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Last modified
7/28/2009 2:39:04 PM
Creation date
4/18/2008 10:00:07 AM
Metadata
Fields
Template:
Weather Modification
Title
Desert Research Institute Fields Operations - 1994 NOAA/UTAH Field Program - Final Report
Date
11/1/1994
Weather Modification - Doc Type
Report
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<br /> Table 3. Summary of 1994 NOAAlUtah Mobile Radiometer Operations <br />DATE TIME PERIOD (MST) OPERATION DESCRIPTION <br />7 February 0900 - 1100 Stationary @ TAR; LW = 0.0-0.6mm; some graupnl <br /> showers; _50 <br /> 1100-1148 TAR to RRS; LW about 0.5mm; _50 at RRS <br /> 1208 - 1245 RRS to FVW; LW = 0.4-0.6mm; +20 at FVW <br /> 1246 - 1335 FVW to RRS; LW decreased to 0.05mm <br /> 1335 - 1443 RRS to HO; occasional S-/S-- on the way down <br />8 February 0737 - 0830 HO to Mile 13; LW = 0.05-0.50; S- to S <br /> 0900 - 1000 Mile 13 to TAR; LW = 0.0-0.2; mainly So; _60 at TAR <br /> 1011 - 1125 TAR to FVW; up to 0.6mm LW near mile 6 <br /> 1141 - 1221 FVW to Mile 11; 0.06-0.40mm LW <br /> 1221 - 1304 Mile 11 to HO; less than 0.25mm LW <br />9 February Computer and NO converter malfunction <br />11 February Radiometer returned to Reno, NV for repair <br />4 March Radiometer back at HO <br />5 March 1345 - 1445 HO to RRS <br /> 1447 - 1715 1-min data at RRS for comparison with USBR <br /> radiometer <br /> 1715 - 1815 RRS to HO <br />10 March 1038 - 1222 Data collection at MPA for comparison with sounding <br /> (1120-1215) <br />11 March 0557 - 0700 HO to RRS; LW less than 0.05mm <br /> 0700 - 0745 Stationary at RRS <br /> 0747 - 0841 RRS to Scofield; very little LW <br /> 0851 - 1001 Scofield to HO; no LW <br /> 1200 - 2000 Thunderstorms in afternoon; rain with SE flow <br />16 March 0740 - 1413 HO to Ely, NV; Bkn AISt/Ci; V=0.8-1.0cm <br /> 1430 - 1931 Ely, NV to 30 mi. east of Fallon, NV; thick AICu between <br /> Austin, NV and this point; LW>OAmm <br /> 2047 - 2300 30 mi. east of Fallon to Stead, NV <br /> <br />13 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I' <br />I <br />I <br />I <br />'I <br />I <br />I <br />I <br />I <br />
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