Karen Politte
EF5
What if a "gustnado" (horrible term - use eddy-whirlwind instead!) forms along the leading edge of the RFD, and then gets spun-up?
I always thought that GUSTnadoes - by their very name - only formed on the leading edge of a gust front. That is how they are characterized - as ground-level eddies that form on the leading edge of outflow from a thunderstorm. Given this description - I don't think that true gustnadoes can be confused with vortices that form on an RFD boundary but I don't know how to categorize the latter, either.
I guess my problem is that for gustnadoes to form they have to be on a gust front - and if they are on a gust front that precludes any tornadic/tornado possibilities as the parent storm has probably already been undercut and is a big windy mess.
Landspouts and waterspouts must fall under the heading of tornadoes according to the NWS definition of the term because they are underneath a cumuliform cloud. As this is the only "official" definition of the word TORnado - there is a pretty large catchment area for what is considered a tornado.
Therein lies one of our problems in defining these phenomena. Due to the official definition being so broad, there is a necessity to "split up" what is considered a tornado into many smaller categories - hence landspout, waterspout, tornado, non-mesocyclonic tornado, non-supercell tornado etc. etc. I think so far the handiest category for me has proved to be tornado vs. non-mesocyclonic tornado - as both can be and have been formed by tornadic supercells.
KL