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A hindcast of the Bohai Bay oil spill during June to August 2011 被引量:2

A hindcast of the Bohai Bay oil spill during June to August 2011
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摘要 An operational three-dimensional oil spill model is developed by the National Marine Environmental Forecasting Center(NMEFC), State Oceanic Administration, China, and the model has been running for 9 a. On June 4 and 17,2011, oil is spilled into the sea water from two separate oil platforms in the Bohai Bay, i.e., Platforms B and C of Penglai 19-3 oilfield. The spill causes pollution of thousands of square kilometres of sea area. The NMEFC’s oil spill model is employed to study the Penglai 19-3 oil-spill pollution during June to August 2011. The wind final analysis data of the NMEFC, which is based on a weather research and forecasting(WRF) model, are analyzed and corrected by comparing with the observation data. A corrected current filed is obtained by forcing the princeton ocean model(POM) with the corrected wind field. With the above marine environmental field forcing the oil spill model, the oil mass balance and oil distribution can be produced. The simulation is validated against the observation, and it is concluded that the oil spill model of the NMEFC is able to commendably simulate the oil spill distribution. Thus the NMEFC’s oil spill model can provide a tool in an environmental impact assessment after the event. An operational three-dimensional oil spill model is developed by the National Marine Environmental Forecasting Center(NMEFC), State Oceanic Administration, China, and the model has been running for 9 a. On June 4 and 17,2011, oil is spilled into the sea water from two separate oil platforms in the Bohai Bay, i.e., Platforms B and C of Penglai 19-3 oilfield. The spill causes pollution of thousands of square kilometres of sea area. The NMEFC’s oil spill model is employed to study the Penglai 19-3 oil-spill pollution during June to August 2011. The wind final analysis data of the NMEFC, which is based on a weather research and forecasting(WRF) model, are analyzed and corrected by comparing with the observation data. A corrected current filed is obtained by forcing the princeton ocean model(POM) with the corrected wind field. With the above marine environmental field forcing the oil spill model, the oil mass balance and oil distribution can be produced. The simulation is validated against the observation, and it is concluded that the oil spill model of the NMEFC is able to commendably simulate the oil spill distribution. Thus the NMEFC’s oil spill model can provide a tool in an environmental impact assessment after the event.
出处 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2017年第11期21-26,共6页 海洋学报(英文版)
基金 The Open Project Fund of the Key Laboratory of Shangdong Province for Marine Ecological Environment and Disaster Prevention and Mitigation of China under contract No.201402 the Project of the Key Laboratory of Marine Spill Oil Identification and Damage Assessment Technology,State Oceanic Administration of China under contract No.201604 the National Marine Public Welfare Research Project of China under contract No.201305031 the Cooperation on the Development of Basic Technologies for the Yellow Sea and East China Sea Operational Oceanographic System funded by the China-Korea Joint Ocean Research and the National Natural Science Foundation of China under contract Nos 41206106 and 41406042
关键词 oil spill HINDCAST Lagrangian random walk oil distribution swept area oil spill hindcast Lagrangian random walk oil distribution swept area
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  • 1刘钦政,张建华,刘煜,王旭,李燕,白珊,吴辉碇.渤海三维海洋温度和海流数值预报[J].海洋预报,2005,22(z1):27-34. 被引量:8
  • 2刘钦政,张存智,刘煜,李燕,白珊,张建华.渤海溢油数值预报研究[J].海洋预报,2005,22(z1):70-76. 被引量:18
  • 3[3]项目专家组,项目执行专家组.我国短期气候预测系统的研究(之二):短期气候预测业务动力模式的研制[M].北京:气象出版社,2000.
  • 4[4]LASG. User's Guide and Reference Manual for the Third Generation of IAP/LASG World Ocean General Circulation Model[M]. Beijing: State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics(LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, 1998.
  • 5[5]Blumberg A F, Mellor G L. A description of a three-dimensional coastal ocean circulation model [A]. In: Heaps, N (Ed).Three-Dimensional Coastal Ocean Models. American Geophysical Union, 1987, 208.
  • 6[6]Song Y, DHaidvogel. Asemi-implicit ocean circulation model using a generalized topography-following coordinate system[J]. J Comp Phys, 1994,115: 228~244.
  • 7[7]Mellor G L, Hakkinen S, Ezer T. A generalization of a sigma coordinate ocean model and an inter-comparison of model vertical grids[J]. In: Pinari, N (Ed). Ocean Forecasting: Theory and Practice. Springer, New York, 2000.
  • 8[8]Haidvogel D B, Arango H G, Hedstrom K S, Beckmann, A, Malanotte-Rizzoli P, Shcheptkin A F. Model evaluation experiments in the North Atlantic basin: simulations in nonlinear terrain-following coordinates [J]. Dynamics of Atmospheres and Oceans 2000, 32: 239~281.
  • 9[9]Chu P C, C W Fan. An accuracy progressive sixth-order finite difference scheme. Journal of Atmospheric and Oceanic Technology[J]. 2001, 18: 1245~1257.
  • 10[10]Thorndike A S, Rothrock D A, Maykut C A, Colony R. The thickness distribution of sea ice [J]. J Geophys Res, 1975,80:4501~4513.

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