In the beer world the malt supplies some, and is supplemented with calcium chloride or calcium sulphate (gypsum), depending on which anion is wanted - the ratio of chloride to sulphate changes the expression of bitterness in beer. I don't know how mead people approach the problem, I suspect just by using strains that drop well.
Yep, you get everything from British cask strains which drop before they've even finished fermenting, to hefe yeast that never drop at all, and everything in between - a typical brewery yeast may have several strains with different floccing behaviour, Guinness has at least four from memory. But if you have a mix then the good floccers will take the poor floccers down with them.
Looking very quickly at Texas geology, it looks like the Edwards aquifer around Austin is very limestone-y so calcium rich, whereas from what I can tell the Ogallala aquifer to the east is far less so. Again, I don't know how mead people approach these things.
There's two aspects, at least from a beer POV. There's chill haze, which is protein that precipitates (but doesn't settle) to form a haze at low temperatures, and then redissolves once it warms up. There's also using cold to help drop out the yeast, which is more of a one-way thing as long as you don't stir it up afterwards.