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Seasonal and spatial variation of atmospheric ^2^1^0Pb and ^7Be deposition: features of the Japan Sea side of Japan [An article from: Journal of Environmental Radioactivity]
Book Details
PublisherElsevier
ISBN / ASINB000RR7BE4
ISBN-13978B000RR7BE1
AvailabilityAvailable for download now
Sales Rank99,999,999
MarketplaceUnited States 🇺🇸
Description
This digital document is a journal article from Journal of Environmental Radioactivity, published by Elsevier in . The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
Monthly depositional fluxes of ^2^1^0Pb and ^7Be at Tatsunokuchi, Japan which faces the Japan Sea were studied over a 12-year period from 1991 to 2002. The data were compared with the spatial variability of these fluxes at Taejon in Korea and at 11 other sites in Japan from Ishigaki of the southern islands of Okinawa to Wakkanai of the northern end of Hokkaido over a 2-year period from 2000 to 2001. The monthly depositions of both ^2^1^0Pb and ^7Be at Tatsunokuchi revealed very similar seasonal variations with a single peak; both depositions were high in winter and low in summer. This phenomenon was found to be not transient but stationary. The deposition of these nuclides was much greater on the Japan Sea side of Japan than on the Pacific Ocean side. The cause for high deposition of ^2^1^0Pb and ^7Be in winter might be explained by a combination of a series of the following processes: blowing out of air masses with a high ^2^1^0Pb concentration near the surface layer over the continent by strong winter monsoons, additional flow of cold air masses with high ^7Be concentration at high latitude, well-mixing with generation of ascending current and convection clouds over the Japan Sea, and heavy snowfalls accompanying them.
Description:
Monthly depositional fluxes of ^2^1^0Pb and ^7Be at Tatsunokuchi, Japan which faces the Japan Sea were studied over a 12-year period from 1991 to 2002. The data were compared with the spatial variability of these fluxes at Taejon in Korea and at 11 other sites in Japan from Ishigaki of the southern islands of Okinawa to Wakkanai of the northern end of Hokkaido over a 2-year period from 2000 to 2001. The monthly depositions of both ^2^1^0Pb and ^7Be at Tatsunokuchi revealed very similar seasonal variations with a single peak; both depositions were high in winter and low in summer. This phenomenon was found to be not transient but stationary. The deposition of these nuclides was much greater on the Japan Sea side of Japan than on the Pacific Ocean side. The cause for high deposition of ^2^1^0Pb and ^7Be in winter might be explained by a combination of a series of the following processes: blowing out of air masses with a high ^2^1^0Pb concentration near the surface layer over the continent by strong winter monsoons, additional flow of cold air masses with high ^7Be concentration at high latitude, well-mixing with generation of ascending current and convection clouds over the Japan Sea, and heavy snowfalls accompanying them.
