lida, T.

Matsuda, M.

Moriizumi, J.

Yamazawa, H.

It was shown by a series of observations of wet deposition of radon decay products at Nagoya, Japan that extremely high deposition rate events were associated with convective precipitation under presence of continental air mass aloft. Atmospheric transport simulations showed that the high deposition rate events were caused by continental radon transported within a relatively thin layer from 1 to 3 km above sea level

Wet Deposition of Radon Decay Products and its Relation with Long-Range Transported Radon

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