Right now many Northwoods lakes are going through (or soon
will) something called the fall turnover. It’s a phenomenon as beneficial as it
is interesting.
Fall turnover is a restorative process, a bit like opening
doors and window in a long-sealed, musty basement and letting lots of clean,
fresh air course through.
A previous column in this space told how lakes stratify (form
layers) in summer – warmer, lighter water above and colder, denser water below.
At the height of the warm season, these layers don’t mix very much because the
difference in density between surface water (at, say, 80 degrees F) and deep
water (at, say, 40 or 45 degrees) is considerable.
So as the summer wears on, all kinds of materials sink from
the surface water into that cold bottom layer. Plant parts, algae, fish
carcasses, dead insects and more drift down and decompose, consuming oxygen. As
a result, the oxygen down there can become quite depleted.
What would happen if your lake remained stratified all the
time? Those deep waters would become largely lifeless, hospitable mainly to
organisms that thrive in anaerobic (without oxygen) conditions.
But fortunately, along comes the fall turnover, generally
sometime in late September or early October (likely on the early side this year
because of all the chilly weather). In simple terms, what happens is that the
surface water gradually cools, and the difference in density between the
surface and deeper water decreases, so that eventually wind and wave action can
mix the layers together. And that means the lake, from surface to bottom,
becomes infused with oxygen.
This is great for all manner of lake creatures – especially
fish that dwell in the depths – that need oxygen to make it through the winter.
How can you
tell if your lake has turned over? Well, for one thing, the water suddenly
becomes cloudier than usual because the mixing action brings up nutrients and
debris from the bottom. You might even notice a hint of sulfur scent (like
rotten eggs) as decomposing material comes to the surface. When the turnover is
complete, the water becomes clear again, likely more so than in high summer.
Some anglers
say fishing is tougher during the turnover because with oxygen available
everywhere, the fish are more scattered.
Different
lakes experience fall turnover in different ways. Deeper lakes take longer to
turn over. Shallow lakes may not turn over at all because they never actually
stratify in the first place – wave action keeps them well mixed all through
summer. The turnover itself can play out in a few days in some lakes, or during
a week or more in others.
So watch for signs of turnover in your lake. It’s another
seasonal milestone, like ice-in and ice-out, that can be fun to track over the
years.
So how small does a lake have to be to experience turnover? I'd guess that the "big" lakes (Michigan, Superior, maybe even Winnebago) are large enough to have winds and waves and incoming flows from rivers to do all the mixing on a more or less constant basis (unless they freeze over).
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