Volume 1 - The Atmospheric Studies Group at TRC
Volume 1 - The Atmospheric Studies Group at TRC
Volume 1 - The Atmospheric Studies Group at TRC
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Table 4-6 lists meteorological d<strong>at</strong>a used in the SEA.DAT file after the adjustments<br />
are made. <strong>The</strong> l<strong>at</strong>eral turbulence intensity (I y ) is used in the CALPUFF turbulence<br />
profile file.<br />
<strong>The</strong> UP.DAT (upper-air) input file is designed to provide CALMET with vertical<br />
profiles of wind and temper<strong>at</strong>ure represent<strong>at</strong>ive of the onshore flow <strong>at</strong> 00Z (mid to<br />
l<strong>at</strong>e afternoon) during the tracer sampling. Both 00Z and 12Z vertical profiles of<br />
wind and temper<strong>at</strong>ure are developed for four levels: surface, 10m, overw<strong>at</strong>er mixing<br />
height, and model-top (3000m). <strong>The</strong> 00Z wind speed <strong>at</strong> 7m is extended to levels up to<br />
the mixing height using a stability-class-dependent power-law profile (A,B=0.07;<br />
C=0.10; D,E,F=0.15) and the speed <strong>at</strong> the model-top is set to th<strong>at</strong> <strong>at</strong> the mixing<br />
height. <strong>The</strong> surface wind speed is set to th<strong>at</strong> <strong>at</strong> 10m, which has been adjusted from<br />
the anemometer height to 10m. Wind direction <strong>at</strong> all levels equals the release wind<br />
direction. Temper<strong>at</strong>ure <strong>at</strong> the surface equals the air temper<strong>at</strong>ure in the SEA.DAT file,<br />
and temper<strong>at</strong>ure aloft is computed from this using the temper<strong>at</strong>ure gradient dT/dz (in<br />
the SEA.DAT file) up to the overw<strong>at</strong>er mixing height. <strong>The</strong> default CALMET<br />
temper<strong>at</strong>ure gradient -0.0045 ºK/m is used above the mixing height. Pressure is<br />
assumed to be 1013 mb <strong>at</strong> the surface, and decreases with height <strong>at</strong> 0.1 mb/m.<br />
Ventura, California<br />
Description<br />
<strong>The</strong> tracer dispersion study in the Ventura, California area was conducted along the<br />
California coast during four test days in September 1980 and four test days in<br />
January 1981 (Areovironment, 1980 and 1981, Zanetti et al., 1981, and Schacher et<br />
al., 1982). D<strong>at</strong>a from all four of the test days in September and three of the four test<br />
days in January are in the d<strong>at</strong>aset. SF 6 tracer was released about 8m above the w<strong>at</strong>er<br />
from a bo<strong>at</strong> loc<strong>at</strong>ed 6 to 8 km from shore, and sampled along two arcs about 10 to 12<br />
km long. <strong>The</strong> first arc is ½ km to 1 km from the shoreline and the second arc is about<br />
7 km from the shoreline. Evalu<strong>at</strong>ion of OCD4 with this d<strong>at</strong>aset focused on the onehour<br />
average concentr<strong>at</strong>ions measured close the shoreline in Arc 1.<br />
Meteorological d<strong>at</strong>a used in the OCD4 evalu<strong>at</strong>ion d<strong>at</strong>aset includes wind <strong>at</strong> 20.5m,<br />
temper<strong>at</strong>ure <strong>at</strong> 7m, and air-sea temper<strong>at</strong>ure difference measured <strong>at</strong> the release<br />
loc<strong>at</strong>ion, and vertical temper<strong>at</strong>ure gradient measured over the w<strong>at</strong>er by an aircraft.<br />
Final Report Vol.1 42