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MODELING LOCAL-SCALE METEOROLOGY
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The Definition of the Mesoscale.
(Note: NOAA ARL is no longer running the RAMS mesoscale model.)
Mesoscale models are used to simulate sub-grid scale phenomena not resolved by regional-scale models. The
mesoscale ranges as defined by Orlanski (1975) :
| Scale |
Range |
Examples |
Applicable Model |
| Micro-scale |
< 2 km |
Turbulent eddies |
LES model |
| Meso-gamma |
2-20 km |
Thunderstorm convection, complex terrain flows |
Non-hydrostatic (ARPS) |
| Meso-beta |
20-200 km |
land-water, sea breezes |
Non-hydrostatic, hydrostatic (MM5, RAMS) |
| Meso-alpha |
200-2000 km |
Fronts, low-pressure systems |
Hydrostatic (Eta,AVN) |
Non-hydrostatic processes are important when the vertical motions in the atmosphere are
changing rapidly. The non-hydrostatic criteria is defined when the ratio of the height (H) to the length (L)
scale of an atmospheric circulation is much less than 1 (H/L << 1). For example, deep
convection non-hydrostatic effects must be parameterized since the length scale is order 1-2 km, but the height of the circulation can reach the top of the troposphere (10 km).
Mesoscale models normally include non-hydrostatic effects when the model grid spacing is
set finer than 10 km.
Popular mesoscale models in use today:
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