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Nonclassical cold-frontal structure caused by dry subcloud air in northern Utah during the Intermountain Precipitation Experiment (IPEX)

Mardi, 19 avril, 2005 11:00
Pavillon Burnside 805, rue Sherbrooke Ouest, Montréal, QC, H3A 0B9, CA
Dr David Schultz, Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma and NOAA/National Severe Storms Laboratory (candidat au reecrutement de professeurs du SST).
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