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<br />USE OF METEOROLOGICAL SATELLITE DATA FOR THE DESIGN, <br />OPERATION AND EVALUATION OF WEATHER MODIFICATION EXPERIMENTS <br /> <br />by <br /> <br />(*) <br />T. H. Vander Haar <br /> <br />I . I NTRODUCT I ON <br /> <br />I. I In 1979 the worl dw i de ava i lab i I i ty of high reso I uti on geostati onary sate II i te data <br />is affecting weather forecasting and research in significant ways. Coupled with second <br />and third generation systems of near-polar orbiting satel I ites, the new World Weather <br />Watch network provides special opportunities for weather modification programs. The pur- <br />pose of this training paper is to describe the use of meteorological satel lite data for <br />the design, operation and "post-hoc" evaluation of weather modification experiments. <br /> <br />1.2 The paper refers to other, more len~lthy summaries with thei r sets of references. <br />It outl ines the sate) I ite observing systems of the early 1980's and refers to the basic <br />facts needed to use satel I ite data. In addition, statements and examples are used to <br />describe the various classes of hardware and computer software avai lable to display and <br />analyze the satell ite data. Examples Gf actual satell ite cloud cl imatologies are provided <br />as they were used in the design of weather modification experiments. Sample case studies <br />of satel I ite data illustrate operational applications. Finally, several post-hoe evalua- <br />tions are examined where satel I ite/air~raft and ground-based data are combined. Background <br />for the paper regarding PEP was drawn from PEP Reports I through 9. <br /> <br />2. OVERVIEW OF SATELLITE SUPPORT TO WEATHER MODIFICATION <br /> <br />2.1 Reynolds et E.l. [1978] provide a recent overview including speculation on the <br />future development sate II ite data appl ication possibi I ities. (It is included as ANNEX B <br />to this paper.) Reynolds and Morris [1978] and Morris [1979] describe very recent results <br />us i ng sate II i tes to determ i ne Cloud To,J Temperature (CTT> for seedab i I i ty cr iter i a. The <br />CrT work is based on the physical principles described by Grant and Elliott [1974]. <br />At this time the largest body of results in the I iterature deals, as those noted above. <br />with the use of satel I ites in support of the modification of mid-latitude wintertime <br />orographic cloud systems. <br /> <br />2.2 However, an increasing amount of recent study has been given to the use of cloud <br />climatologies in the design of summertime cumulus weather modification projects (eg. H1PLEX, <br />see Reynolds and Vonder Haar [1976,1977,1978J; other areas, Stadt and Grant [1976]). Real <br />time operational support is addressed by Reynolds and Matthews [1976] . Scheetz and Grant <br />[1976] focused on very low level upslope clouds as viewed from satel lites. <br /> <br />2.3 Purdom [1974] and others have provided extensive discussion of satel I ite support <br />to mesoscale forecasting -- an important aspect of any weather modification project. <br />Griffith et E.l. [1976] , Smith and Kidder [1978], Reynolds and Smith [1978] and others <br />assess the use of satel I ites to determine precipitation amounts. More research is needed <br />but I imited "success" on certain types of cumulus ensembles has been reported. Combined <br />sate I I ite-radar-other data approaches!ook more promising with regard to precipitation <br />determination than either satel I ite or radar or gauge data alone. Hi I Iger and Vonder Haar <br />[1977,1979] report use of satellite tenperature and moisture soundings at the mesoscale <br />to define the environmental conditions before during and after a modification study or event. <br /> <br />* <br />Department of Atmospheric Science, Colorado State University, Fort Collins, Colorado, USA <br />