rfinkelnburg/lxc_scripts
Scripts for more convenient lxc controlling...
Developer Profile
rfinkelnburg
Discovered public repositories for rfinkelnburg in the GitHub catalog.
rfinkelnburg/WRF_modified_modules
My modified WRF/Polar WRF FORTRAN modules.
rfinkelnburg/WRF_control
Control scripts for consecutive sequential WRF runs using intermediate formate files (IFF's) generated from former WRF modelling as input.
rfinkelnburg/WRF_manip_tools
This tool is intended to overcome limitations related to subordinated WRF down-scaling. It provides methods to generate or manipulate WPS and WRF input files for the subordinated down-scaling using former produced WRF outputs and/or further data sets. Currently, the tools are rather specific for a high resolution down-scaling project at Hansbreen glacier, Spitsbergen (Svalbard) and have to be adjusted for other areas or data sets. The tool suite is written in C++, Ansi-style, on Ubuntu/Debian.
rfinkelnburg/Trajectory
Source code of Finkelnburg, R., 2007. Entwicklung und Anwendung eines rechnergestützten Modells zur Ursachenanalyse großräumiger Luftschadstofftransporte (Development and application of a computerized model for cause analysis of large-scale air pollution transport). Diploma thesis, Technische Universität Berlin: Berlin. (see http://opus4.kobv.de/opus4-tuberlin/frontdoor/index/index/docId/4835)
rfinkelnburg/MetPhoMod
MetPhoMod the METeorogy and atmospheric PHOtochemstry mesoscale MODel. A prognostic three-dimensional Eulerian model for the simulation of summer smog was implemented which fully couples meteorological processes and gas phase chemistry. The model includes modules for atmospheric dynamics, atmospheric turbulence, transport, gas-phase chemistry, short- and long-wave radiation transfer, and surface interactions, including emission and deposition of trace gases. (see Perego, S., 1999. Metphomod ± a Numerical Mesoscale Model for Simulation of Regional Photosmog in Complex Terrain: Model Description and Application During Pollumet 1993 (Switzerland). Meteorol. Atmos. Phys., 70, 43-69. DOI: 10.1007/s007030050024)