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Last modified
7/28/2009 2:40:44 PM
Creation date
4/24/2008 2:54:45 PM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
6-07-DR-20020
Project Name
Sierra Cooperative Pilot Project
Title
Satelite Studies During the 1976-77, 1977-78 Sierra Cooperative Pilot Project
Date
2/1/1979
Weather Modification - Doc Type
Report
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<br />ABSTRACT <br /> <br />~ <br /> <br />SATELLITE STUDIES DURING THE 1976~77 AND <br />1977-78 SIERRA COOPERATIVE PILOT PROGRAM <br /> <br />~ <br />. <br /> <br />Digital imagery from the SMS~2 geostationary satellite was recorded <br /> <br />for analysis in support of the Sierra Cooperative Pilot Project. <br /> <br />Imagery of five storms during the 1976-77 and 1977-78 seasons of the <br /> <br />project have been analyzed in detail using the CSU ADVISAR. Temporal <br /> <br />variations ~n cloud top temperature were charted and synoptic and meso- <br /> <br />scale cloud features have been studied. <br /> <br />Results show the highest precipitation and lowest cloud top tempera- <br /> <br />o <br />tures, below -35 C, occur about one or two hours ahead of the surface <br /> <br />cold front within the frontal band. Following the frontal passage, an <br /> <br />unstable convective orographic cloud remains over the Sierra for up to <br /> <br />~~ <br /> <br />8 hours, with cloud top temperatures around -lSoC, well within the <br /> <br />*~ <br /> <br />seeding window range. <br /> <br />Mesoscale features including banded and cellular convection and <br /> <br />cloud streets have been observed by the satellite, with their effects <br /> <br />often showing up in the precipitation gage records. Large convective <br /> <br />lines and cells were tracked onshore and were found to move with the <br /> <br />winds somewhat below the 50 kPa level. Cells intensify in the Central <br /> <br />Valley of California, usually dissipating as they climb the Sierra. <br /> <br />Trajectories of large cells curve to the left upon encountering the <br /> <br />foothills, becoming nearly parallel to the mountains under certain <br /> <br />conditions. <br /> <br />Precipitation is greatest on the west slopes of the Sierra due to <br /> <br />~ <br /> <br />the orographic effect. Lee-side precipitation appears to be dependent <br /> <br />on the presence of high, cold cloud tops which lead to precipitation <br /> <br />. <br /> <br />particles being carried over the crest. <br /> <br />i <br />
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