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Last modified
7/28/2009 2:33:39 PM
Creation date
4/11/2008 3:44:09 PM
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Template:
Weather Modification
Title
Atmospheric Tests of an Organic Nucleant in a Supercooled Fog
Date
12/2/1989
State
CA
Country
United States
Weather Modification - Doc Type
Report
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<br />.J1Y -. <br /> <br />seeding track was normally 3 to 4 km and the flight legs of <br />the cloud physics aircraft within the fog averaged about 1 <br />km either side of the track of the seeder aircraft. <br /> <br />Since the MOLAS effort has demonstrated the <br />reality of APIPs (reports in preparation), both the seeder <br />and monitoring aircraft were flown at relatively low power <br />settings to minimize any possibility that the aircraft <br />themselves would produce ice crystals that might be <br />ascribed erroneously to the organic nucleant. This potential <br />problem is something that must be considered in all future <br />cloud physics studies that make use of aircraft platforms. <br /> <br />The hydrometer q:mcentrations, sizes and habits <br />were determined using three probes manufactured by <br />Particle Measuring Systems, Inc. of Boulder, Colorado, that <br />are flown routinely aboard the University of Wyoming King <br />Air 200T aircraft. These include: a Forward Scattering <br />Spectrometer Probe (FSSP), and OAP-200X (lD-C) and <br />OAP-2D-C (2D-C) probes. The FSSP detects particles up <br />to 30 JLm in size in increments of 2 JLm, the ID-C detects <br />particles up to 187 JLm in diameter in increments of 12.5 <br />JLm, and the 2D-C detects particles up to 500 JLm in <br />intervals of 25 JLm. Water contents within the fog were <br />estimated using Johnson-Williams instrumentation. More <br />informatIOn on the University of Wyoming King Air data <br />system can be obtained by referring to Endsley ~l .aI., <br />(1986). <br /> <br />3. TEST RESULTS <br /> <br />On the day (2 December 1989) of the P. syringae <br />test flights, supercooled fog covered the lake surface and <br />the valley to the east and was banked against the Sierra <br />range to the immediate west (Figure 2). Fog top was 2060 <br />m MSL at a temperature of about -80C. The temperature <br />rose to over + 80C only 500 m above the fog. A partial plot <br />of temperature versus height is provided in Figure 3. <br /> <br />I ... ~..... ..-".... - ~~. <br /> <br />J .... ._: . :~~. <br />r ..... <br />. .. ,.. <br />r_:~t,,-~~- ,.r...I!.......~-.. .I\"~....... <br />1E:~If......._~~:~~ .. ~ 11.'1:""": <br /> <br />r . . ."!jl......... <br />:": .."T."i'~"=- . <br /> <br />-. <br /> <br />~- '.-.-.... <br />..... I. -J . <br /> <br />. . <br />.'tI.. ."'" . <br /> <br />" <br /> <br />I <br /> <br /> <br />Figure 2 Photograph above the supercooled fog <br />over Mono Lake on 1 December 1989. <br /> <br />Temoerature vs Hei?ht over Mono Lake on 2 December 1989 <br /> <br />3500 h <br /> <br />.5 3000 n <br />.i: <br />eL <br />~ 2500-. <br /> <br />... c% <br />~ <br />,,~ <br />J- <br /> <br />2000 n <br /> <br /> <br />-9 .8 -7 ~ -5 -4 -3 -2 -1 0 +1 +2 +3 +4 +5 +6 +7 +l! +9 <br /> <br />T("C) <br /> <br />Ei~.ure 3 Plot of temperature (OC) vs height (m) over Mono Lake on 2 December 191\9. <br /> <br />129 <br />
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