Q 3.. Type of observations
Post processing
Model operational suit in NWP
Models operational suites:
Weather forecast range from
24 hours to 7 days
Numerical Weather Prediction (NWP)
ois the part of Meteorology Science which is dealing with modeling of the atmospheric conditions and trying to predict these conditions in the near future.
oIt is among the most expensive technologies in term of CPU consumption.
oAt GHQ Meteorological Department, It is based on three specific models:
NWP consists in :
Horizontal resolution
Vertical resolution.
◦Fine near the surface, weak upward.
◦When the number of vertical levels is large enough, convective circulation is better taken into account by the models.
Increasing horizontal resolution by a factor of two (2) increases
the number of “cubes”, and implies computation machines 8 times faster.
The horizontal resolution of an NWP model is directly related to
the size of the weather feature it can simulate.
The horizontal resolution of an NWP model is directly related to the size of the weather feature it can simulate.
The resolution is related to
either the spacing between grid points for grid-point models or
the number of waves used to represent weather data for spectral models.
Models Grids Vertical Resolution
Hydrostatic approach
assume hydrostatic equilibrium, in which the downward weight of the atmosphere balances the upward-directed pressure gradient.
Non-hydrostatic
processes and their effect become important when the length of a feature is approximately equal to its height.
◦Convective storms.
◦Gust fronts.
◦Gravity waves (mountain waves and turbulence)
Necessity of physics parameterization
Some atmospheric phenomena need to be parameterized in order to take into account their impact, because:
Global models
The most popular global models are :
Global models are used to
forecast general synoptic circulation and to provide Initial and Lateral Boundary Data for Limited Area models.
Limited Area Models (LAM).
Limited Area Models (LAM).
They resolve the atmospheric equations on regional or local limited area domains.
They can use very high resolution (100m to 50km) and more vertical levels. They can catch very small phenomena.
They are adequate to incorporate complex physics parameterizations (especially microphysics, deep/shallow convection and boundary layer turbulence).
They can run on small to medium computers (normal PCs, workstations, Servers, Clusters)
Limited Area Models (LAM).
They are obliged to get
LBC and Initial data from global models
The most popular LAMs are: