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<br />25 <br /> <br />.- <br />. <br />. <br />. <br />. <br />. <br />.-. <br />., <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />e <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />precipitation estimates are generated every 5 <br />minutes and are accumulated from hours to <br />days to months. <br /> <br />In-situ (in-cloud) measurements <br /> <br />Aircraft in-situ measurements in and around <br />clouds with a state-of-the-art cloud physics <br />aircraft provide an immense amount of data <br />within the micro scale environment of cloud <br />structures. The high sampling frequencies of <br />the most modern airborne instrumentation <br />available and the fast speed of the flying <br />aircraft laboratory provide for a <br />comprehensively detailed data set of the cloud <br />microphysical structure and as it is modified by <br />the surrounding environment through time. In <br />the absence of clouds of sufficient depth, radar <br />and satellite can provide little data on the <br />atmospheric environment. Cloud physics <br />aircraft can actually "touch" the atmospheric <br />moisture as cloud droplet spectrometers, liquid <br />water content sensors and <br />temperature/dewpoint probes measure several <br />variable properties in and around clouds on the <br />mountains and on the plains with no major <br />limitations on the vertical and aerial extent of <br />the measurements other than the terrain and <br />the service ceiling of the aircraft. In-situ <br />observations from aircraft are indispensable for <br />documenting the composition of clouds and <br />providing data for the diagnosis of the <br />processes within them. <br /> <br />SOAR now has the capability to use such <br />instrumentation. These instruments could be <br />used to "look" for a seeding effect (or lack of) in <br />clouds in real time as they occur. Such <br />documentation of seeding effect in the SOAR <br />target area already exists and is documented <br />in a paper by Woodley et. al. (2005) presented <br />at the 16th Conference on Advertent and <br />Inadvertent Weather Modification. <br /> <br />