June 8th featured an interesting setup across the high plains. A cold front was expected to extend from a surface low in northern Minnesota through South Dakota and Central Nebraska and intersect a dryline near the Kansas/Colorado Border. Behind the front in Northeastern Colorado, a post-frontal upslope regime with maximized shear was forecast.
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The 26th was the final day of our chase vacation and it was shaping up to be a rather significant weather event across the high plains from Colorado into Western Kansas. Southeasterly return flow across the high plains was expected to advect moisture into eastern Colorado which made that area look like a decent target.
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May 25th featured rather brisk southwesterly flow across the southwest United States permeating into Texas, Oklahoma and Kansas. While at the surface mid 60°F dewpoints stretched into eastern New Mexico. The dryline was rather broad, however we expected that to be the focal point for severe initiation later in the afternoon. The question was where?
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May 24th featured a convectively modified boundary stretching from near Wichita down into the southern Texas Panhandle where it intersected a dryline that extended further south into the Trans-Pecos region of southwest Texas. It was looking like the same area as the day before would have the best chance for severe weather.
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May 23rd featured an expansive enhanced risk of severe weather stretching from Emporia, KS southwest into the southern Texas Panhandle. A stationary front was positioned across Northern Oklahoma into the Texas Panhandle. South of this feature dewpoints into the upper 60s to low 70s was advecting into the area setting the stage for severe weather as MLCAPE values were forecast to reach 3,000 J/Kg.
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