4.7 Article

The Meridionally Averaged Model of Eastern Boundary Upwelling Systems (MAMEBUSv1.0)

Journal

GEOSCIENTIFIC MODEL DEVELOPMENT
Volume 14, Issue 2, Pages 763-794

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/gmd-14-763-2021

Keywords

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Funding

  1. National Science Foundation [OCE-1538702, OCE-1751386, OCE-1635632, ACI-1548562]
  2. National Aeronautics and Space Administration [80NSSC19K1192]

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Eastern boundary upwelling systems (EBUSs) are active regions in the ocean with significant impacts on ocean ecology, biogeochemistry, and global fish catch. Studied using models ranging from 2-D to global, the Meridionally Averaged Model of Eastern Boundary Upwelling Systems (MAMEBUS) aims to combine the advantages of 2-D and 3-D approaches by parameterizing key 3-D processes in a 2-D framework. MAMEBUS facilitates future studies to efficiently explore the parameters controlling zonal variations in EBUSs.
Eastern boundary upwelling systems (EBUSs) are physically and biologically active regions of the ocean with substantial impacts on ocean biogeochemistry, ecology, and global fish catch. Previous studies have used models of varying complexity to study EBUS dynamics, ranging from minimal two-dimensional (2-D) models to comprehensive regional and global models. An advantage of 2-D models is that they are more computationally efficient and easier to interpret than comprehensive regional models, but their key drawback is the lack of explicit representations of important three-dimensional processes that control biology in upwelling systems. These processes include eddy quenching of nutrients and meridional transport of nutrients and heat. The authors present the Meridionally Averaged Model of Eastern Boundary Upwelling Systems (MAMEBUS) that aims at combining the benefits of 2-D and 3-D approaches to modeling EBUSs by parameterizing the key 3-D processes in a 2-D framework. MAMEBUS couples the primitive equations for the physical state of the ocean with a nutrient- phytoplankton-zooplankton-detritus model of the ecosystem, solved in terrain-following coordinates. This article defines the equations that describe the tracer, momentum, and biological evolution, along with physical parameterizations of eddy advection, isopycnal mixing, and boundary layer mixing. It describes the details of the numerical schemes and their implementation in the model code, and provides a reference solution validated against observations from the California Current. The goal of MAMEBUS is to facilitate future studies to efficiently explore the wide space of physical and biogeochemical parameters that control the zonal variations in EBUSs.

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