Spatiotemporal variations in vertical profiles of Fukushima-derived 137Cs in the Kuroshio-Oyashio confluence region from 2011 to 2018: Implications for local water mass dynamics and basin-scale circulations-Reference-Cited by-同舟云学术

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Spatiotemporal variations in vertical profiles of Fukushima-derived 137Cs in the Kuroshio-Oyashio confluence region from 2011 to 2018: Implications for local water mass dynamics and basin-scale circulations

Published:2024-11 Issue: Volume:228 Page:103321
ISSN:0079-6611
Container-title:Progress in Oceanography
language:en
Short-container-title:Progress in Oceanography

Author:

Zhang Fule^ORCID,Huang Dekun^ORCID,Xu Yunping^ORCID,Huang Jiang,Du Jinzhou,Yu Tao

Funder

China Postdoctoral Science Foundation

Publisher

Elsevier BV

Reference71 articles.

1. Different responses of plankton community to mesoscale eddies in the western equatorial Pacific Ocean;An;Deep-Sea Research Part I,2024

2. Water masses labeled with global fallout 137Cs formed by subduction in the North Pacific;Aoyama;Geophys. Res. Lett.,2008

3. Cross equator transport of 137Cs from North Pacific Ocean to South Pacific Ocean (BEAGLE2003 cruises);Aoyama;Prog. Oceanogr.,2011

4. Surface pathway of radioactive plume of TEPCO Fukushima NPP1 released 134Cs and 137Cs;Aoyama;Biogeosciences,2013

5. 134Cs and 137Cs in the North Pacific Ocean derived from the March 2011 TEPCO Fukushima Dai-ichi Nuclear Power Plant accident, Japan. Part two: estimation of 134Cs and 137Cs inventories in the North Pacific Ocean;Aoyama;J. Oceanogr.,2016

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