Variability of aerosol extinction of solar radiation in Antarctica

Temporal variations of the aerosol optical depth and transmission coefficient of the atmosphere are considered using data from Mirny Observatory, Antarctica. Year-to-year variability of these parameters is determined mainly by stratospheric aerosol pollution due to volcanic activity. A considerable...

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Published in:Antarctic Science
Main Author: Radionov, V. F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102094000635
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102094000635
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spelling crcambridgeupr:10.1017/s0954102094000635 2024-03-03T08:38:59+00:00 Variability of aerosol extinction of solar radiation in Antarctica Radionov, V. F. 1994 http://dx.doi.org/10.1017/s0954102094000635 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102094000635 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 6, issue 3, page 419-424 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0954102094000635 2024-02-08T08:26:21Z Temporal variations of the aerosol optical depth and transmission coefficient of the atmosphere are considered using data from Mirny Observatory, Antarctica. Year-to-year variability of these parameters is determined mainly by stratospheric aerosol pollution due to volcanic activity. A considerable increase of atmospheric turbidity has been observed since the end of September 1991. This phenomenon seems to be associated with the Mount Pinatubo volcanic eruption. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Cambridge University Press Mirny ENVELOPE(93.009,93.009,-66.553,-66.553) Antarctic Science 6 3 419 424
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Radionov, V. F.
Variability of aerosol extinction of solar radiation in Antarctica
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Temporal variations of the aerosol optical depth and transmission coefficient of the atmosphere are considered using data from Mirny Observatory, Antarctica. Year-to-year variability of these parameters is determined mainly by stratospheric aerosol pollution due to volcanic activity. A considerable increase of atmospheric turbidity has been observed since the end of September 1991. This phenomenon seems to be associated with the Mount Pinatubo volcanic eruption.
format Article in Journal/Newspaper
author Radionov, V. F.
author_facet Radionov, V. F.
author_sort Radionov, V. F.
title Variability of aerosol extinction of solar radiation in Antarctica
title_short Variability of aerosol extinction of solar radiation in Antarctica
title_full Variability of aerosol extinction of solar radiation in Antarctica
title_fullStr Variability of aerosol extinction of solar radiation in Antarctica
title_full_unstemmed Variability of aerosol extinction of solar radiation in Antarctica
title_sort variability of aerosol extinction of solar radiation in antarctica
publisher Cambridge University Press (CUP)
publishDate 1994
url http://dx.doi.org/10.1017/s0954102094000635
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102094000635
long_lat ENVELOPE(93.009,93.009,-66.553,-66.553)
geographic Mirny
geographic_facet Mirny
genre Antarc*
Antarctic Science
Antarctica
genre_facet Antarc*
Antarctic Science
Antarctica
op_source Antarctic Science
volume 6, issue 3, page 419-424
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102094000635
container_title Antarctic Science
container_volume 6
container_issue 3
container_start_page 419
op_container_end_page 424
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