Modular Ocean Model
For shallow-water Lagrangian particle routing.
The Basic Model Interface is a set of functions for coupling models to models and models to data
Open-source MATLAB-based computational platform for modeling and analyzing steel frame buildings in OpenSEES.
System of HydrodYnamic Finite Element Modules
Header-only C++-Library for grid file I/O
Mesh generation using PyVista
Python GUI of Earth Observations and Model Evaluation Toolkit
Computing the spectrum of a four level atomic system
This is the repository is linked to the software MovingBoundaryMinerals.jl, which describes the diffusion-limited growth in mineral couples.
Python library for working with Integrated Water Flow Models
PaleoSea2D is an elaborate plugin for FEFLOW to simulate the postglacial evolution of a regional fractured-rock aquifer & aquitard subsurface system as a consequence of a major marine transgression combined with sedimentation of fines, rapid decrease in the relative sea/lake water level (~RSL), and convective migration of groundwater salinity.
A collection of different numerical examples implemented in deal.ii. Besides the geometry and mesh, the scripts also apply the boundary conditions if desired.
Soil Model for Enhanced Weathering (SMEW): a dynamic, depth-averaged ecohydrological and biogeochemical model for enhanced weathering dynamics in the upper soil layers.
An open source parallel programming language aimed at numerical modelling. Compiles to Fortran / MPI
Simple and fast 2D (depth-averaged) simulation model for snow avalanches
Computational SHG Modeling — A complete Fortran-based framework for simulating thermal effects in Second Harmonic Generation using FDM and coupled physics.
Motion detection of less than one pixel between two images dominated by background Poisson noise.
A collection of different numerical examples in LS-Dyna. Besides the geometry and mesh, the keyword files also apply the boundary conditions.
PaleoSea1D is an IFM plugin for FEFLOW to simulate diffusive or advective-dispersive transport of salinity in a forming aquitard and in the underlying aquifer.
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