Particle-tracking simulation for the drift/diffusion of spilled oils in the Sea of Okhotsk with a three-dimensional, high-resolution model
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  • 作者:Jun Ono (1) (2)
    Kay I. Ohshima (3)
    Keisuke Uchimoto (4)
    Naoto Ebuchi (3)
    Humio Mitsudera (3)
    Hajime Yamaguchi (1)
  • 关键词:Sea of Okhotsk ; East Sakhalin Current ; Soya Warm Current ; Spilled oil ; Particle ; tracking experiment
  • 刊名:Journal of Oceanography
  • 出版年:2013
  • 出版时间:August 2013
  • 年:2013
  • 卷:69
  • 期:4
  • 页码:413-428
  • 全文大小:1527KB
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  • 作者单位:Jun Ono (1) (2)
    Kay I. Ohshima (3)
    Keisuke Uchimoto (4)
    Naoto Ebuchi (3)
    Humio Mitsudera (3)
    Hajime Yamaguchi (1)

    1. Graduate School of Frontier Sciences, The University of Tokyo, Kashiwanoha 5-1-5, Kashiwa, Chiba, 277-8561, Japan
    2. National Institute of Polar Research, Tachikawa, Tokyo, Japan
    3. Institute of Low Temperature Science, Hokkaido University, Sapporo, Hokkaido, Japan
    4. Research Institute of Innovative Technology for the Earth, Kizugawa, Kyoto, Japan
文摘
To conduct the simulation of oil spills in the Sea of Okhotsk, we developed a three-dimensional, high-resolution ocean circulation model. The model particularly improved the reproducibility of velocity field during the strong stratification period. Particle-tracking experiments with the effects of evaporation and biodegradation were performed using the combined data of daily ocean currents from the present model and the hourly diurnal tidal currents from the tidal model. The results are shown by the relative concentration of the particles averaged over the 8?years of 1998-005 based on the ensemble forecast idea. For the case of particles released from the Sakhalin II oil field, the particles deployed in September–January are carried southward by the East Sakhalin Current, finally arriving at the Hokkaido coast, after 60-0 days. The particles deployed in March–August are diffused offshore by the synoptic wind drift, and hardly transported to regions south of Sakhalin. For the case of particles released from the region off Prigorodnoye, the oil export terminal, after the diffusion by the synoptic wind drift, a part of them are carried offshore of Hokkaido by the Soya Warm Current. The particles released in November–April flow out to the Japan Sea through the Soya Strait, mainly by the synoptic wind drift and secondly by the diffusion due to strong tidal currents around the Soya Strait. By considering the effects of evaporation and biodegradation, the relative concentration of the particles is considerably decreased before arriving at the Hokkaido coast, particularly in the case of drift from the Sakhalin II oil field.

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