COMMENT ON AEROSOL EFFECT ON ANTARCTIC OZONE

The structure of the aerosol layer disturbed by a cold air was suggested from the lidar measurements at Syowa Station (69°00′S, 39°35′E). The particle layer containing sublayers of spherical or nonspherical aerosols was frequently observed in Antarctic spring. It is a point one sholud not ignore whe...

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Bibliographic Details
Main Authors: イワサカ ヤスノブ /, Yasunobu IWASAKA, Guang-Yu SHI
Format: Report
Language:English
Published: Water Research Institue, Nagoya University 1987
Subjects:
Antarctic
Syowa Station
Antarc*
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3519
http://id.nii.ac.jp/1291/00003519/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3519&item_no=1&attribute_id=18&file_no=1
Description
Summary:The structure of the aerosol layer disturbed by a cold air was suggested from the lidar measurements at Syowa Station (69°00′S, 39°35′E). The particle layer containing sublayers of spherical or nonspherical aerosols was frequently observed in Antarctic spring. It is a point one sholud not ignore when he discusses aerosol effects on "Antarctic ozone depletion" through radiative processes and heterogeneous chemical reactions.

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