Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)

Total ozone data obtained with a Dobson instrument at Syowa Station are compared with Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) version 6 data for 1979 through March 1988. Generally speaking TOMS data show larger values of a few percent compared with Dobson data. Monthly averaged differences...

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Main Author: Kazuo Shibasaki
Format: Report
Language:English
Published: Kokugakuin University 1993
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3798
http://id.nii.ac.jp/1291/00003798/
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003798 2023-05-15T18:02:11+02:00 Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract) Kazuo Shibasaki 1993-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3798 http://id.nii.ac.jp/1291/00003798/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3798&item_no=1&attribute_id=18&file_no=1 en eng Kokugakuin University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3798 http://id.nii.ac.jp/1291/00003798/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 7, 105(1993-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3798&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1993 ftnipr 2022-12-17T19:45:54Z Total ozone data obtained with a Dobson instrument at Syowa Station are compared with Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) version 6 data for 1979 through March 1988. Generally speaking TOMS data show larger values of a few percent compared with Dobson data. Monthly averaged differences demonstrate a clear seasonal variation of summer maximum. This behavior was the same as my previous work in which Dobson data were compared with TOMS version 5 data over Syowa Station. My previous work also revealed a long term trend of difference due to TOMS version 5 data which have been affected by the deterioration of the diffuser plate attached to the TOMS instrument. No such long term trend is recognized in the present result which shows the superiority of the new calibration method adopted in the TOMS version 6 data analysis. However, the clear seasonal variation of difference between Dobson total ozone data and new version of TOMS data suggests a problem which may inherently exist in the TOMS data or Dobson data. This problem should be further examined. As for absolute value, as mentioned above, mean TOMS version 6 data are larger than Dobson data by several percent. This difference is larger than that of TOMS version 5. Report Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Syowa Station
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description Total ozone data obtained with a Dobson instrument at Syowa Station are compared with Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) version 6 data for 1979 through March 1988. Generally speaking TOMS data show larger values of a few percent compared with Dobson data. Monthly averaged differences demonstrate a clear seasonal variation of summer maximum. This behavior was the same as my previous work in which Dobson data were compared with TOMS version 5 data over Syowa Station. My previous work also revealed a long term trend of difference due to TOMS version 5 data which have been affected by the deterioration of the diffuser plate attached to the TOMS instrument. No such long term trend is recognized in the present result which shows the superiority of the new calibration method adopted in the TOMS version 6 data analysis. However, the clear seasonal variation of difference between Dobson total ozone data and new version of TOMS data suggests a problem which may inherently exist in the TOMS data or Dobson data. This problem should be further examined. As for absolute value, as mentioned above, mean TOMS version 6 data are larger than Dobson data by several percent. This difference is larger than that of TOMS version 5.
format Report
author Kazuo Shibasaki
spellingShingle Kazuo Shibasaki
Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
author_facet Kazuo Shibasaki
author_sort Kazuo Shibasaki
title Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
title_short Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
title_full Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
title_fullStr Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
title_full_unstemmed Comparison of total ozone over Syowa Station between NIMBUS 7 TOMS version 6 data and Dobson data (abstract)
title_sort comparison of total ozone over syowa station between nimbus 7 toms version 6 data and dobson data (abstract)
publisher Kokugakuin University
publishDate 1993
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3798
http://id.nii.ac.jp/1291/00003798/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3798&item_no=1&attribute_id=18&file_no=1
geographic Syowa Station
geographic_facet Syowa Station
genre Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3798
http://id.nii.ac.jp/1291/00003798/
AA10756213
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 7, 105(1993-09)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3798&item_no=1&attribute_id=18&file_no=1
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