Larry J. Kosch
From time to time I hear storm chasers and nowcasters talk about CAPE. Just what is CAPE?? And how does this figure into the chaos of severe weather forcasting?? Thanks. LJK.
Originally posted by Joe Nield
low topped tornadic supercells
See Jon Davies' excellent case study of this event for more:
Originally posted by Glen Romine+--><div class='quotetop'>QUOTE(Glen Romine)</div><!--QuoteBegin-Joe Nieldlow topped tornadic supercells
See Jon Davies' excellent case study of this event for more:
I would disagree that this is a good case to consider as a benchmark for low-topped supercells. This event really doesn't fit the mold, and I don't think this particular analysis is some of Jon's best work - though his case studies are generally top-notch. I think this link of his is more typical of the types of mini-supercell tornado events most often observed in the plains.
http://members.cox.net/jdavies1/041803cne/...e/041803cne.htm
Glen[/b]
More accurate for what?
I re-ask my original question: What do you forecast differently with a CAPE of 3,250 versus 3,000? Especially (in the real world) if you were to launch a rawinsonde in the same airmass at the same time 20 miles away, the CAPE might vary by 1000 j?