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along lines of constant depth, mixing must be rotated relative to the coordinate grid- a process that can be computationally expensive. By contrast, in codes which represent the ocean in terms of constant-density layers (which represent the flow in the ocean interior much more faithfully)- representation of the ocean mixed layer becomes a challenge.
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and encouraged by community feedback, led to the release of v2.0 (MOM2) in 1995. Pacanowski and
Stephen Griffies released v3.0 (MOM3) in 1999. Griffies, Matthew Harrison, Rosati and Pacanowski, with considerable input from a scientific community of hundreds of users, resulted in significant evolution
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at GFDL rewrote the Bryan-Cox-Semtner code in a modular form, enabling different options and configurations to be more easily generated and new physical parameterizations to be more easily included. This version, released on
December 5, 1990, became known as Modular Ocean Model v1.0 (MOM1). Further
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near the ocean surface. However, level coordinate models have problems when it comes to the representation of thin bottom boundary layers (Winton et al., 1998) and thick sea ice. Additionally, because mixing in the ocean interior is largely along lines of constant potential density rather than
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MOM has traditionally been a level-coordinate ocean model, in which the ocean is divided into boxes whose bottoms are located at fixed depths. Such a representation makes it easy to solve the momentum equations and the well-mixed, weakly stratified layer known as the ocean
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physical climate model series and the ESM2M Earth System Model. Versions of MOM have been used in hundreds of scientific papers by authors around the world. MOM4 is used as the basis for the El Nino prediction system employed by the
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of the code released as v4.0 (MOM4) in 2003. An update, v4.1 (MOM4p1) was released by
Griffies in 2009, as was the latest version v5.0 (MOM5), which was released in 2012.
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MOM3, MOM4, and MOM5 are used as a code base for the ocean component of the GFDL coupled models used in the
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Three-dimensional ocean circulation model for studying the ocean climate system
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system. The model is developed and supported primarily by researchers at the
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Atmospheric, oceanographic, cryospheric, and climate models
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MOM owes its genesis to work at GFDL in the late 1960s by
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979:Numerical climate and weather models
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180:(NOAA/GFDL) in Princeton, NJ, USA.
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628:Regional and mesoscale atmospheric
201:assessment reports, including the
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293:"Modular Ocean Model version 1"
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68:5.1.0 / March 25, 2014
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852:Land surface parametrization
442:Numerical weather prediction
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20:Modular Ocean Model (MOM)
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735:Atmospheric dispersion
321:MOM5 community website
70:; 10 years ago
42:; 33 years ago
989:Physical oceanography
40:December 5, 1990
953:Scientific modelling
467:Ensemble forecasting
295:. GFDL. 6 April 2017
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427:Oceanographic model
155:Modular Ocean Model
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894:Discontinued
767:DISPERSION21
316:MOM6 project
297:. Retrieved
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228:Bert Semtner
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26:Developer(s)
573:IFS (ECMWF)
412:Model types
361:MOM1 manual
356:MOM2 manual
351:MOM3 manual
346:MOM4 manual
336:MOM5 manual
240:Tony Rosati
236:Keith Dixon
224:Michael Cox
191:mixed layer
973:Categories
797:PUFF-PLUME
757:AUSTAL2000
616:GME / ICON
583:GEM / GDPS
532:GFDL CM2.X
299:2019-04-12
280:References
220:Kirk Bryan
203:GFDL CM2.X
100:Written in
75:2014-03-25
47:1990-12-05
838:GEOS-Chem
31:NOAA/GFDL
807:SAFE AIR
640:RR / RAP
252:See also
184:Overview
90:MOM6
843:CHIMERE
802:RIMPUFF
782:MERCURE
762:CALPUFF
612:JMA-GSM
527:HadGEM1
510:Climate
214:History
170:climate
134:Website
123:License
104:Fortran
73: (
45: (
917:NOGAPS
833:MOZART
752:ATSTEP
747:AERMOD
726:ADCIRC
716:MITgcm
658:HIRLAM
620:ARPEGE
603:NAVGEM
522:HadCM3
238:, and
52:(MOM1)
864:CLASS
859:JULES
828:CLaMS
812:SILAM
721:FESOM
711:FVCOM
692:HyCOM
678:HRDPS
654:RAQMS
598:NAEFS
557:ECHAM
552:CFSv2
167:ocean
141:.noaa
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869:ISBA
792:OSPM
787:NAME
777:MEMO
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742:ADMS
696:ROMS
674:RGEM
669:HWRF
662:LAPS
645:RAMS
593:MPAS
547:CESM
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222:and
199:IPCC
153:The
143:.gov
139:gfdl
111:Type
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912:NGM
907:MM5
903:LFM
900:Eta
706:MOM
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665:RPM
650:WRF
635:NAM
588:GFS
578:FIM
176:'s
159:MOM
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