Abstract
The 1995 Arizona Program was a field experiment aimed at advancing the understanding of winter storm development in a mountainous region of central Arizona. From 15 January through 15 March 1995, a wide variety of instrumentation was operated in and around the Verde Valley southwest of Flagstaff, Arizona. These instruments included two Doppler dual-polarization radars, an instrumented airplane, a lidar, microwave and infrared radiometers, an acoustic sounder, and other surface-based facilities. Twenty-nine scientists from eight institutions took part in the program. Of special interest was the interaction of topographically induced, storm-embedded gravity waves with ambient upslope flow. It is hypothesized that these waves serve to augment the upslope-forced precipitation that falls on the mountain ridges. A major thrust of the program was to compare the observations of these winter storms to those predicted with the Clark-NCAR 3D, nonhydrostatic numerical model.
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CITATION STYLE
Klimowski, B. A., Becker, R., Betterton, E. A., Bruintjes, R., Clark, T. L., Hall, W. D., … Uttal, T. (1998). The 1995 Arizona Program: Toward a Better Understanding of Winter Storm Precipitation Development in Mountainous Terrain. Bulletin of the American Meteorological Society, 79(5), 799–813. https://doi.org/10.1175/1520-0477(1998)079<0799:TAPTAB>2.0.CO;2
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