GIANT PARTICLES IN THE LOWER STRATOSPHERE

Polar stratospheric clouds (PSCs) are well known phenomena in the lower polar stratosphere. Using the data of balloon flights at McMurdo Station, Antarctica, D. J. HOFMANN et al. (J. Geophys. Res., 93,665,1988) and D. J. HOFMANN (Nature, 337,447,1989) have recently showed vertical profiles of aeroso...

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Main Authors: ワダ マコト, Makoto WADA
Format: Report
Language:English
Published: ABSTRACT 1991
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003654 2023-05-15T13:49:01+02:00 GIANT PARTICLES IN THE LOWER STRATOSPHERE ワダ マコト Makoto WADA 1991-05 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3654 http://id.nii.ac.jp/1291/00003654/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3654&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3654 http://id.nii.ac.jp/1291/00003654/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 4, 121-122(1991-05) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3654&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1991 ftnipr 2022-12-10T19:45:46Z Polar stratospheric clouds (PSCs) are well known phenomena in the lower polar stratosphere. Using the data of balloon flights at McMurdo Station, Antarctica, D. J. HOFMANN et al. (J. Geophys. Res., 93,665,1988) and D. J. HOFMANN (Nature, 337,447,1989) have recently showed vertical profiles of aerosol above the altitude of 10km. The upper limit of the particle size of their measurements was less than about 1μm. We present here the results of balloon observations for measuring relatively large particles (more than 10μm) in the lower stratosphere. The sounding instrument of particles was similar in design to that described by M. MURAKAMI et al. (J. Meteorol. Soc. Jpn., 65,803,1987) called Cloud Particle Video Sonde (CPVS), whose main device was a TV camera. Four balloon flights for sounding stratospheric particles were carried out on May 28,August 5,August 20 and September 2 in 1988 at Syowa Station (69°S, 40°E), Antarctica. Giant particles which look like liquid particles were found on pictures transmitted from the TV camera ascending with the balloon. The size of the largest one was about 150μm diameter. Particles of more than 100μm diameter were found every flight in the lower stratosphere. There is a possibility that the film does not show liquid particles, but non-uniformity of the surface of the film itself, because CPVS uses water-repellent film for collecting particles and the coating was probably not uniform on the film surface. An attempt to check this point is being carried out. Report Antarc* Antarctica E. Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Hofmann ENVELOPE(160.600,160.600,-82.667,-82.667) McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850) Syowa Station
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description Polar stratospheric clouds (PSCs) are well known phenomena in the lower polar stratosphere. Using the data of balloon flights at McMurdo Station, Antarctica, D. J. HOFMANN et al. (J. Geophys. Res., 93,665,1988) and D. J. HOFMANN (Nature, 337,447,1989) have recently showed vertical profiles of aerosol above the altitude of 10km. The upper limit of the particle size of their measurements was less than about 1μm. We present here the results of balloon observations for measuring relatively large particles (more than 10μm) in the lower stratosphere. The sounding instrument of particles was similar in design to that described by M. MURAKAMI et al. (J. Meteorol. Soc. Jpn., 65,803,1987) called Cloud Particle Video Sonde (CPVS), whose main device was a TV camera. Four balloon flights for sounding stratospheric particles were carried out on May 28,August 5,August 20 and September 2 in 1988 at Syowa Station (69°S, 40°E), Antarctica. Giant particles which look like liquid particles were found on pictures transmitted from the TV camera ascending with the balloon. The size of the largest one was about 150μm diameter. Particles of more than 100μm diameter were found every flight in the lower stratosphere. There is a possibility that the film does not show liquid particles, but non-uniformity of the surface of the film itself, because CPVS uses water-repellent film for collecting particles and the coating was probably not uniform on the film surface. An attempt to check this point is being carried out.
format Report
author ワダ マコト
Makoto WADA
spellingShingle ワダ マコト
Makoto WADA
GIANT PARTICLES IN THE LOWER STRATOSPHERE
author_facet ワダ マコト
Makoto WADA
author_sort ワダ マコト
title GIANT PARTICLES IN THE LOWER STRATOSPHERE
title_short GIANT PARTICLES IN THE LOWER STRATOSPHERE
title_full GIANT PARTICLES IN THE LOWER STRATOSPHERE
title_fullStr GIANT PARTICLES IN THE LOWER STRATOSPHERE
title_full_unstemmed GIANT PARTICLES IN THE LOWER STRATOSPHERE
title_sort giant particles in the lower stratosphere
publisher ABSTRACT
publishDate 1991
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3654
http://id.nii.ac.jp/1291/00003654/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3654&item_no=1&attribute_id=18&file_no=1
long_lat ENVELOPE(160.600,160.600,-82.667,-82.667)
ENVELOPE(166.667,166.667,-77.850,-77.850)
geographic Hofmann
McMurdo Station
Syowa Station
geographic_facet Hofmann
McMurdo Station
Syowa Station
genre Antarc*
Antarctica
E. Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Antarc*
Antarctica
E. Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3654
http://id.nii.ac.jp/1291/00003654/
AA10756213
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 4, 121-122(1991-05)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3654&item_no=1&attribute_id=18&file_no=1
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