Here's todays WT-A...
B) Both of These
As spring gives way into summer, cool-air incursions become few and far between, and temperatures in Wichita often soar above 100 deg F. However, this does not mean the end of the storm season, as the plentiful Gulf moisture in the area needs only the appropriate catalysts to trigger powerful thunderstorms. These catalysts can include:
Your Answer: Both of These
Dry lines are low-pressure troughs that travel west to east, and the air behind them is drier (but not cooler) than the air ahead. These incursions of dry air from the Southwest Desert are typically associated with thunderstorm and tornado development further south, in Oklahoma and Texas, but effects are felt in Kansas as well. Thunderstorms generated by daytime heating, on the other hand, are a phenomenon that overspreads much of the US in the summer when sufficient moisture is available. The sun shining on the land produces rising columns of air and cloud development, and the afternoon will see areas of isolated to widespread thunderstorm activity, depending on conditions.
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EZ2, FATS & Larry: D), sorry guys, better luck tomorrow!
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