I recently started a thread on heat events, inspired by all the talk of heat domes in the central and eastern U.S. as of late. While the following is related to heat domes, I thought it was more appropriate to post in here. A side effect of heat domes is the "ring of fire" phenomenon, in which heavy thunderstorms develop along the periphery of a hot air mass. Examples include the "super derecho" in 2012. My gut instinct is that geography gets in the way of "ring of fire"-esque events. The Rockies block moisture from the Gulf of Mexico while the Cascades block surface moisture originating from the monsoon down in Arizona. What's more, there's a lot less 28+ degree water in the Gulf of California and the tropical eastern Pacific, compared to the Gulf of Mexico as can be evidenced by NOAA's SST maps. I think that's why thunderstorms in the western U.S. tend to be dry, and we don't get the kind of drenching storms that they get east of the Rockies. You won't get them unless the source of moisture is something like the remnants of an eastern Pacific hurricane (like 7/20/12), or there's a freak progressive event like 8/6/97, 9/5/13, 8/3-5/99, 6/22/93 or 8/12/14.