The diurnal change in the vertical distribution of atmospheric 222Rn due to the growth and rise of the stable stratification height in the atmospheric boundary layer-Reference-Cited by-同舟云学术

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The diurnal change in the vertical distribution of atmospheric 222Rn due to the growth and rise of the stable stratification height in the atmospheric boundary layer

Published:2005 Issue: Volume: Page:489-496
ISSN:1569-4860
Container-title:Radioactivity in the Environment
language:
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Author:

Yoshioka K.,Iida T.

Publisher

Elsevier

Reference9 articles.

1. Variation of radon and thoron concentrations in relation to the wind speed;Ikebe;J. Meteorol. Soc. Jpn.,1970

2. Influence of solar radiation and heat emission on radon-222 daughter concentrations in surface air;Fujinami;J. Geophys. Res.,1988

3. The vertical profile of 222Rn concentration in the lower atmospheric boundary layer at Shimane peninsula;Yoshioka,1998

4. Science of Atmospheric Convection;Asai,1983

5. Science of Atmospheric Boundary Layer;Kondo,1982

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Radionuclide Behaviour and Transport in the Tropical Atmospheric Environment;Radioactivity in the Environment;2012

2. Continuous Observation of Atmospheric222Rn Concentrations for Analytic Basis of Atmospheric Transport in East Asia;Journal of Nuclear Science and Technology;2008-09

3. Seasonal Variation in Radon Concentration in the Atmosphere Simultaneously Measured in Donghae on Korean Peninsula, Matsue on Shimane Peninsula, and Oki Island in the Sea of Japan;Journal of Nuclear Science and Technology;2008-06

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