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Last modified
7/28/2009 2:33:58 PM
Creation date
3/5/2008 10:53:13 AM
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Weather Modification
Title
Summary of the NOAA/Utah Atmospheric Modification Program: 1990-1996
Date
9/1/1998
State
UT
Weather Modification - Doc Type
Report
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<br />1.2 Objectives and Research Reported <br /> <br />The research reported herein is based on the last several years of the NOAAlUtah AMP when field work <br />'was conducted on the Wasatch Plateau (hereafter Plateau) of central Utah, approximately between the <br />towns of Fairview and Price. Earlier work was conducted on the Tushar Mountains of southern Utah. <br />That work, which has its own body of publications (e.g., Huggins and Sassen 1990), is not discussed in <br />this report. The single exception is the paper by Sassen and Zhao (1993), which is quite relevant to the <br />Plateau findings and was published during the Plateau phase. A review of the earlier years of NOAA <br />AMP work, with an extensive list of references, is given by Reinking (1992). <br /> <br />The NOAAlUtah AMP had two main objectives. First, the program was designed to physically evaluate <br />the effectiveness oftheUtah operational seeding program which has been partially funded by the State of <br />Utah. Second, the program was to recommend to the Utah Division of Water Resources any changes <br />which might improve future effectiveness of the operational seeding program., The operational <br />program's goal was to increase the high mountain snowpack, which should lead to springand summer <br />-streamflow augmentation (Super and McPartland 1993). Numerous findings and recommendations <br />which could improve the operational program are to be found in the articles and papers summarized <br />herein. Any decisions to implement such recommendations are the responsibility of the Utah Division of <br />Water Resources and cooperating local water management agencies which jointly fund the operational <br />program. <br /> <br />1.3 Problems with Statistical Evaluations <br /> <br />Three statistical evaluations of the operational program have been reported by Thompson and Griffith <br />(1981), Griffith et al. (1991), and recently by Griffith et al. (1997). The reader is referred to these same <br />articles for details of the operational program which used valley-basedAgI generators, typically spaced <br />on the order of 16km apart (Griffith 1996). A small minority of all generators were sited in or ~ear <br />canyon mouths which could help transport and dispersion over mountainous terrain. <br /> <br />While all three of the statistical evaluations have suggested seasonal snowfall increases in the <br />10-20 percent range, one should be very cautious about accepting such indications. Griffith et al. (1997) <br />correctly point out that their (statistical) techniques, "are not as rigorous or scientifically acceptable as is <br />the randomization technique used in research." A sizeable body of literature exists which discusses the <br />many difficulties of after-the-fact statistical analysis of operational seedirig programs and why such <br />attempts should be viewed with caution. Dennis (1980) and Gabriel (1981) discusses some of the <br />problems that can result from improperly applied statistical approaches. Most of these arguments will <br />not be repeated here. However, a major problem is the lack of any randomization with operational <br />seeding programs, considered by many statisticians and meteorologists as essential for valid statistical <br />testing. Target-control analysis of the type applied to'Utah's operational seeding program must assume <br />that precipitation relationships are stable over decades. This assumption presents a major difficulty <br />(Dennis 1980). In the Utah analyses, these relationships are assumed stable over long distances, from <br />central and southern Utah target gages well into Nevada and Arizonawhere control gages were selected. <br />But it is well known that precipitation relationships can change over time and space for a variety of <br />reasons ranging from large scale climatic changes (e.g., EI Nino) to local changes in the environment of a <br />precipitation gage (e.g., growth of vegetation affecting gage catch). <br /> <br />The three analyses cited above were done by the company hired to conduct the operational seeding. <br />While it is common practice for cloud seeding operators to analyze their programs, statisticians have <br />pointed out that this approach can leadto bias, favoring positive results. Dennis (1980) discusses a <br /> <br />2 <br />
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