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<br />I <br /> <br />12 <br /> <br />I <br /> <br />From a single station analysis of the Durango rawinsonde data and the <br /> <br />I <br /> <br />mesoscale streamline analysis of the E.G. & G. surface synoptic winds it was <br /> <br />possible to synthesize a detailed picture of the storm structure and its <br /> <br />I <br /> <br />sequence. From the standard National Weather Service data it was possible <br /> <br />I <br /> <br />to understand the San Juan storms in relation to the macroscale dynamics. <br /> <br />. <br />The microscale characteristics of the individual storms were discerned from <br /> <br />I <br /> <br />the aircraft and ground data. <br /> <br />I <br /> <br />III. Su}fr~RY OF ~~JOR RESULTS AND CONCLUSIONS <br /> <br />I <br /> <br />A sunnnary of the major results and conclusions drm\ln from these studies <br /> <br />will be presented in this section. The major analysis effort was concentrated <br /> <br />I <br /> <br />on the storms studied and flights made during the 1974-75 \\linter season. One <br /> <br />flight \.]as made in 1973 and three storms were flOlm in 1974. Since in <br /> <br />I <br /> <br />December 1974 the \;lyoming Q/A was neHly equipped \<lith a rather complete com- <br /> <br />I <br /> <br />pliment of cloud physics equipment and a Doppler system for horizontal winds <br /> <br />and the NCAR QI A was ne'ivly equipped 'i-lith an inertial navigation system in <br /> <br />I <br /> <br />January 1975 and a ne\\lly installed air sensing probe in March 1975, it <br /> <br />seemed appropriate that the analysis concentrate on these quality data. <br /> <br />'I <br /> <br />Each storm studied and flight made over Wolf Creek Pass during the 1974-75 <br /> <br />I <br /> <br />season is described in detail in Section V. This is not to imply that the <br /> <br />storms and flights made in 1973 and 1974 were ignored. Indeed, the results <br /> <br />I <br /> <br />and conclusions presented in this section are consistent with the earlier <br /> <br />data but the earlier data were not as complete and therefore could not <br /> <br />I <br /> <br />support the results and conclusions so well. <br /> <br />I <br /> <br />I <br /> <br />I <br />