Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard

The historical total ozone measurements taken with Dobson Spectrophotometer #8 at Longyearbyen (78.2° N, 15.6° E), Svalbard, Norway, in the period 1950–1962 have been re-analyzed and homogenized based on the original measurement logs, using present-day procedures. In lack of sufficient calibration i...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Vogler, C., Brönnimann, S., Hansen, G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-6-4763-2006
https://www.atmos-chem-phys.net/6/4763/2006/
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spelling ftcopernicus:oai:publications.copernicus.org:acp3824 2023-05-15T17:08:28+02:00 Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard Vogler, C. Brönnimann, S. Hansen, G. 2018-06-28 application/pdf https://doi.org/10.5194/acp-6-4763-2006 https://www.atmos-chem-phys.net/6/4763/2006/ eng eng doi:10.5194/acp-6-4763-2006 https://www.atmos-chem-phys.net/6/4763/2006/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-6-4763-2006 2019-12-24T09:58:44Z The historical total ozone measurements taken with Dobson Spectrophotometer #8 at Longyearbyen (78.2° N, 15.6° E), Svalbard, Norway, in the period 1950–1962 have been re-analyzed and homogenized based on the original measurement logs, using present-day procedures. In lack of sufficient calibration information, an empirical quality assessment was performed, based on a climatological comparison with ozone measurements in Tromsø, using TOMS data at both sites in the period 1979–2001, and ground-based Dobson data in the period 1950–1962. The assessment revealed that the C wavelength pair direct-sun (DS) measurements are most trustworthy (and most frequent), while the WMO standard reference mode AD direct-sun has a systematic bias. Zenith-blue (ZB) measurements at solar zenith angles (SZA) <78° were adjusted to DS data using different empirical functions before and after 1957 (the start of the International Geophysical Year). ZB measurements at larger SZAs were homogenized by means of a normalization function derived from days with measurements over a wide range of SZAs. Zenith-cloudy measurements, which are particularly frequent during the summer months, were homogenized by applying correction factors depending on the cloud type (high thin clouds and medium to low thick clouds). The combination of all measurements yields a total of 4685 single values, covering 1637 days from September 1950 to September 1962; moon measurements during the polar night add another 137 daily means. The re-evaluated data show a convincing consistence with measurements since 1979 (TOMS, SAOZ, Dobson) as well as with the 1957–1962 data stored at the World Ozone and UV Data Centre (WOUDC). Text Longyearbyen polar night Svalbard Tromsø Copernicus Publications: E-Journals Longyearbyen Norway Svalbard Tromsø Atmospheric Chemistry and Physics 6 12 4763 4773
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The historical total ozone measurements taken with Dobson Spectrophotometer #8 at Longyearbyen (78.2° N, 15.6° E), Svalbard, Norway, in the period 1950–1962 have been re-analyzed and homogenized based on the original measurement logs, using present-day procedures. In lack of sufficient calibration information, an empirical quality assessment was performed, based on a climatological comparison with ozone measurements in Tromsø, using TOMS data at both sites in the period 1979–2001, and ground-based Dobson data in the period 1950–1962. The assessment revealed that the C wavelength pair direct-sun (DS) measurements are most trustworthy (and most frequent), while the WMO standard reference mode AD direct-sun has a systematic bias. Zenith-blue (ZB) measurements at solar zenith angles (SZA) <78° were adjusted to DS data using different empirical functions before and after 1957 (the start of the International Geophysical Year). ZB measurements at larger SZAs were homogenized by means of a normalization function derived from days with measurements over a wide range of SZAs. Zenith-cloudy measurements, which are particularly frequent during the summer months, were homogenized by applying correction factors depending on the cloud type (high thin clouds and medium to low thick clouds). The combination of all measurements yields a total of 4685 single values, covering 1637 days from September 1950 to September 1962; moon measurements during the polar night add another 137 daily means. The re-evaluated data show a convincing consistence with measurements since 1979 (TOMS, SAOZ, Dobson) as well as with the 1957–1962 data stored at the World Ozone and UV Data Centre (WOUDC).
format Text
author Vogler, C.
Brönnimann, S.
Hansen, G.
spellingShingle Vogler, C.
Brönnimann, S.
Hansen, G.
Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
author_facet Vogler, C.
Brönnimann, S.
Hansen, G.
author_sort Vogler, C.
title Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
title_short Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
title_full Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
title_fullStr Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
title_full_unstemmed Re-evaluation of the 1950–1962 total ozone record from Longyearbyen, Svalbard
title_sort re-evaluation of the 1950–1962 total ozone record from longyearbyen, svalbard
publishDate 2018
url https://doi.org/10.5194/acp-6-4763-2006
https://www.atmos-chem-phys.net/6/4763/2006/
geographic Longyearbyen
Norway
Svalbard
Tromsø
geographic_facet Longyearbyen
Norway
Svalbard
Tromsø
genre Longyearbyen
polar night
Svalbard
Tromsø
genre_facet Longyearbyen
polar night
Svalbard
Tromsø
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-6-4763-2006
https://www.atmos-chem-phys.net/6/4763/2006/
op_doi https://doi.org/10.5194/acp-6-4763-2006
container_title Atmospheric Chemistry and Physics
container_volume 6
container_issue 12
container_start_page 4763
op_container_end_page 4773
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