4A.4 The Curious Case of Sunrise Snow

Tuesday, 8 January 2019: 9:15 AM
North 131C (Phoenix Convention Center - West and North Buildings)
Kimberly L. Elmore, CIMMS/Univ. of Oklahoma and NOAA/NSSL, Norman, OK; and M. E. Baldwin, A. Gerard, and H. D. Reeves

Recently, a cursory perusal over five years of Meteorological Phenomena Identification Near the Ground (mPING)precipitation-type data over the months spanning November through March revealed an increase in the proportion of snow observations around local sunrise. The higher rate of snow observations lasts 3-4 h and then decreases. Dubious of this, ASOS observations over the same period are examined and show a similar characteristic. Finally, we examine RAP 1 h precipitation type forecasts and also see the same signal. This paper examines these characteristics in some detail and further refines their observational characteristics, while examining possible explanations.
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