Stratospheric clouds and ozone depletion in the Arctic during January 1989

The role of stratospheric clouds in springtime polar ozone depletion has been recognized in the Antarctic but not, to date, in the Arctic. Measurements made from two instrumented balloons in January 1989 have been used to establish both the appearance of Arctic stratospheric clouds and the signature...

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Veröffentlicht in:Nature (London) 1989-07, Vol.340 (6229), p.117-121
Hauptverfasser: Hofmann, D. J, Deshler, T. L, Aimedieu, P, Matthews, W. A, Johnston, P. V, Kondo, Y, Sheldon, W. R, Byrne, G. J, Benbrook, J. R
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container_end_page 121
container_issue 6229
container_start_page 117
container_title Nature (London)
container_volume 340
creator Hofmann, D. J
Deshler, T. L
Aimedieu, P
Matthews, W. A
Johnston, P. V
Kondo, Y
Sheldon, W. R
Byrne, G. J
Benbrook, J. R
description The role of stratospheric clouds in springtime polar ozone depletion has been recognized in the Antarctic but not, to date, in the Arctic. Measurements made from two instrumented balloons in January 1989 have been used to establish both the appearance of Arctic stratospheric clouds and the signature of the onset of O sub(3) depletion at or around the altitude of these clouds. Comparison of the O sub(3) profile in the region of the clouds with those obtained during the past three austral spring seasons at McMurdo Station in Antarctica suggests the beginning of O sub(3) depletion at a height of 22-26 km.
doi_str_mv 10.1038/340117a0
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source Nature; Alma/SFX Local Collection
subjects Atmospheric composition. Chemical and photochemical reactions
Earth, ocean, space
Exact sciences and technology
External geophysics
Ocean, Atmosphere
Physics of the high neutral atmosphere
Sciences of the Universe
title Stratospheric clouds and ozone depletion in the Arctic during January 1989
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