Science China Earth Sciences

, Volume 56, Issue 8, pp 1447–1451

An ensemble estimation of impact times and strength of Fukushima nuclear pollution to the east coast of China and the west coast of America

Authors

    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • Wei Li
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • HongLi Fu
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • XueFeng Zhang
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • XiDong Wang
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • XinRong Wu
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
  • LianXin Zhang
    • Key Laboratory of Marine Environmental Information Technology, State Oceanic AdministrationNational Marine Data and Information Service
Research Paper

DOI: 10.1007/s11430-012-4520-2

Cite this article as:
Han, G., Li, W., Fu, H. et al. Sci. China Earth Sci. (2013) 56: 1447. doi:10.1007/s11430-012-4520-2

Abstract

Based on the statistics of all surface drifting buoys of 1978–2011 and Lagrangian tracers simulated from high quality ocean reanalysis currents, the impact times and strength of Fukushima nuclear pollution to the east coast of China and the west coast of America have been estimated. Under the circumstances of the radioactive pollutants drifting in the ocean surface, preliminary research results show that while the tracers took about 4 years to reach the west coast of USA, there are two types of tracers to carry out Fukushima nuclear pollutants to reach the east coast of China, corresponding to 1.5-year recirculation gyre transport and 3.5-year subtropical circulation transport. The distributions of the impact strength at these time scales are given according to the variation of relative number concentration with time combined with the decaying rate of radioactive matter. For example, starting from 1% at 1.5-year, of the initial level at the originating area of Fukushima nuclear pollution, the impact strength of Cesium-137 in the South China Sea continuously increases up to 3% by 4 years, while the impact strength of Cesium-137 in the west coast of America is as high as 4% due to the role of strong Kuroshio-extension currents as a major transport mechanism of nuclear pollutants for that area.

Keywords

Fukushima nuclear pollutionensemble estimationsurface drifting buoyocean reanalysisLagrangian tracer

Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2012