ADREA-I: A Three-Dimensional Transient Transport Code for Complex Terrain and Other Applications
- 12 May 1991
- journal article
- research article
- Published by Taylor & Francis in Nuclear Technology
- Vol. 94 (2) , 135-148
- https://doi.org/10.13182/nt91-a34537
Abstract
The ADREA-I code is a three-dimensional transient analytical tool that can provide atmospheric boundary layer and dispersion analysis at the mesoscale and microscale levels, under any atmospheric stability conditions and with any ground complexity, and it is particularly suitable for large topographical disturbances and consequently large atmospheric altitudes. The code, in response to the need to treat large topographical disturbances with the highest spatial and temporal numerical resolution possible, introduces new features in the description of anomalous topography, turbulent diffusion coefficients, and numerical approach. Applications carried out within the framework of validation and demonstration studies of ADREA-I give reasonable results.Keywords
This publication has 17 references indexed in Scilit:
- Turbulent diffusion modelling FQR wind flow and dispersion analysisAtmospheric Environment (1967), 1989
- Numerical simulations of stratiform boundary-layer clouds on the meso-γ-scale. Part I: The influence of terrain height differencesBoundary-Layer Meteorology, 1988
- Terrain classification and derived meteorological parameters for interregional transport modelsAtmospheric Environment (1967), 1983
- A Numerical Experiment on the Mountain and Valley WindsJournal of the Meteorological Society of Japan. Ser. II, 1982
- MASCON—A Mass Consistent Atmospheric Flux Model for Regions with Complex TerrainJournal of Applied Meteorology, 1978
- A Numerical Study on the Effects of a Mountain on the Land and Sea BreezesJournal of the Meteorological Society of Japan. Ser. II, 1978
- Representation of the Heated Planetary Boundary Layer in Mesoscale Models with Coarse Vertical ResolutionJournal of the Atmospheric Sciences, 1975
- The evolution of a convective planetary boundary layer ? A higher-order-closure model studyBoundary-Layer Meteorology, 1974
- Three-dimensional numerical study of turbulence in an entraining mixed layerBoundary-Layer Meteorology, 1974
- Three-dimensional numerical study of the height and mean structure of a heated planetary boundary layerBoundary-Layer Meteorology, 1974