Table of Contents - The Atmospheric Studies Group at TRC
Table of Contents - The Atmospheric Studies Group at TRC Table of Contents - The Atmospheric Studies Group at TRC
Section 8: CALMET Model Files Table 8-4 (Continued) Input Group 5 - Wind Field Options and Parameters Variable Type Description Default Value ISTEPPG integer Timestep (hours) of the prognostic model input data IGFMET integer Use coarse CALMET fields as initial guess fields LVARY logical Control variable for use of varying radius of influence. If no stations with valid data are found within the specified radius of influence, then the closest station with valid data will be used. (T=use, F=do not use.) RMAX1 real Maximum radius of influence over land in the surface layer (km). This parameter should reflect the limiting influence of terrain features on the interpolation at this level. RMAX2 real Maximum radius of influence over land in layers aloft (km). RMAX2 is generally larger than RMAX1 because the effects of terrain decrease with height. RMAX3 real Maximum radius of influence overwater (km). RMAX3 is used for all layers overwater. It must be large enough to ensure that all grid points over water are large enough to be within the radius of influence of at least one observation. RMIN real Minimum radius of influence used in the wind field interpolation (km). This parameter should be assigned a small value (e.g., 1. 1 0 F - - - 0.1 4.0 (Input Group 5 Continued) 8-43
Section 8: CALMET Model Files Table 8-4 (Continued) Input Group 5 - Wind Field Options and Parameters Variable Type Description Default Value TERRAD real Radius of influence of terrain features (km) - R1 real Weighting parameter for the diagnostic wind field in the surface layer (km). This parameter controls the relative weighting of the first-guess wind field produced by the diagnostic wind field model and the observations. R1 is the distance from an observational station at which the observation and the first-guess field are equally weighted. R2 real Weighting parameter for the diagnostic wind field in the layers aloft (km). R2 is applied in the upper layers in the same manner as R1 is used in the surface layer. RPROG real Weighting parameter (km) for the prognostic wind field data DIVLIM real Convergence criterion for the divergence minimization procedure NITER integer Maximum number of iterations for the divergence minimization procedure NSMTH integer array Number of smoothing passes in each layer NZ values must be entered. NINTR2 integer array Maximum number of stations used in the interpolation of data to a grid point for each layer 1-NZ. This allows only the "NINTR2" closest stations to be included in the interpolation. The effect of increasing NINTR2 is similar to smoothing. NZ values must be entered. CRITFN real Critical Froude number used in the evaluation of terrain blocking effects - - - 5.0E-6 50 2,(MXNZ-1)*4 99 1.0 (Input Group 5 Continued) 8-44
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Section 8: CALMET Model Files<br />
<strong>Table</strong> 8-4 (Continued)<br />
Input <strong>Group</strong> 5 - Wind Field Options and Parameters<br />
Variable Type Description Default Value<br />
ISTEPPG integer Timestep (hours) <strong>of</strong> the prognostic model input<br />
d<strong>at</strong>a<br />
IGFMET integer Use coarse CALMET fields as initial guess<br />
fields<br />
LVARY logical Control variable for use <strong>of</strong> varying radius <strong>of</strong><br />
influence. If no st<strong>at</strong>ions with valid d<strong>at</strong>a are<br />
found within the specified radius <strong>of</strong> influence,<br />
then the closest st<strong>at</strong>ion with valid d<strong>at</strong>a will be<br />
used. (T=use, F=do not use.)<br />
RMAX1 real Maximum radius <strong>of</strong> influence over land in the<br />
surface layer (km). This parameter should<br />
reflect the limiting influence <strong>of</strong> terrain fe<strong>at</strong>ures<br />
on the interpol<strong>at</strong>ion <strong>at</strong> this level.<br />
RMAX2 real Maximum radius <strong>of</strong> influence over land in<br />
layers al<strong>of</strong>t (km). RMAX2 is generally larger<br />
than RMAX1 because the effects <strong>of</strong> terrain<br />
decrease with height.<br />
RMAX3 real Maximum radius <strong>of</strong> influence overw<strong>at</strong>er (km).<br />
RMAX3 is used for all layers overw<strong>at</strong>er. It<br />
must be large enough to ensure th<strong>at</strong> all grid<br />
points over w<strong>at</strong>er are large enough to be within<br />
the radius <strong>of</strong> influence <strong>of</strong> <strong>at</strong> least one<br />
observ<strong>at</strong>ion.<br />
RMIN real Minimum radius <strong>of</strong> influence used in the wind<br />
field interpol<strong>at</strong>ion (km). This parameter<br />
should be assigned a small value (e.g., <br />
1.<br />
1<br />
0<br />
F<br />
-<br />
-<br />
-<br />
0.1<br />
4.0<br />
(Input <strong>Group</strong> 5 Continued)<br />
8-43