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involves choosing critical parameters and submitting batch jobs, which might not begin running for hours or days. The data files must then be returned to the user’s workstation for analysis and plotting. Typically, only a few such parameter variation runs are made, resulting in model output not completely representative of the behavior of a given region. In(More)
Visualization of computational oceanography is traditionally a post-processing step. This batch orientation is clumsy if one wants to observe the effect of a wide range of parameters on the solution. This paper describes the conversion of an ocean circulation model from this traditional design to an interactive program in which the computed solution is(More)
Visualization of computational oceanography is traditionally a post-processing step. This batch orientation is clumsy if one wants to observe the effect of a wide range of parameters on the solution. This paper describes the conversion of an ocean circulation model from this traditional design to an interactive program in which the computed solution is(More)
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