Investigating the seasonal vertical structure of phytoplankton in shelf seas

Jonathan Sharples
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引用次数: 41

Abstract

A 1-dimensional (vertical) physical-biological coupled model is presented. The model is designed for investigations into the link between the vertical turbulent structure of a coastal or shelf sea water column, and the primary production. The physical model employs a turbulence closure scheme to provide the link between local vertical stability (driven by seasonal solar heating) and the vertical turbulent mixing (driven by tidal currents and surface wind stress). The biological component of the model is a simple cell quota, threshold limitation model, with either 1 or 2 taxa/species of phytoplankton growing in response to light and dissolved inorganic nitrogen. The user has control over all model physical and biological driving parameters. Graphical screen output, suitable for basic visualisation and teaching purposes, is generated as the model operates, and more detailed data are written to files for later analysis.

In order to demonstrate the model's use in simple hypothesis investigation, an example of the model operation is illustrated. This focuses on the effect that the springs-neaps tidal cycle has on the production within the summer sub-surface biomass maximum, illustrating the fortnightly input of new nitrogen into the thermocline and the subsequent new production.

陆架海域浮游植物的季节垂直结构研究
提出了一个一维(垂直)物理-生物耦合模型。该模型旨在研究海岸或陆架水柱的垂直湍流结构与初级生产之间的联系。物理模型采用湍流闭合方案来提供局部垂直稳定性(由季节性太阳能加热驱动)和垂直湍流混合(由潮流和表面风应力驱动)之间的联系。该模型的生物学组成部分是一个简单的细胞配额、阈值限制模型,其中1或2个浮游植物分类群/物种对光和溶解的无机氮的反应而生长。用户可以控制所有模型的物理和生物驾驶参数。适用于基本可视化和教学目的的图形屏幕输出是在模型运行时生成的,更详细的数据被写入文件以供稍后分析。为了证明该模型在简单假设调查中的应用,举例说明了该模型的操作。这集中于春季-小潮潮周期对夏季地表下生物量最大值内生产的影响,说明了每两周向温跃层输入新氮以及随后的新生产。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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