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CSIB?v1 (Canadian Sea-ice Biogeochemistry): a sea-ice biogeochemical model for the NEMO community ocean modelling framework

机译:CSIB?v1(加拿大海冰生物地球化学):用于NEMO社区海洋建模框架的海冰生物地球化学模型

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Process-based numerical models are a useful tool for studying marine ecosystems and associated biogeochemical processes in ice-covered regions where observations are scarce. To this end, CSIB?v1 (Canadian Sea-ice Biogeochemistry version?1), a new sea-ice biogeochemical model, has been developed and embedded into the Nucleus for European Modelling of the Ocean (NEMO) modelling system. This model consists of a three-compartment (ice algae, nitrate, and ammonium) sea-ice ecosystem and a two-compartment (dimethylsulfoniopropionate and dimethylsulfide) sea-ice sulfur cycle which are coupled to pelagic ecosystem and sulfur-cycle models at the sea-ice–ocean interface. In addition to biological and chemical sources and sinks, the model simulates the horizontal transport of biogeochemical state variables within sea ice through a one-way coupling to a dynamic-thermodynamic sea-ice model (LIM2; the Louvain-la-Neuve Sea Ice Model version?2). The model results for 1979 (after a decadal spin-up) are presented and compared to observations and previous model studies for a brief discussion on the model performance. Furthermore, this paper provides discussion on technical aspects of implementing the sea-ice biogeochemistry and assesses the model sensitivity to (1)?the temporal resolution of the snowfall forcing data, (2)?the representation of light penetration through snow, (3)?the horizontal transport of sea-ice biogeochemical state variables, and (4)?light attenuation by ice algae. The sea-ice biogeochemical model has been developed within the generic framework of NEMO to facilitate its use within different configurations and domains, and can be adapted for use with other NEMO-based sub-models such as LIM3 (the Louvain-la-Neuve Sea Ice Model version?3) and PISCES (Pelagic Interactions Scheme for Carbon and Ecosystem Studies).
机译:基于过程的数值模型是研究缺乏观测的冰雪覆盖地区的海洋生态系统和相关生物地球化学过程的有用工具。为此,已经开发了一种新的海冰生物地球化学模型CSIB?v1(加拿大海冰生物地球化学版本?1),并将其嵌入到欧洲海洋建模核心(NEMO)建模系统中。该模型由一个三室(冰藻,硝酸盐和铵盐)海冰生态系统和一个两室(二甲基磺丙酸二甲酯和二甲基硫醚)海冰硫循环组成,这些循环与海洋中上层生态系统和硫循环模型耦合-ice-ocean接口。除了生物和化学来源和汇,该模型还通过单向耦合至动态-热力学海冰模型(LIM2; Louvin-la-Neuve海冰模型)来模拟海冰内生物地球化学状态变量的水平传输。版本2)。提出了1979年的模型结果(十年旋转之后),并将其与观测值和先前的模型研究进行了比较,以简要讨论模型性能。此外,本文对实施海冰生物地球化学的技术方面进行了讨论,并评估了模型对以下方面的敏感性:(1)降雪强迫数据的时间分辨率;(2)透雪光的表示;(3) “海冰生物地球化学状态变量的水平传输”,以及(4)冰藻对光的衰减。海冰生物地球化学模型是在NEMO的通用框架内开发的,以促进其在不同配置和领域中的使用,并且可以适应与其他基于NEMO的子模型(如LIM3)一起使用(卢旺-拉-新海冰模型版本3)和PISCES(碳与生态系统研究的相互作用)。

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