Preprints
https://doi.org/10.5194/sp-2024-8
https://doi.org/10.5194/sp-2024-8
23 Sep 2024
 | 23 Sep 2024
Status: this preprint is currently under review for the journal SP.

Numerical Models for Monitoring and Forecasting Ocean Biogeochemistry: a short description of present status

Gianpiero Cossarini, Andy Moore, Stefano Ciavatta, and Katja Fennel

Abstract. The ability to model biogeochemical features in the ocean is a key factor in predicting the health of the ocean: it involves the representation of processes and cycles of chemical elements (such as carbon, nutrients and oxygen) and the dynamics of living organisms such as phytoplankton, zooplankton and bacteria. This paper gives an overview of the main modelling aspects aimed at describing the low trophic levels of marine ecosystems and shows how they can be coupled with advection and diffusion models to simulate the dynamics and distribution in the ocean. The complexity of biogeochemical models can vary considerably depending on the topics of interest, assumed hypothesis and simplification of the numerical parameterization. The paper also discusses the uncertainties in the numerical solution due to the lack of knowledge about the parameterizations, the initial and boundary conditions, the lack of a robust observation network and the high computational cost of running such models

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Gianpiero Cossarini, Andy Moore, Stefano Ciavatta, and Katja Fennel

Status: open (until 18 Nov 2024)

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Gianpiero Cossarini, Andy Moore, Stefano Ciavatta, and Katja Fennel
Gianpiero Cossarini, Andy Moore, Stefano Ciavatta, and Katja Fennel

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Short summary
Marine biogeochemistry refers to the cycling of chemical elements resulting from physical transport, chemical reaction, uptake, and processing by living organisms. Biogeochemical models can have a wide range of complexity, from single parameterizations of processes to fully explicit representations of several nutrients, trophic levels, and functional groups. Uncertainty sources are the lack of knowledge about the parameterizations, initial and boundary conditions and the lack of observations
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