The black dots on the hodograph as well as dashed horizontal gray lines on the skew T–log p diagram represent 1-km height increments up to 10 km. (2000), and the green dot indicates the CM1 grid motion to keep the storm centered. The red dot on the hodograph indicates storm motion calculated by the method of Bunkers et al. The virtual temperature profile is in purple. The modified sounding that was used as the CM1 base-state is depicted in solid lines on the skew T–log p (red and green) and hodograph (black). The observed temperature and dewpoint traces are dashed red and green lines, respectively, and the observed wind profile is a dashed blue line on the hodograph. Skew T–log p diagram of NSSL’s Probe 1 observed sounding east of Cheyenne, WY, in the preconvective environment at 1930 UTC.
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