RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES

P(論文) Recent interannual changes of zonal mean temperatures of mid and high latitudes in the lower and middle stratosphere are investigated for the period from 1980 to 1986 with the use of TIROSN and NOAA series satellite data (50-10 mb) and NMC data (300-50 mb). The zonal mean temperatures of the S...

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Main Authors: ヒロオカ, トシヒコ, カワヒラ, コウジ, HIROOKA, Toshihiko, KAWAHIRA, Kohji
Language:English
Published: National Institute of Polar Research 1991
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3652/files/KJ00000767855.pdf
https://doi.org/10.15094/00003652
https://nipr.repo.nii.ac.jp/records/3652
_version_ 1829314278679642112
author ヒロオカ, トシヒコ
カワヒラ, コウジ
HIROOKA, Toshihiko
KAWAHIRA, Kohji
author_facet ヒロオカ, トシヒコ
カワヒラ, コウジ
HIROOKA, Toshihiko
KAWAHIRA, Kohji
author_sort ヒロオカ, トシヒコ
collection National Institute of Polar Research Repository, Japan
description P(論文) Recent interannual changes of zonal mean temperatures of mid and high latitudes in the lower and middle stratosphere are investigated for the period from 1980 to 1986 with the use of TIROSN and NOAA series satellite data (50-10 mb) and NMC data (300-50 mb). The zonal mean temperatures of the Southern Hemisphere lower stratosphere (300-50 mb layer) decrease in all seasons as already shown (K. KAWAHIRA and T. HIROOKA : Geophys. Res. Lett., 16,41,1989). Those of the Northern Hemisphere lower stratosphere also decrease in all seasons, although it is relatively difficult to discern such cooling in winter because of the irregular occurrence of stratospheric sudden warmings; in that case, the temperatures increase in higher latitudes while decreasing in lower latitudes. On the other hand, as for the middle stratosphere (50-10 mb layer), an increase of zonal mean temperature can be seen only in the Southern Hemisphere winter. In other seasons of the middle stratosphere of both hemispheres, significant interannual temperature changes cannot be seen from the current short analysis period. These trends found in the temperature field seem to be associated with interannual changes of general circulation of the stratosphere. Therefore, further observations of other dynamical quantities are needed in order to thoroughly understand the recent changes of stratospheric temperatures. departmental bulletin paper
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
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003652
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
4
120
AA10756213
https://nipr.repo.nii.ac.jp/record/3652/files/KJ00000767855.pdf
https://doi.org/10.15094/00003652
https://nipr.repo.nii.ac.jp/records/3652
publishDate 1991
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003652 2025-04-13T14:25:53+00:00 RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES ヒロオカ, トシヒコ カワヒラ, コウジ HIROOKA, Toshihiko KAWAHIRA, Kohji 1991-05 application/pdf https://nipr.repo.nii.ac.jp/record/3652/files/KJ00000767855.pdf https://doi.org/10.15094/00003652 https://nipr.repo.nii.ac.jp/records/3652 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 4 120 AA10756213 https://nipr.repo.nii.ac.jp/record/3652/files/KJ00000767855.pdf https://doi.org/10.15094/00003652 https://nipr.repo.nii.ac.jp/records/3652 1991 ftnipr https://doi.org/10.15094/00003652 2025-03-19T10:19:56Z P(論文) Recent interannual changes of zonal mean temperatures of mid and high latitudes in the lower and middle stratosphere are investigated for the period from 1980 to 1986 with the use of TIROSN and NOAA series satellite data (50-10 mb) and NMC data (300-50 mb). The zonal mean temperatures of the Southern Hemisphere lower stratosphere (300-50 mb layer) decrease in all seasons as already shown (K. KAWAHIRA and T. HIROOKA : Geophys. Res. Lett., 16,41,1989). Those of the Northern Hemisphere lower stratosphere also decrease in all seasons, although it is relatively difficult to discern such cooling in winter because of the irregular occurrence of stratospheric sudden warmings; in that case, the temperatures increase in higher latitudes while decreasing in lower latitudes. On the other hand, as for the middle stratosphere (50-10 mb layer), an increase of zonal mean temperature can be seen only in the Southern Hemisphere winter. In other seasons of the middle stratosphere of both hemispheres, significant interannual temperature changes cannot be seen from the current short analysis period. These trends found in the temperature field seem to be associated with interannual changes of general circulation of the stratosphere. Therefore, further observations of other dynamical quantities are needed in order to thoroughly understand the recent changes of stratospheric temperatures. departmental bulletin paper Other/Unknown Material Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan
spellingShingle ヒロオカ, トシヒコ
カワヒラ, コウジ
HIROOKA, Toshihiko
KAWAHIRA, Kohji
RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title_full RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title_fullStr RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title_full_unstemmed RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title_short RECENT INTERANNUAL CHANGES OF STRATOSPHERIC TEMPERATURES
title_sort recent interannual changes of stratospheric temperatures
url https://nipr.repo.nii.ac.jp/record/3652/files/KJ00000767855.pdf
https://doi.org/10.15094/00003652
https://nipr.repo.nii.ac.jp/records/3652