134Cs and 137Cs in the North Pacific Ocean derived from the March 2011 TEPCO Fukushima Dai-ichi Nuclear Power Plant accident, Japan. Part one: surface pathway and vertical distributions

Author:

Aoyama Michio,Hamajima Yasunori,Hult Mikael,Uematsu Mitsuo,Oka Eitarou,Tsumune Daisuke,Kumamoto Yuichiro

Funder

Houshanou-chousa-kenkyuhi, MEXT

J-RAPID, Japan Science and Technology Agency

Publisher

Springer Science and Business Media LLC

Subject

Oceanography

Reference45 articles.

1. Aoyama M, Hirose K (1995) The temporal and spatial variation of 137Cs concentration in the western North Pacific and its marginal seas during the period from 1979 to 1988. J Environ Radioact 29:57–74. doi: 10.1016/0265-931X(94)00050-7

2. Aoyama M, Hirose K (2004) Artificial radionuclides database in the Pacific Ocean: HAM database. Sci World J 4:200–215. doi: 10.1100/tsw.2004.15

3. Aoyama M, Hirose K (2008) Radiometric determination of anthropogenic radionuclides in seawater. In: Pavel PP (ed) Radioactivity in the environment. Elsevier, Oxford, pp 137–162. doi: 10.1016/S1569-4860(07)11004-4

4. Aoyama M, Hirose K, Nemoto K et al (2008) Water masses labeled with global fallout 137Cs formed by subduction in the North Pacific. Geophys Res Lett 35:L01604. doi: 10.1029/2007GL031964

5. Aoyama M, Fukasawa M, Hirose et al (2011) Cross equator transport of 137Cs from North Pacific Ocean to South Pacific Ocean (BEAGLE2003 cruises). Prog Oceanogr 89:7–16. doi: 10.1016/j.pocean.2010.12.003

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