The mountains do wonders for these things, in a bad way if you need rain!![]()
Not necessarily, afternoon lee trough on eastern mountains can sometimes help to redevelop/trigger convection with a pattern dominated by a 500mb ridge, especially old boundaries left over, normally you get large amounts of CAPE but such little triggering in these setups along with some Capping which is why there’s flat cumulus most of the time in summer days, outflow boundary can easily break that, especially in a THETA-E ridge, and plus the MCS/outflow boundary isn’t coming from the west, but more from the north/northwest