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Exponential time differencing for the tracer equations appearing in primitive equation ocean models

机译:原始方程海洋模型中出现的示踪方程的指数时间差异

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The tracer equations are part of the primitive equations used in ocean modeling and describe the transport of tracers, such as temperature, salinity or chemicals, in the ocean. Depending on the number of tracers considered, several equations may be added to and coupled to the dynamics system. In many relevant situations, the time-step requirements of explicit methods imposed by the transport and mixing in the vertical direction are more restrictive than those for the horizontal, and this may cause the need to use very small time steps if a fully explicit method is employed. To overcome this issue, we propose an exponential time differencing (ETD) solver where the vertical terms (transport and diffusion) are treated with a matrix exponential, whereas the horizontal terms are dealt with in an explicit way. We investigate numerically the computational speed-ups that can be obtained over other semi-implicit methods, and we analyze the advantages of the method in the case of multiple tracers. (C) 2020 Elsevier B.V. All rights reserved.
机译:示踪方程是海洋建模中使用的原始方程的一部分,并描述了海洋中的示踪剂的运输,例如温度,盐度或化学物质。取决于所考虑的示踪器的数量,可以添加若干方程并耦合到动态系统。在许多相关情况中,传输和混合在垂直方向上施加的显式方法的时间步骤要求比水平的更严格,这可能导致需要使用非常小的时间步骤如果是完全显式的方法是雇用。为了克服这个问题,我们提出了一种指数时间差异(ETD)求解器,其中垂直术语(传送和扩散)用矩阵指数处理,而水平术语以明确的方式处理。我们在数字上调查,可以通过其他半隐式方法获得的计算速度,并且我们在多个示踪剂的情况下分析该方法的优点。 (c)2020 Elsevier B.v.保留所有权利。

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