NWP basics Flashcards
weather prediction forecast range from
24 hours to 7 days
Numerical Weather Prediction (NWP) definition
o) is the part of Meteorology Science which is dealing with modeling of the atmospheric conditions and trying to predict these conditions in the near future.
models of NWP
- WRF (Weather Research & Forecasting) model for weather parameters prediction
- WAM (Wave Model) for sea state forecast
- WRF-CHEM for pollutants and dust transport
NWP consists in:
- Subdividing a chosen geographic 3D area in thousands (or millions) of little cubes (boxes)
- Gathering all current (and past) actual information about atmosphere and ocean : all types of observational data.
- Affecting one value for the main meteorological parameters (Pressure, Temperature, Wind, Humidity) in each cube.
- Calculating through complex equations (momentum, thermodynamics, physics) the modifications affecting these meteorological parameters in time.
- Presenting the predicted parameters values in a comprehensible standard format (charts, meteograms, soundings, …etc).
which type of resolution can show you the small scale phenomenas
When resolution is fine enough (< 10km), small scale phenomena (thunder storms, convective cells, sea breeze, local sand storms… etc) could be well depicted.
Increasing………………………. by a factor of two (2) increases the number of “cubes”, and implies computation machines ………..times faster.
horizontal resolution
8
The horizontal resolution of an NWP model is directly related to
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.
conditions for vertical resolution grids
- Vertical resolution must be quite fine (on the order of a few millibars) near the earth’s surface.
- An increase in resolution is necessary near and below the tropo-pause to predict the jet stream accurately.
- Different numerical models use a variety of vertical coordinates types to represent atmospheric layers.
Atmospheric state at t
t = to + Δt
Atmospheric state
to + N*Δt
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.
Some atmospheric phenomena need to be parameterized in order to take into account their impact, because:
- Computers are not yet powerful enough to directly treat them.
- They are often not understood well enough to be represented by an equation.
- Their effects profoundly impact model fields and are crucial to creating realistic forecasts
Global models
resolve atmospheric equations on the whole globe
global models can not use …………… because of…………………
very fine resolution
computer limitations
global models cannot detect
small scale phenomena
Global models are used to
forecast general synoptic circulation and to provide Initial and Lateral Boundary Data for Limited Area models.