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Last modified
7/28/2009 2:28:24 PM
Creation date
10/1/2006 2:14:58 PM
Metadata
Fields
Template:
Weather Modification
Project Name
Annual Report
Title
Seeding Operations & Atmospheric Research, 2005 Annual Report
Prepared By
Duncan Axisia
Date
12/31/2005
Weather Modification - Doc Type
Report
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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />effect on precipitation development through <br />either of two distinct mechanisms: <br /> <br />1. introduction of embryos on which <br />raindrops form: or <br />2. broadening of the initial droplet sIZe <br />distribution resulting in acceleration of all <br />stages of the coalescence process. <br /> <br />In 1990. G. Mather reported a case of <br />inadvertent seeding of douds by hygrosa:>pic <br />partides emitted from a Kraft paper mill in <br />South Africa This observation led to further <br />doud seeding experiments in South Africa <br />(Mather et at.. 1997), Mexico (Bruinljes, 1999) <br />and in Thailand (Silverman, 2002) with highly <br />encouraging results. <br /> <br />Planned research with hygroscopic seeding in <br />Texas was conducted in 2005 utilizing the <br />SOAR research aircraft and its O"ew. Prof. <br />Daniel Rosenfeld and Dr. William Woodley <br />identified a patented means of processing <br />common salt (NaCI) to virtually any desired <br />size as verified after production by analysis <br />with an electron microscope (Figure 11). A <br />desiccant was added to the salt powder during <br />its production to prevent its dumping. The <br />mcx:lel simulations of Segal et al. (2004) <br />indicated that 3 to 5 microns diameter would be <br />the optimal size range and partides of this size <br />were produced for initial experiments to be <br />conducted in Texas (SPECTRA II). <br /> <br />Inadvertent anthropogenic seeding <br />and its implications for operational <br />cloud seeding <br /> <br />Studies conducted by Rosenfeld (1999.2000) <br />using satellite data reveal qualitative evidence <br />suggesting that industrial plumes change the <br />composition of CCN in sum a way as to have <br />an adverse effect on precipitation processes <br />downwind of industrial centers. A later study <br />by Boryn (2003) would lend credence to these <br />findings by quantifying decreases of up to 50% <br />in orographic snowfall rates over Colorado due <br />to the addition of tiny anthropogenic sulfate <br />aerosols. Building off of Boryo's work, Givati <br />and Rosenfeld (2004) constructed trend <br />analyses of rain gauges downwind of industrial <br />centers in Califomia and Israel to ascertain the <br />effect of concentrated plumes of tiny CCN on <br /> <br />. <br />, <br />. <br /> <br />orographic precipitation formation. After <br />comparing the long-range trends of rainfall <br />upwind of the mountainous regions to rain <br />gauge trends in situ of orographicaUy favored <br />regions for precipitation it was found that <br />regions along the coast experienced static to <br />even positive trends in precipitation whereas <br />those regions downwind of industrial centers <br />experienced negative trends. During the same <br />time period. it was found that although air <br />pollution is decreasing in these regions, the <br />production of very small CCN is increasing due <br />to factors such as greater diesel consumption <br />among others Further substantiating the <br />causative evidence is the observation that no <br />such difference in rainfall trends were seen in <br />high elevation rain gauge data downwind of <br />pristine areas devoid of large industrial centers. <br /> <br />The implications for these results are of great <br />importance in regards to the question of <br />operational doud seeding and its viability. <br />These results qualitatively and quantitatively <br />illustrate the ability of anthropogenic sources to <br />inadvertently modify the weather in such a way <br />as to distort natural precipitation processes in a <br />statistically significant manner. In his review on <br />the current state of weather modification <br />Roland List (2004) states: <br /> <br />Weather mcxJification Vv'C:tks beyond any doubl Ndxxty <br />else but nature itself is doing weather mcxJification on a <br />grand scale: c:kuds and cloud systems, unable to yield <br />rain over con~nents due to heavy loads of small-sized <br />cloud coodensabon nuclei (CCN; many prtxluced by <br />bi<rnass burning) are revitalized, while moving back over <br />!he oreans, by !he ingestion of sea sa~ nudei, and can <br />yield rain again {Rosenfeld (2003), confirmed by R. <br />Bruinljes (2003. pe=la1 COf1'mJnicaIiooII. <br /> <br />Therefore. the use of anthropogenic material in <br />a deliberate manner to augment precipitation <br />processes remains a viable altemative to other <br />water conservation efforts. [n addition. these <br />studies reveal the need for operational seeding <br />programs to have an understanding of typical <br />CCN sizes and concentrations in their <br />respective water districts so as to deliver <br />scientifically sound treatments of CCN to <br />clouds for rainfall augmentation. <br /> <br />18 <br />
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