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Backward Calculation Based on the Advection and Diffusion of Oil Spills on the Sea Surface
作者姓名:刘浩  尹宝树  林建国
作者单位:Open Laboratory of Circulations and Waves,Institute of Oceanology,CAS,Qingdao 266071,Shandong,ChinaG raduate School,CAS,Beijing,100039,China,Open Laboratory of Circulations and Waves,Institute of Oceanology,CAS,Qingdao 266071,Shandong,China,College of Environmental Science and Engineering,Dalian Maritime University,Dalian 116026,Liaoning,China
基金项目:so their help is greatly appreciated in addition,国家科技攻关项目
摘    要:Advection and diffusion equation is an effective means of investigating the motional state of oil spills. Common study is based on the known initial and boundary conditions to calculate the equation onwards. Unlike previous works, in this paper we focus on backward calculating advection and diffusion equation, namely, starting computation from the moment when the oil spill is found back to the moment when the incident occurs. Through such a simulation, we hope to trace the track of oil spills …

关 键 词:反馈计算  水平对流扩散  数值耗散  石油污染  海难溢油事故

Backward Calculation Based on the Advection and Diffusion of Oil Spills on the Sea Surface
LIU Hao,YIN Baoshu,Lin Jianguo.Backward Calculation Based on the Advection and Diffusion of Oil Spills on the Sea Surface[J].Marina Science Bulletin,2005,7(1):63-68.
Authors:LIU Hao  YIN Baoshu  Lin Jianguo
Institution:1. Open Laboratory of Circulations and Waves, Institute of Oceanology, CAS, Qingdao 266071, Shandong, China;Graduate School, CAS, Beijing, 100039, China
2. Open Laboratory of Circulations and Waves, Institute of Oceanology, CAS, Qingdao 266071, Shandong, China
3. College of Environmental Science and Engineering, Dalian Maritime University, Dalian 116026, Liaoning, China
Abstract:In the light of the problem of oil pollution brought about by ships, in this paper we present the concept of backward tracing oil spills. In the course of backward calculation of the two-dimensional convection & diffusion equation, on the one hand, the advection term itself has the strong unilateral property, which means information in the upper reaches is transmitted downstream via the advection term; on the other hand, because of the opposite direction of calculation, it is essential for information to be conveyed upstream by means of the advection term. In addition, unlike that in the forward calculation, the diffusion term in the backward calculation is prone to accumulate errors, and thus renders the whole scheme unstable. Therefore, we adopt the central difference to deal with both the convectional term and the diffusion term. By examining two practical examples (1) under the unlimited boundary condition, and (2) under the limited boundary condition, it is proven that this method could achieve fundamentally satisfactory results not only in the open ocean but also in the closed or semi-closed bay.
Keywords:Backward calculation  advection-diffusion  n umerical dissipation
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