jiharris0220
Member
The MCS will create a boundary of very enhanced SRH and surface vorticity where unstable air can pile up onto.
The tail end of the MCS seems like it will break up and actually become discrete supercells that will take advantage of this enhanced environment along with OWS supercells that also ride the same boundary.
To the south, along the dryline, shear magnitude is lower but these storms will be even more discrete and have a very broad warm sector to take advantage of.
The tail end of the MCS seems like it will break up and actually become discrete supercells that will take advantage of this enhanced environment along with OWS supercells that also ride the same boundary.
To the south, along the dryline, shear magnitude is lower but these storms will be even more discrete and have a very broad warm sector to take advantage of.