Observations of total ozone amounts and lower stratospheric temperatures during a stratospheric sudden warming in the Antarctic by TOVS of NOAA-7

A comparison of total ozone amounts and lower stratospheric temperature during the 1982 stratospheric sudden warming in the Antarctic is made by the TIROS Operational Vertical Sounder (TOVS) data of NOAA-7 received at Syowa Station. A method assuming a vertical ozone profile is applied to obtain tot...

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Bibliographic Details
Main Authors: Kazuya Suzuki, Takashi Yamanouchi, Takeo Yoshino, Sadao Kawaguchi
Format: Report
Language:English
Published: University of Electro-Communications/National Institute of Polar Research/University of Electro-Communications/National Institute of Polar Research 1985
Subjects:
Antarctic
Syowa Station
The Antarctic
Antarc*
Memoirs of National Institute of Polar Research
Polar Research
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1832
http://id.nii.ac.jp/1291/00001832/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1832&item_no=1&attribute_id=18&file_no=1
Description
Summary:A comparison of total ozone amounts and lower stratospheric temperature during the 1982 stratospheric sudden warming in the Antarctic is made by the TIROS Operational Vertical Sounder (TOVS) data of NOAA-7 received at Syowa Station. A method assuming a vertical ozone profile is applied to obtain total ozone amounts. The total ozone can be determined independently of the surface measurements. A good agreement between the total ozone amounts derived from satellite data and those of Dobson measurements is seen at Syowa Station. RMS error is 12 DU ((10)^<-3>・atm・cm). A good correlation between the total ozone and the lower stratospheric temperature is observed in the Antarctic. Patterns similar to the wave number 5 structure of the total ozone during the Southern Hemisphere summer are seen during the 1982 sudden warming.

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