Jump to content

AWESOME-OCIM: Difference between revisions

From OceanWiki
Line 22: Line 22:


== Model overview ==
== Model overview ==
A Working Environment for Simulating Ocean Movement and Elemental cycling with an Ocean Circulation Inverse Model (AWESOME OCIM) is a tool for simulating ocean movement and tracer biogeochemical properties within a transport matrix model (TMM) framework.<ref>Smith, John. ''Astronomy Basics''. 2020.</ref> The circulation of the ocean is described in the form of a matrix where the ocean is discretized into a 3D shoebox by latitude, longitude, and depth. The circulation matrix is based off of
A Working Environment for Simulating Ocean Movement and Elemental cycling with an Ocean Circulation Inverse Model (AWESOME OCIM) is a tool for simulating ocean movement and tracer biogeochemical properties within a transport matrix model (TMM) framework.<ref>John, S. G., Liang, H., Weber, T., DeVries, T., Primeau, F., Moore, K., Holzer, M., Mahowald, N., Gardner, W., Mishonov, A., Richardson, M. J., Faugere, Y., & Taburet, G. (2020). AWESOME OCIM: A simple, flexible, and powerful tool for modeling elemental cycling in the oceans. Chemical Geology, 533, 119403. https://doi.org/10.1016/j.chemgeo.2019.119403
 
</ref> The circulation of the ocean is described in the form of a matrix where the ocean is discretized into a 3D shoebox by latitude, longitude, and depth. The circulation matrix is based off of


== Scales of interest ==
== Scales of interest ==

Revision as of 10:41, 7 April 2026


Model type
Approach: Statistical, Mechanistic optimized, or Mechanistic time-dependent
Computational demand: Local or HPC
Spatial resolution: grid: e.g. um, L, ocean basin; domain:
Temporal resolution: time step: e.g. s, h, day, steady-state; output:

Model overview

A Working Environment for Simulating Ocean Movement and Elemental cycling with an Ocean Circulation Inverse Model (AWESOME OCIM) is a tool for simulating ocean movement and tracer biogeochemical properties within a transport matrix model (TMM) framework.[1] The circulation of the ocean is described in the form of a matrix where the ocean is discretized into a 3D shoebox by latitude, longitude, and depth. The circulation matrix is based off of

Scales of interest

Data inputs

Example Studies & Code

Classic examples

Recent applications

Limitations

References

  1. ↑ John, S. G., Liang, H., Weber, T., DeVries, T., Primeau, F., Moore, K., Holzer, M., Mahowald, N., Gardner, W., Mishonov, A., Richardson, M. J., Faugere, Y., & Taburet, G. (2020). AWESOME OCIM: A simple, flexible, and powerful tool for modeling elemental cycling in the oceans. Chemical Geology, 533, 119403. https://doi.org/10.1016/j.chemgeo.2019.119403