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| '''Python Ocean Model 2.0 (pyOM2)''' | '''Python Ocean Model 2.2 (pyOM2)''' |
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| == Introduction == | === Introduction === pyOM2 is a numerical circulation ocean model powered by [[https://www.python.org|Python]]. Features are: |
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| * Cartesian or pseudo-spherical coordinate systems | |
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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. Non-hydrostatic situations as well as large-scale oceanic flows can be considered, Cartesian or pseudo-spherical coordinate systems can be used. Several idealized experiments and examples are preconfigured and can be easily chosen and modified using two alternative configuration methods based on Fortran90 or Python. Prerequisites for the installation is a Fortran 90 compiler and the Lapack library, and for the Fortran front the NetCDF-library (since IO is realized mainly using the NetCDF format). For the Python front end, the numerical module \verb+numpy+ is required and several other modules can be used in addition, e.g. to provide a graphical user interface. Both version are based on identical Fortran90 code which is fully parallelized based on the MPI-library to enhance performance. |
* Hydrostatic or non-hydrostatic configurations |
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| * energetically consistent parameterisations | |
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| === Resources === * Model Manual [[attachment:pyOM2.pdf|Here]] |
* Fortran and Python front end |
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| * Ocean Model Source Code [[attachment:pyOM_2.1.tar.gz|Here]] | * Graphical User Interface |
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| == Prerequisites and Installation == === Prerequisites === |
* fully parallelized using [[http://www.mpi-forum.org/|MPI]] |
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| ... | 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. |
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| === Installation === | === Downloads === * [[attachment:pyOM2_2.pdf|Documentation]] |
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| ... | * Source code as [[attachment:pyOM2.2.0_shipping.tar.gz|tar ball]] |
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| === Installation === | |
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| == Sample Configurations == === Kelvin-Helmholtz Instability === [[https://wiki.zmaw.de/ifm/TO/pyOM/Kelvin-Helmholtz%20Instability|Content Here]] |
For installation details refer to the [[attachment:pyOM2.pdf|Documentation]] |
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| {{{ kelvin_helm1.py }}} === Rayleigh–Bénard Convection === [[https://wiki.zmaw.de/ifm/TO/pyOM/Rayleigh–Bénard%20Convection|Content Here]] |
=== Idealized configurations === * Vertical shear instability [[TO/pyOM2/Kelvin Helmholtz|configuration]] |
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| {{{ rayleigh.py }}} === Eady's Baroclinic Instability === [[https://wiki.zmaw.de/ifm/TO/pyOM/Rayleigh–Bénard%20Convection|Content Here]] |
* Holmboe instability [[TO/pyOM2/Holmboe|configuration]] |
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| {{{ eady1.py / eady2.py }}} === Eddy-driven zonal jets === [[https://wiki.zmaw.de/ifm/TO/pyOM/Eddy-driven%20Zonal%20Jets|Content Here]] |
* Internal gravity wave beam [[TO/pyOM2/internal wave|configuration]] |
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| {{{ jets1.py }}} === Thermohaline Circulation === [[https://wiki.zmaw.de/ifm/TO/pyOM/Thermohaline%20Circulation|Content Here]] |
* Rayleigh-Bernard convection [[TO/pyOM2/Rayleigh Bernard|configuration]] |
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| {{{ THC1.py }}} === Southern Ocean Circulation === [[https://wiki.zmaw.de/ifm/TO/pyOM/Southern%20Ocean%20Circulation|Content Here]] |
* eddy-driven zonal jet [[TO/pyOM2/zonal jets|configuration]] |
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| {{{ acc1.py }}} === ENSO Response === [[https://wiki.zmaw.de/ifm/TO/pyOM/ENSO%20Response|Content Here]] |
* the classical Eady problem [[TO/pyOM2/Eady 1|configuration]] |
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| {{{ enso1.py }}} === Equatorial Waves === [[https://wiki.zmaw.de/ifm/TO/pyOM/Equatorial%20Waves|Content Here]] |
* another Eady setup with linear stability analysis [[TO/pyOM2/Eady 2|configuration]] |
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| {{{ eq_waves1.py }}} === Isopycnal Diffusion === [[https://wiki.zmaw.de/ifm/TO/pyOM/Isopycnal%20Diffusion|Content Here]] |
* small closed basin with wind-driven channel [[TO/pyOM2/ACC 1|configuration]] |
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| {{{ isopyc_test1.py }}} An example of the python GUI for Eady's baroclinic instability case is shown below. |
* large closed basin and hydrostatic channel [[TO/pyOM2/ACC 2|configuration]] |
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| {{attachment:pyOM.png}} | === Realistic configurations === * 4x4 deg global ocean [[TO/pyOM2/4x4 global model|model]] * 4x4 deg global ocean with 45 levels [[TO/pyOM2/4x4 global model 45 levels|model]] * 2x2 deg global ocean with 45 levels [[TO/pyOM2/2x2 global model 45 levels|model]] * 1x1 deg global ocean [[TO/pyOM2/1x1 global model|model]] * 4/3 x 4/3 deg North Atlantic regional [[TO/pyOM2/1.3x1.3 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 2.2 (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
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 with 45 levels 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