4.7 Article

The Gulf of St. Lawrence Biogeochemical Model: A Modelling Tool for Fisheries and Ocean Management

Journal

FRONTIERS IN MARINE SCIENCE
Volume 8, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2021.732269

Keywords

biogeochemical model description; coastal biogeochemistry; Gulf of St; Lawrence; dissolved oxygen; carbonate system; nutrient transport and transformation; riverine contribution

Funding

  1. Fisheries and Oceans Canada: the Aquatic Climate Change Adaptation Services Program (ACCASP)
  2. Strategic Program for Ecosystem-based Research and Advice (SPERA)
  3. Center of Expertise on Hydropower Impacts on Fish and Fish Habitat (CHIF)
  4. Centre for Ocean Model Development and Applications (COMDA)

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This paper provides a detailed description and analysis of the coupled physical-biogeochemical model of the Gulf of St. Lawrence, with a focus on the microbial loop and riverine contributions. The model successfully reproduces key features of the system, such as phytoplankton bloom and hypoxic areas.
The goal of this paper is to give a detailed description of the coupled physical-biogeochemical model of the Gulf of St. Lawrence that includes dissolved oxygen and carbonate system components, as well as a detailed analysis of the riverine contribution for different nitrogen and carbonate system components. A particular attention was paid to the representation of the microbial loop in order to maintain the appropriate level of the different biogeochemical components within the system over long term simulations. The skill of the model is demonstrated using in situ data, satellite data and estimated fluxes from different studies based on observational data. The model reproduces the main features of the system such as the phytoplankton bloom, hypoxic areas, pH and calcium carbonate saturation states. The model also reproduces well the estimated transport of nitrate from one region to the other. We revisited previous estimates of the riverine nutrient contribution to surface nitrate in the Lower St. Lawrence Estuary using the model. We also explain the mechanisms that lead to high ammonium concentrations, low dissolved oxygen, and undersaturated calcium carbonate conditions on the Magdalen Shallows.

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