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Adapting to life: ocean biogeochemical modelling and adaptive remeshing

机译:适应生活:海洋生物地球化学建模和自适应网格化

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An outstanding problem in biogeochemical modelling of the ocean is that many of the key processes occur intermittently at small scales, such as the sub-mesoscale, that are not well represented in global ocean models. As an example, state-of-the-art models give values of primary production approximately two orders of magnitude lower than those observed in the ocean's oligotrophic gyres, which cover a third of the Earth's surface. This is partly due to their failure to resolve sub-mesoscale phenomena, which play a significant role in nutrient supply. Simply increasing the resolution of the models may be an inefficient computational solution to this problem. An approach based on recent advances in adaptive mesh computational techniques may offer an alternative. Here the first steps in such an approach are described, using the example of a~simple vertical column (quasi 1-D) ocean biogeochemical model. We present a novel method of simulating ocean biogeochemical behaviour on a vertically adaptive computational mesh, where the mesh changes in response to the biogeochemical and physical state of the system throughout the simulation. We show that the model reproduces the general physical and biological behaviour at three ocean stations (India, Papa and Bermuda) as compared to a high-resolution fixed mesh simulation and to observations. The simulations capture both the seasonal and inter-annual variations. The use of an adaptive mesh does not increase the computational error, but reduces the number of mesh elements by a factor of 2–3, so reducing computational overhead. We then show the potential of this method in two case studies where we change the metric used to determine the varying mesh sizes in order to capture the dynamics of chlorophyll at Bermuda and sinking detritus at Papa. We therefore demonstrate adaptive meshes may provide a~suitable numerical technique for simulating seasonal or transient biogeochemical behaviour at high spatial resolution whilst minimising computational cost.
机译:海洋生物地球化学建模中的一个突出问题是,许多关键过程间歇性地在小范围内发生,例如亚中尺度,这在全球海洋模型中没有得到很好的体现。例如,最先进的模型给出的初级生产值比在覆盖地球表面三分之一的海洋贫营养回旋中观测到的值低大约两个数量级。部分原因是由于它们无法解决亚中尺度现象,而后者在营养供应中起着重要作用。简单地增加模型的分辨率可能是该问题的低效计算解决方案。基于自适应网格计算技术的最新进展的方法可以提供替代方案。这里,以简单的垂直柱(准一维)海洋生物地球化学模型为例,描述了这种方法的第一步。我们提出了一种在垂直自适应计算网格上模拟海洋生物地球化学行为的新颖方法,其中网格在整个模拟过程中响应系统的生物地球化学和物理状态而变化。我们显示,与高分辨率固定网格模拟和观测结果相比,该模型再现了三个​​海洋站(印度,爸爸和百慕大)的一般物理和生物学行为。模拟捕获了季节性和年度间的变化。自适应网格的使用不会增加计算误差,但是会将网格元素的数量减少2-3倍,因此减少了计算开销。然后,我们在两个案例研究中展示了这种方法的潜力,在这些案例研究中,我们更改了用于确定变化的网格大小的度量,以便捕获百慕大的叶绿素和爸爸的下沉碎屑的动态。因此,我们证明自适应网格可以为在高空间分辨率下模拟季节性或瞬时生物地球化学行为同时最小化计算成本提供合适的数值技术。

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