On San Francisco Bay, we'd call them FLEBBS, we made that up or got it from Latitiude 38 or Kimball's Sailing The Bay book, where the flood met the ebb. But there were only 6 feet of normal tidal range. Up your way, druid, you're dealing with 14 foot tidal differences, so when the incoming meets the outgoing there are larger differences. You're also talking about two different things here: ebb meets flood vs. wind again water. The latter can occur in the same place on different tide directions with different wind directions. Of course, your third is when river outflows meet tidal streams, but those are only bores in the river entrances, not out to sea. The Columbia River is infamous for setting up just these conditions on big ebb periods.
Names? Heck, I dunno, but I'm sure some research would turn 'em up.