Kevin Walter
EF1
I'm bored right now, so I want to throw out something I've been pondering for some time. When we all look at surface maps, we often note high temperature/dewpoint spreads and can sometimes disregard an environment as one that would exhibit "too high of an LCL for tornadogenesis". However, in a typical setup for supercells and tornadoes, you have wind shear, which means the anvil will be blown off out ahead of the storm, providing some "shade" for the air east of the storm that will later become the storm's inflow. Thus, in a storm-local sense, you may have surface conditions of 73 over 65, rather than 90 over 65 like all the "synoptic" observing networks in the region (ASOS) are reporting (the obs we're using to make our assumptions). It would be interesting to go back and look at some of the mobile mesonet temperature and humidity trends we took here at TTU in our storm intercepts this year to look into this.
Just throwing this out, feel free to comment at will.
Just throwing this out, feel free to comment at will.