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| == Introduction == | |
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| === Introduction === | |
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| pyOM2.0 (Python Ocean Model) is a numerical circulation ocean model which was written for educational purpose. It is meant to be a simple and easy to use numerical tool to configure and to integrate idealized and realistic numerical simulations of the ocean in Boussinesq approximation. |
pyOM2 is a numerical circulation ocean model. Idealized and realistic configurations are simple and easy to configure and to integrate. |
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| * Non-hydrostatic configurations | * Hydrostatic or non-hydrostatic configurations |
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| Several idealized and realistics experiments and examples are preconfigured and can be easily chosen and modified using two alternative configuration methods based on Fortran90 or Python. |
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| * pyOM2 installed on small Debian system as Virtual box client | * pyOM2 installed on lightweight Debian system as Virtual box client |
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| == Prerequisites and Installation == |
=== Prerequisites and Installation === |
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| the module numpy, several other modules can be used to provide | the module Numpy, several other modules can be used to provide |
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| === Installation === | For installation details refer to the [[attachment:pyOM2.pdf|Documentation]] |
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| For installation details look at [[attachment:pyOM2.pdf|Documentation]] | === Idealized configurations === |
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| * Vertical shear instability in a non-hydrostatic [[/Kelvin Helmholtz|configuration]] | |
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| == Sample Configurations == | * Holmboe instability in a non-hydrostatic [[/Holmboe|configuration]] |
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| Several idealized experiments and examples are preconfigured and can be easily chosen and modified using two alternative configuration methods based on Fortran90 or Python. |
* Internal gravity wave beams in a non-hydrostatic [[/internal wave|configuration]] * Rayleigh-Bernard convection in a non-hydrostatic [[/Rayleigh Bernard|configuration]] * eddy-driven zonal jets in a wide hydrostatic channel [[/zonal jets|configuration]] * the classical Eady problem in a narrow hydrostatic channel [[/Eady 1|configuration]] * another Eady setup with linear stability analysis [[/Eady 2|configuration]] * small closed basin with wind-driven channel [[/ACC 1|configuration]] * large closed basin and hydrostatic channel [[/ACC 2|configuration]] === Realistic configurations === * 4x4 deg global ocean [[/4x4 global model|model]] * 4x4 deg global ocean with 45 levels [[/4x4 global model 15 levels|model]] * 2x2 deg global ocean [[/2x2 global model|model]] * 1x1 deg global ocean [[/1x1 global model|model]] * 4/3 x 4/3 deg North Atlantic regional [[/1.3x1.3 North Atlantic model|model]] * 1/3 x 1/3 deg North Atlantic regional model * 1/12 x 1/12 deg North Atlantic regional model |
Python Ocean Model 2.0 (pyOM2)
Contents
Introduction
pyOM2 is a numerical circulation ocean model. Idealized and realistic configurations are simple and easy to configure and to integrate.
Features are:
* Cartesian or pseudo-spherical coordinate systems
* Hydrostatic or non-hydrostatic configurations
* several energetically consistent parameterisations
* Fortran and Python front end
* Graphical User Interface
Fortran and Python version are based on the identical Fortran90 code which is fully parallelized based on the MPI-library to enhance performance. Several idealized and realistics experiments and examples are preconfigured and can be easily chosen and modified using two alternative configuration methods based on Fortran90 or Python.
Resources
Source code as tar ball
- pyOM2 installed on lightweight Debian system as Virtual box client
Prerequisites and Installation
Prerequisites for the Fortran front are Fortran 90 compiler, Lapack and NetCDF library
Prerequisites for the Python front end is Python and the module Numpy, several other modules can be used to provide a graphical user interface, Netcdf IO, etc
For installation details refer to the Documentation
Idealized configurations
* Vertical shear instability in a non-hydrostatic configuration
* Holmboe instability in a non-hydrostatic configuration
* Internal gravity wave beams in a non-hydrostatic configuration
* Rayleigh-Bernard convection in a non-hydrostatic configuration
* eddy-driven zonal jets in a wide hydrostatic channel configuration
* the classical Eady problem in a narrow hydrostatic channel 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