Re: Term: "Lake has turned over" ???
Got a book around here somewhere that explains it, but, at least in this part of the world, the reason why the fishing is off is the impact on the oxygen.Over winter the plants die out and start to rot. This takes oxygen from the water at lower levels. The upper levels still have O2 under the ice, although it can become depleted and the lake will winter kill. Once the ice is off, the wind will replenish the O2 and the fishing is great. Then the lake turns over like Turtle described. The O2 depleted water comes to the top and mixes. With less O2 overall, the fish become less active and fishing can be off for a week or so. In extreme cases, there is a fish kill.Very common on small to middle sized lakes.
Old thread but:
There is more to why fishing is off after turnover.
Fall turnover is what we talk about in the northeast. That happens when the water
temperature at the surface drops to a point that it is close to or equals the thermocline temps.
The thermocline is the layer of water that is both cold and has enough oxygen. Below the thermocline is the really cold layer which has very little dissolved oxygen. Plantlife aside, when the temps equal out, the whole lake then mixes- "turns over". Yes, you get the junk, the slime, the weeds at varying amounts in different lakes, but when the water mixes, then the oxygen AND temps get distributed over the whole lake.
When the whole lake equalizes, the fish-concentrating components- temperature zones, oxygen levels, and baitfish schools- are eliminated or reduced, spreading the gamefish out. So while other issues mentioned may play a part in the whole fishing experience, lake turnover in northern climates is not a mysterious phenomenon, but is an expected event or circumstance.
In winter, water under the ice
can depletes its oxygen. Plant decay, etc. can contribute. The air cannot stir up the water surface and entrain it with oxygen. That is what causes winter kill, especially in lakes that do not have a great deal of volume to hold oxygenated water over winter, or a hard-running river inflow to bring in O2.
In spring, a lake does not "turn over" again, but water bodies start to "stratify" by temperature, and other than high wind activity, the layers essentially (especially in deeper lakes) do not 'mix' again until fall. This stratification is what creates the "thermocline".
At least in the northeast, turnover happens every fall in any and every sized lake except for maybe shallow ponds, caused by the same thing that makes ice float.
Vermont isn't Arizona though