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WMOD00284
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Last modified
7/28/2009 2:32:39 PM
Creation date
1/8/2008 12:16:50 PM
Metadata
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Template:
Weather Modification
Applicant
Thompson, J.R., G.W. Wilderson, and D.A. Griffith, North American Weather Consultants
Sponsor Name
USBR
Title
Cloud Seeding Data Collection, and Analysis Assoc. with the Colo River Augmentation Demonstration Program
Prepared For
USBR, Divison of Atmospheric Research
Prepared By
Thompson, Wilderson, Griffith
Date
12/1/1987
State
AZ
Weather Modification - Doc Type
Scientific Study
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<br />each of the eight SF6 flights and these can be found ln the <br />individual discussions of each test case. <br /> <br />The primary data reduction effort was directed toward <br />the raw SF6 data. In particular, software was written to <br />remove baseline drift from the analyzer output and also to <br />filter out short term noise. Typically the output signal <br />would drop with increasing altitude and remain fairly constant <br />while flying level, Therefore a program was written to adjust <br />the SF6 data to a baseline which corresponded to a zero reading, <br />and to remove erroneous noise generated by small changes in <br />cabin pressure or by rapid acceleration. Once a baseline <br />had been established a correction equation was applied to <br />the raw data to convert analyzer output (volts) to concentration <br />in parts per trillion (ppt). These correction equations were <br />obtained from the pre- and postflight calibrations (Table <br />4-5). For this report delta-h (height of SF6 plume above <br />release elevation) values for individual plumes were hand <br />extracted from the data. An example of the baseline correction <br />is shown in Figure 4.5. Note that the baseline is smooth after <br />the correction and that the y-axis is portrayed in units of <br />concentration instead of voltage. <br /> <br />When rUnnlng the raw SF6 data through the software a <br />minimum concentration value was used to search for the occurrence <br />of a SF6 plume. Typically a value of 10 ppt was chosen since <br />the noise of the analyzer ran around 5 ppt. Therefore plume <br />widths were calculated with the baseline set at 10 ppt. Plume <br />widths were calculated from the times the 10 ppt limit was <br />exceeded and the true air speed of the aircraft. Corrections <br />were made to these calculations when the aircraft transect <br /> <br />4-14 <br /> <br /> <br />I <br />I <br />f <br />I <br />'I <br />I <br />, <br />I <br />, <br />I <br />J <br />I <br />f <br />,I <br /> <br />I <br />I <br />I <br />I <br />, <br /> <br />
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