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A MODEL OF PLANKTON DYNAMICS COUPLED WITH A LES OF THE SURFACE MIXED LAYER

机译:浮游生物动力学模型,耦合与表面混合层的LES

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The dynamics of phytoplankton populations are not only determined by biological processes such as growth/mortality rates, nutrient levels and predator-prey interactions, but by the distributions of the micro-organisms, which are governed by the physical structures and motions of the ocean (Denman & Gargett 1995). These biological-physical interactions take place over a wide range of different scales, e.g. upwelling gyres over many kilometres are often nutrient rich and associated with high phytoplankton concentrations, whilst individual predator-prey encounters are governed by turbulent motion on the scale of millimetres. In this presentation the influence of physical processes on an intermediate scale (tens of metres), namely those associated with the large-eddy structures of turbulence in the surface mixed layer, on a simple ecosystem will be examined. The objective of the work will be to see what characteristics of the water motion, e.g. horizontal and vertical mixing, vortical structures, are associated with high levels of phytoplankton activity, and how these are correlated with local nutrient and predatory zooplankton concentrations.
机译:浮游植物种群的动态不仅由生物学方法(如生长/死亡率,营养水平和捕食者 - 杂种相互作用)决定,而是通过微生物的分布,其受海洋的物理结构和运动( Denman&Gargett 1995)。这些生物学 - 物理相互作用在各种不同的尺度上进行,例如,超过千公里的升高的旋转往往营养丰富,与高浮游植物浓度有关,同时个体捕食者 - 猎物遭遇受到毫米尺度的湍流运动来控制。在该介绍中,将研究在简单的生态系统上对具有表面混合层中的湍流的大涡流结构相关的物理过程对中间刻度(几十米)的影响。这项工作的目的是看到水运动的特点,例如,水平和垂直混合,涡旋结构与高水平的浮游植物活动相关,以及这些活动的型植物活性与局部营养素和捕食性浮游动物浓度相关。

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