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| * pyOM2 installed on lightweight Debian system as Virtual box client | * pyOM2 installed on lightweight Debian system as [[attachment:pyOM2.vdi|Virtual box client]] |
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| * Vertical shear instability in a non-hydrostatic [[TO/pyOM2/Kelvin Helmholtz|configuration]] | * Vertical shear instability [[TO/pyOM2/Kelvin Helmholtz|configuration]] |
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| * Holmboe instability in a non-hydrostatic [[TO/pyOM2/Holmboe|configuration]] | * Holmboe instability [[TO/pyOM2/Holmboe|configuration]] |
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| * Internal gravity wave beams in a non-hydrostatic [[TO/pyOM2/internal wave|configuration]] | * Internal gravity wave beam [[TO/pyOM2/internal wave|configuration]] |
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| * Rayleigh-Bernard convection in a non-hydrostatic [[TO/pyOM2/Rayleigh Bernard|configuration]] | * Rayleigh-Bernard convection [[TO/pyOM2/Rayleigh Bernard|configuration]] |
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| * eddy-driven zonal jets in a wide hydrostatic channel [[TO/pyOM2/zonal jets|configuration]] | * eddy-driven zonal jet [[TO/pyOM2/zonal jets|configuration]] |
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| * the classical Eady problem in a narrow hydrostatic channel [[TO/pyOM2/Eady 1|configuration]] | * the classical Eady problem [[TO/pyOM2/Eady 1|configuration]] |
Python Ocean Model 2.0 (pyOM2)
Introduction
pyOM2 is a numerical circulation ocean model powered by Python. Features are:
* Cartesian or pseudo-spherical coordinate systems
* Hydrostatic or non-hydrostatic configurations
* energetically consistent parameterisations
* Fortran and Python front end
* Graphical User Interface
* fully parallelized using MPI
Idealized and realistic configurations are simple and easy to configure and to integrate. Fortran and a Python version are based on the identical Fortran90 core code. Several idealized and realistic examples are preconfigured and can be easily chosen and modified using two alternative configuration methods based on Fortran90 or Python.
Downloads
Source code as tar ball
pyOM2 installed on lightweight Debian system as Virtual box client
Installation
For installation details refer to the Documentation
Idealized configurations
* Vertical shear instability configuration
* Holmboe instability configuration
* Internal gravity wave beam configuration
* Rayleigh-Bernard convection configuration
* eddy-driven zonal jet configuration
* the classical Eady problem configuration
* another Eady setup with linear stability analysis configuration
* small closed basin with wind-driven channel configuration
* large closed basin and hydrostatic channel configuration
Realistic configurations
* 4x4 deg global ocean model
* 4x4 deg global ocean with 45 levels model
* 2x2 deg global ocean model
* 1x1 deg global ocean model
* 4/3 x 4/3 deg North Atlantic regional model
* 1/3 x 1/3 deg North Atlantic regional model
* 1/12 x 1/12 deg North Atlantic regional model