Earth:Nucleus for European Modelling of the Ocean

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Short description: General model of ocean circulation developed by a European consortium


The Nucleus for European Modeling of the Ocean (NEMO) is a general model of ocean circulation developed by a European consortium and used in many countries of Europe.

Composition

NEMO is an ocean modeling platform composed of several models and numerical techniques for the use and processing of incoming and outgoing data. It has five main components:

  • Ocean: NEMO-OPA (Océan Parallélisé)
  • Sea ice: NEMO-LIM ("Louvain-la-neuve sea Ice Model")[1]
  • Biogeochemistry: NEMO-TOP/PISCES ("Tracer in the Ocean Paradigm")[2]
  • Grid refinement tools: NEMO-AGRIF
  • Data assimilation system: NEMO-TAM ("Tangent linear and Adjoint Model")[3]

It can be associated with other components of the climatic system, atmosphere and land surface, by means of OASIS.

Grid

Nemo is available in various configurations.[4]

Global configurations use ORCA tripolar grids, which allow the entire oceanic domain to be covered without singularity points.[5] In fact, the grid formed by the meridians and the parallels has two singularities: the North Pole and the South Pole. Near these two points the mesh size tends to zero, making the use of modeling equations problematic. To overcome the problem, the poles of the ORCA grids are positioned on the terrestrial sphere in such a way as to be located on continents. Since the South Pole is located on the Antarctic continent, a modification of the standard grid is not required, while the North Pole, which is located in the Arctic Ocean, is replaced by two points located one in North America and the other in Siberia. The ORCA grid is available in different horizontal resolutions ranging from about 2 degrees to 1/12 degree.

Development

The development of NEMO is organized and controlled by a European consortium[6] created in 2008 and formed by:

References

  1. ↑ Rousset, C.; Vancoppenolle, M.; Madec, G.; Fichefet, T.; Flavoni, S.; Barthélemy, A.; Benshila, R.; Chanut, J. et al. (2015-10-01). "The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities". Geosci. Model Dev. 8 (10): 2991–3005. doi:10.5194/gmd-8-2991-2015. ISSN 1991-9603. Bibcode: 2015GMD.....8.2991R. https://www.geosci-model-dev.net/8/2991/2015/. 
  2. ↑ Aumont, O.; Ethé, C.; Tagliabue, A.; Bopp, L.; Gehlen, M. (2015-08-13). "PISCES-v2: an ocean biogeochemical model for carbon and ecosystem studies". Geosci. Model Dev. 8 (8): 2465–2513. doi:10.5194/gmd-8-2465-2015. ISSN 1991-9603. Bibcode: 2015GMD.....8.2465A. https://www.geosci-model-dev.net/8/2465/2015/. 
  3. ↑ Vidard, A.; Bouttier, P.-A.; Vigilant, F. (2015-04-29). "NEMOTAM: tangent and adjoint models for the ocean modelling platform NEMO". Geosci. Model Dev. 8 (4): 1245–1257. doi:10.5194/gmd-8-1245-2015. ISSN 1991-9603. Bibcode: 2015GMD.....8.1245V. https://www.geosci-model-dev.net/8/1245/2015/. 
  4. ↑ Madec, Gurvan (2016). NEMO ocean engine. https://www.nemo-ocean.eu/wp-content/uploads/NEMO_book.pdf. 
  5. ↑ Gurvan Madec, Maurice Imbard (May 1996). "A global ocean mesh to overcome the North Pole singularity". Climate Dynamics 12 (6): 381–388. doi:10.1007/BF00211684. Bibcode: 1996ClDy...12..381M. 
  6. ↑ "NEMO goernance and strategy". https://www.nemo-ocean.eu/consortium/governance/. 

External links




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