PRELIMINARY RESULTS FROM RADON OBSERVATION AT SYOWA STATION, ANTARCTICA, DURING 1996

P(論文) The concentration of ^<222>Rn in surface air was measured for the first time at Syowa Station, Antarctica in the period September 1996-January 1997 by an electrostatic collection method. The concentration of ^<222>Rn was higher in the first half than the latter half of the monitori...

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Bibliographic Details
Main Authors: ウイ, ヒロタカ, タサカ, シゲキ, ハヤシ, マサヒコ, オサダ, カズオ, イワサカ, ヤスノブ, UI, Hirotaka, TASAKA, Shigeki, HAYASHI, Masahiko, OSADA, Kazuo, IWASAKA, Yasunobu
Language:English
Published: National Institute of Polar Research 1998
Subjects:
Austral
Syowa Station
Antarc*
Antarctica
Polar meteorology and glaciology
Online Access:https://nipr.repo.nii.ac.jp/record/2873/files/KJ00002364383.pdf
https://doi.org/10.15094/00002873
https://nipr.repo.nii.ac.jp/records/2873
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Summary:P(論文) The concentration of ^<222>Rn in surface air was measured for the first time at Syowa Station, Antarctica in the period September 1996-January 1997 by an electrostatic collection method. The concentration of ^<222>Rn was higher in the first half than the latter half of the monitoring period. Daily mean ^<222>Rn concentration averaged 270mBq/m^3 for the first half of the period and 150mBq/m^3 for the latter half of the period. The maximum daily mean ^<222>Rn concentration was 630mBq/m^3,and the minimum concentration was 70mBq/m^3. The daily mean values were higher than those measurement in previous studies in Antarctica. Remarkable ^<222>Rn concentration increases (radon storms), which accompanied cyclones, were observed twice during the austral spring at Syowa Station. The first radon storm occurred on 18-21 September and the second on 16-20 October 1996. The daily mean ^<222>Rn concentrations in the first and second radon storms attained 530mBq/m^3 and 630mBq/m^3 respectively. On the other hand, the hourly mean ^<222>Rn concentration attained 1200mBq/m^3 in the second event. This implies that the ^<222>Rn concentrations vary on a short time scale. The main feature of the ^<222>Rn concentration record corresponds to intense mixing of air masses from mid-latitude continents to Antarctica. This implies that the variations of ^<222>Rn may be related to the wind direction. The concentrations of ^<222>Rn seem to increase with southerly wind and decrease with northerly or northeasterly wind. departmental bulletin paper

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