DOAJ Articles
container_issue 3
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container_title Annales Geophysicae
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description The Global Ozone Monitoring Experiment (GOME) onboard the ERS-2 satellite has been in operation since July 1995. The Norwegian ground-based total ozone network has played an important role both in the main validation during the commissioning phase and in the validation of upgraded versions of the analysis algorithms of the instrument. The ground-based network consists of various spectrometer types (Dobson, Brewer, UV filter instruments). The validation of the second algorithm version used until January 1998 reveals a very good agreement between GOME and ground-based data at solar zenith angles <60° and deviations of GOME total ozone data from ground-based data of up to ±60 DU (~20%) at zenith angles >60°. The deviations strongly depend on the season of the year, being negative in summer and positive in winter/spring, The deviations furthermore show a considerable scattering (up to ±25 DU in monthly average values of 5° SZA intervals), even in close spatial and temporal coincidence with ground-based measurements, especially in the high Arctic. The deviations are also dependent on the viewing geometry/ground pixel size with an additional negative offset for the large pixels used in the backswath mode and at solar zenith angles >85°, compared to forward-swath pixels. Key words. Atmospheric composition and structure (middle atmosphere · composition and chemistry; instruments and techniques)
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spelling ftdoajarticles:oai:doaj.org/article:83e9a53fb4684890915b21b60897b57e 2025-01-16T20:40:46+00:00 Validation of GOME total ozone by means of the Norwegian ozone monitoring network G. Hansen A. Dahlback F. Tønnessen T. Svenøe 1999-03-01T00:00:00Z https://doi.org/10.1007/s00585-999-0430-9 https://doaj.org/article/83e9a53fb4684890915b21b60897b57e EN eng Copernicus Publications https://www.ann-geophys.net/17/430/1999/angeo-17-430-1999.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.1007/s00585-999-0430-9 0992-7689 1432-0576 https://doaj.org/article/83e9a53fb4684890915b21b60897b57e Annales Geophysicae, Vol 17, Pp 430-436 (1999) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 1999 ftdoajarticles https://doi.org/10.1007/s00585-999-0430-9 2022-12-31T03:22:04Z The Global Ozone Monitoring Experiment (GOME) onboard the ERS-2 satellite has been in operation since July 1995. The Norwegian ground-based total ozone network has played an important role both in the main validation during the commissioning phase and in the validation of upgraded versions of the analysis algorithms of the instrument. The ground-based network consists of various spectrometer types (Dobson, Brewer, UV filter instruments). The validation of the second algorithm version used until January 1998 reveals a very good agreement between GOME and ground-based data at solar zenith angles <60° and deviations of GOME total ozone data from ground-based data of up to ±60 DU (~20%) at zenith angles >60°. The deviations strongly depend on the season of the year, being negative in summer and positive in winter/spring, The deviations furthermore show a considerable scattering (up to ±25 DU in monthly average values of 5° SZA intervals), even in close spatial and temporal coincidence with ground-based measurements, especially in the high Arctic. The deviations are also dependent on the viewing geometry/ground pixel size with an additional negative offset for the large pixels used in the backswath mode and at solar zenith angles >85°, compared to forward-swath pixels. Key words. Atmospheric composition and structure (middle atmosphere · composition and chemistry; instruments and techniques) Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Annales Geophysicae 17 3 430 436
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
G. Hansen
A. Dahlback
F. Tønnessen
T. Svenøe
Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title_full Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title_fullStr Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title_full_unstemmed Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title_short Validation of GOME total ozone by means of the Norwegian ozone monitoring network
title_sort validation of gome total ozone by means of the norwegian ozone monitoring network
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
url https://doi.org/10.1007/s00585-999-0430-9
https://doaj.org/article/83e9a53fb4684890915b21b60897b57e