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Last modified
7/28/2009 2:35:09 PM
Creation date
3/11/2008 11:22:19 AM
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Template:
Weather Modification
Title
1991 Final Report of Desert Research Institute Field Operations, Data Collections and Data Processing
Prepared For
Utah Department of Natural Resources Division of Water Resources
Prepared By
Arlen W. Huggins
Date
8/1/1991
State
UT
Weather Modification - Doc Type
Report
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<br />radiating temperature of the atmosphere at 20 and 30 GHz are determined from a <br /> <br />set of radiosondes that encompass the period of radiometer data. The entire set <br /> <br />of 1991 Mt. Pleasant soundings will be used for these calculations. Real time <br /> <br /> <br />measurements during the 1991 season were made using a set of retrieval <br /> <br />coefficients derived from a set of 1987 soundings taken from Beaver, Utah. Data <br /> <br />for 1991 will be archived only after the new coefficients are applied to the raw <br />data. <br /> <br />For mobile radiometer data, it will likely be necessary to apply an <br /> <br />........-~-"-~-.~.....--- <br /> <br />adaptive retrieval relationship to the data. This is due to the fact that <br /> <br /> <br />altitude changes were typical along the radiometer routes and the retrieval <br /> <br /> <br />relationships can be expected to change with altitude. In fact, the baseline <br /> <br />values of liquid and vapor were observed to drift with the changes in altitude <br /> <br /> <br />when a constant set of coefficients was used. Figure 9 demonstrates this effect <br /> <br />during a traverse of Route 1 on 28 February 1991. No liquid existed in the <br /> <br />clouds over the Plateau from 0830 to 0915 as the radiometer descended from the <br /> <br />DOT site to the valley, yet the liquid depth baseline increased from about .05 <br />mm at the top of the Plateau to .15 mm at the bottom of the Plateau. Vapor depth <br />also increased, but much of the change in vapor can be attributed to an increase <br />in microwave emission from additional moisture in the lowest layer of the <br />atmosphere. Retrieval coefficients from the 1991 soundings will be processed <br /> <br />using the surface and numerous levels above the surface as the base level. From <br /> <br />this multiple set of coefficients an altitude-dependent relationship will be <br />determined and applied to the raw data. <br /> <br />D. Ka-band Radar Maintenance <br />The Utah Ka-band radar was maintained during the 1991 Field Program by DRI <br /> <br />20 <br /> <br />I <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 />
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