As stated two pages earlier, after about 9:00 p.m. (2100 MDT) rain rates increased substantially.   We also noted that most of the heaviest rain fell during the last part of the event.   It turns out that the main activity seemed to become "locked-in" over the Spring Creek and Canal Importation drainage basins at this time.   Click here to view a loop of rainfall accumulations (summed every 15-min) which was computed from polarmetrically calibrated Doppler radar at CSU's CHILL radar located in Greeley, Colorado   for the period 0216 - 0400 UTC.

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