A Design Method for Parallel Framework of Ocean Numerical Models
A numerical model and design method technology, applied in the direction of calculation, electrical digital data processing, special data processing applications, etc., can solve problems such as difficult development, achieve the effect of reducing calculation time, improving calculation efficiency and timeliness
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Embodiment 1
[0067] Parallelization of 2D Tidal Waves with Assimilated Numerical Models
[0068] In this embodiment, a two-dimensional tidal wave accompanying assimilation numerical model is used to simulate the tide of the Bohai-Yellow Sea. The determination of open boundary conditions and bottom friction coefficients is a very important aspect in the numerical simulation of tidal currents. The adjoint assimilation method can be used to invert the open boundary conditions and bottom friction coefficients in tidal models. In this experiment, the two-dimensional tidal wave accompanying assimilation model is used to assimilate altimeter data to simulate the M 2 Divide the tide. First, the original serial program is changed to a parallel program using the FPOM framework. The serial program has a total of 1210 lines (excluding blank lines, but includes necessary comments). After changing to parallel, a total of 110 lines of code are added, 104 lines are modified, and the parallel progra...
Embodiment 2
[0071] Parallelization of one and a half layer reduced gravity wind-induced circulation numerical models
[0072] In this example, a 1.5-layer reduced gravity wind-induced current model is used to carry out numerical simulation experiments of Indian Ocean currents. Ocean currents exist throughout the world's oceans, and their temporal and spatial changes are continuous, through which the world's oceans are organically linked. According to the actual wind field on the ocean, taking into account the fact that the Coriolis force varies with latitude and the friction of the terrain, the basic characteristics of ocean currents can be simulated, and the basic characteristics of ocean currents can be mastered. research is of great significance. Since the simulation of ocean currents requires a relatively high resolution, its calculation load is very large. In this calculation example, the numerical model is firstly parallelized by using FPOM. After parallelization, the program ...
Embodiment 3
[0076] Parallelization of numerical models of oceanic westward intensification
[0077] In this example, a one-and-a-half-layer barotropic model is used to simulate the westward strengthening of the ocean current field under the action of a steady wind field. Westward strengthening is an important phenomenon in oceanic circulation. Stommel and Munk et al. explained the westward strengthening of the ocean theoretically through the β effect, bottom friction and nonlinear inertial effects respectively. Since the spatial scale of the ocean is often large and requires a large amount of calculation, it is often time-consuming, and the total calculation time needs to be shortened through parallelism. In this example, FPOM is used to parallelize the numerical model first. After parallelization, the program code has a total of 453 lines (excluding blank lines and comment lines), of which 24 lines of code are added and 10 lines of code are modified in the process of changing from se...
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