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Last modified
7/28/2009 2:33:47 PM
Creation date
3/5/2008 10:45:43 AM
Metadata
Fields
Template:
Weather Modification
Title
1994 Field Operation Plan
Date
1/1/1994
State
UT
Weather Modification - Doc Type
Report
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<br />3. 1994 FACILITIES AND INSTRUMENTATION <br /> <br />3.1 Seeding Sites <br /> <br />Two high-altitude seeding sites will be used. One will be the HAS (High Altitude Site) used in 1991 at an <br />elevation of 2500 m. The other seeding site will be the AHS (Aspen Hills Site) about 5 km south of HAS at <br />2350 m elevation. Each site will be equipped with a Desert Research Institute (DRI) remote-controlled AgI <br />generator, a remote-controlled propane dispenser and a remote-controlled mass flow controller for <br />dispensing SF6 tracer gas. Each site will have automatic measurements of wind speed, direction, air <br />temperature and relative humidity. The HAS will be equipped with a Rosemount icing detector for SLW <br />observations. These and other sites to be mentioned are shown on Fig. 1. <br /> <br />Three valley AgI generators will be used during some T &D experiments. They will be located by NA WC <br />(North American Weather Consultants), the firm which conducts the Utah operational seeding program. <br />NA WC will site these generators with the intention of targeting the "upwind highway" where Plateau-top <br />sampling of AgI will be concentrated. The upwind highway refers to that portion of Highway 31 which <br />parallels the west edge of the Plateau top. It extends from the intersection of Highways 31 and 264 to the <br />RRS site 6.5 km further south. <br /> <br />Simulated seeding will be conducted by releasing SF 6 gas from the mouth of Birch Creek Canyon during <br />some experiments. The specific release site is not shown on Fig. 1, but it will be near the 2000 m contour <br />about 2.5 km east of the Project H.Q. This site was used a few times during the 1991 program. Some <br />nighttime (non-aircraft) investigations of AgI releases from this site may be conducted. <br /> <br />3.2 Cloud Physics Aircraft <br /> <br />The instrumented NOAA King Air C-9Q aircraft used in 1991 will again be available. The aircraft will be <br />equipped to monitor ice particles (2D-C probe), cloud droplets (FSSP probe), AgI (NCAR IN counter), SF6 <br />gas concentration (fast-response analyzer), horizontal position (GPS and Loran-C), liquid water content <br />(King probe) and state parameters. Horizontal winds will be calculated from some of these measurements. <br />The aircraft will be based at the Provo Airport about 75 km northwest of RRS. <br /> <br />A special Federal Aviation Administration waiver has been requested for 1994 to permit in-cloud, IFR <br />(instrument flight rules) sampling to within 300 m of the highest terrain within 8 km of the flight path (the <br />normal vertical restriction is 600 m). Aircraft sampling during 1991 was done under such a waiver. This <br />low-level sampling will allow measurements of ground-released plumes near the mountainous terrain. The <br />aircraft would often be unable to penetrate the ground-released plumes with normal vertical terrain <br />separation. <br /> <br />3.3 Instrumented Van <br /> <br />An instrumented four-wheel drive 3/4 ton van will be equipped to monitor ice particles with a vane-mounted <br />2D-C probe above the van which will keep the probe pointed into the resultant wind. A nearby anemometer <br />will measure wind speed to determine the 2D-C's strobe rate. Silver iodide IN will be measured with an <br />NCAR acoustical ice nucleus counter (hereafter NCAR IN counter) and SF6 gas with a fast-response <br />analyzer. Other van measurements will include horizontal position with a GPS, air temperature, relative <br />humidity and pressure. An aircraft-type Rosemount icing detector will monitor the presence of SLW. <br /> <br />The concept of using a vane-mounted 2D-C probe was briefly tested in 1991. However, a head-on collision <br />rendered the probe inoperable for most of the field season. While only limited 2D-C observations were <br />obtained along the upwind highway, they showed the concept was practical. It is expected that wind-blown <br />snow will contaminate measurements of falling ice particles along windier portions of the highway. The <br />extent of this potential problem must be determined by experience. <br /> <br />4 <br /> <br />
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