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Contribution to the Themed Section: Advances in Plankton Modelling and Biodiversity Evaluation A 1D physical-biological model of the impact of highly intermittent phytoplankton distributions

机译:对主题部分的贡献:浮游生物建模和生物多样性评估的进展一维高度间歇性浮游植物分布影响的一维物理生物学模型

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Highly intermittent spatial variability of phytoplankton is observed ubiquitously in marine ecosystems, especially when measurements are performed at the micro-scale level. Therefore, theoretical developments and new modelling tools are required to understand the observed small-scale vertical structure and its relationship to ecosystem behaviour. Nearly all current ecosystem models are formulated entirely based on the mean field approximation, ignoring subgrid scale variability. Even if such approximation may be reasonable for meso-scales (and above), it cannot account for micro-scale dynamics, which may also impact macroscopic properties at the larger scale. To consider intermittency of variables in plankton ecosystem models, we apply a newly developed modelling approach called the closure approach. Detailed simulations were conducted, combining fluid-dynamics of the 1D water column with the nutrient-phytoplankton closure ecosystem model for application to a site in the northern North Sea. Compared with a control model, which does not account for such intermittency, the closure model produced substantially different spatio-temporal patterns of mean phytoplankton biomass and growth rate, which depended on the overall level of variability. In this study, we (i) seek to explore the effects of sub-scale variability coupled with physical transport and (ii) begin to address the yet unresolved question of how to consistently model the advection and diffusion of the variances and co-variances used to represent sub-scale variability in the closure approach. Our results suggest that it may be necessary to account explicitly for the intermittent distribution of plankton and nutrients, even in large-scale biogeochemical models.
机译:在海洋生态系统中普遍观察到浮游植物的高度间歇性空间变异性,尤其是在微观尺度上进行测量时。因此,需要理论上的发展和新的建模工具来理解所观察到的小规模垂直结构及其与生态系统行为的关系。几乎所有当前的生态系统模型都是完全基于平均场近似公式制定的,而忽略了亚电网规模的可变性。即使这种近似对于中尺度(或更高尺度)可能是合理的,它也不能解释微观尺度的动力学,这也可能在更大尺度上影响宏观性质。为了考虑浮游生物生态系统模型中变量的间歇性,我们应用了一种新开发的建模方法,称为封闭方法。进行了详细的模拟,将一维水柱的流体动力学与营养性浮游植物封闭生态系统模型相结合,以应用于北海北部某个地点。与不考虑这种间歇性的控制模型相比,封闭模型产生的浮游植物平均生物量和生长速度的时空格局基本不同,这取决于总体变异水平。在这项研究中,我们(i)寻求探索子尺度变异性与物理运输的关系,并且(ii)开始解决尚未解决的问题,即如何一致地对所使用的方差和协方差的对流和扩散建模代表封闭方法中的子规模可变性。我们的结果表明,即使在大规模生物地球化学模型中,可能也必须明确考虑浮游生物和营养物的间歇性分布。

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