I recall Combs saying that on the West Coast, they figure an average of 10% strays in any system, sort of a natural fail safe system. If all the fish returned to their natal streams and you get a Mt St Helen's event like on the Cowlitz, you would never get another run without the dribs and drabs from other systems, also maintains genetic diversity.
I got called for spot burning a couple of years ago and last fall as well, so I'm not using "real" stream names anymore except for big rivers. Suffice it to say that everything from step a crossers like Mustela creek to the Genny, Black and Niagara, gets a fish now and then. And some have natural reproduction documented back to mid 20th century rainbow plantings way before the current program. Certainly water temperature is a huge limiting factor for recruitment (fish attaining a size that allows them to be a part of the fishery), but the eggs have to hatch out to fry, and what Mike C was saying is that a lot of the streams have limited substrate of the right size for the number of fish that come into spawn. If Pair B spawns where Pair A spawned last week, a lot of Pair A's eggs are wiped out by Pair B. And Kings need the bigger, rounder stones, areas of which are limited in these shale bottomed streams that were stripped of a lot of cobble over the last 200 years for building all those beautiful cobblestone houses we see in WNY (and yes a lot of those were also picked up from fields after frost heaving from the winter, but the ease of gravel harvesting from streams is well known, part of the reason for Article 15 of ECL). Low flow is also a function of shade removal, but it is related to conversion of the whole watershed to greater amounts of impervious cover, rooftops, parking lots, roadways, etc, that cut off percolation to groundwater and route runoff directly to streams in rainstorms, causing higher highs, lower lows and shorter duration to the " events", what is called greater flashiness in the stream, instead of the aboriginal forested condition where a lot of water gets held in the leaf canopy and slowly reaches the ground and mainly infiltrates to groundwater, keeping flows between storms higher and cooler. definitely what has happened in IC over the last 30 years. Also, the silt at Russo may come from development upstream and settle at Russo due to lower gradient. Eliminate the source of sediment upstream in the PM area (and at places like the old Sheafer Landfill in Ontario County), and the stream will gradually clean itself in the depositional places downstream. This is also evident in the areas below Philbrick since the wall got built.
I think I am in the run-on sentence competition!
L13