Nucleus for European Modelling of the Ocean
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.
Contents
1 Composition
2 Grid
3 Development
4 References
5 External links
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]
- Grinding 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:
French National Center for Scientific Research, France
Mercator Ocean, France
Natural Environment Research Council, United Kingdom
Met Office, United Kingdom
Euro-Mediterranean Center on Climate Change, Italy
National Institute of Geophysics and Volcanology, Italy
References
^ Rousset, C.; Vancoppenolle, M.; Madec, G.; Fichefet, T.; Flavoni, S.; Barthélemy, A.; Benshila, R.; Chanut, J.; Levy, C. (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..mw-parser-output cite.citationfont-style:inherit.mw-parser-output .citation qquotes:"""""""'""'".mw-parser-output .citation .cs1-lock-free abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-subscription abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registrationcolor:#555.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration spanborder-bottom:1px dotted;cursor:help.mw-parser-output .cs1-ws-icon abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png")no-repeat;background-position:right .1em center.mw-parser-output code.cs1-codecolor:inherit;background:inherit;border:inherit;padding:inherit.mw-parser-output .cs1-hidden-errordisplay:none;font-size:100%.mw-parser-output .cs1-visible-errorfont-size:100%.mw-parser-output .cs1-maintdisplay:none;color:#33aa33;margin-left:0.3em.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-formatfont-size:95%.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-leftpadding-left:0.2em.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-rightpadding-right:0.2em
^ 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.
^ 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.
^ Madec, Gurvan (2016). NEMO ocean engine (PDF).
^ 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.CS1 maint: Uses authors parameter (link)
^ "NEMO goernance and strategy".
External links
- www.nemo-ocean.eu