
What Happens During the Fall Turnover?
During the heat of late summer, deep reservoirs like Lake Texoma form three distinct thermal layers: the warm upper epilimnion, the rapidly cooling thermocline (metalimnion), and the frigid, oxygen-depleted hypolimnion near the lake bottom.
As nighttime ambient temperatures dip in September and October, the surface water cools. Water reaches its maximum physical density at 39.2Β°F (4Β°C). As the top layer reaches this threshold, it becomes heavier than the water beneath it and begins to sink. When combined with autumnal winds, the entire water column mixesβa limnological event known as the turnover.
The Fishery Impact: Why the Bite Shuts Down Temporarily
Turnover can temporarily frustrate anglers for several reasons:
Tournament Winning Adjustments on Texoma
- Follow the Washita Arm for Clarity: The Red River arm frequently turns over earlier due to shallower depths and higher mineral suspension. If your regular spots near Soldier Creek or Eisenhower State Park are murky, run north into the Washita River arm where clear tributary inflows buffer the turnover effect.
- Ditch Bottom Rigs for Suspended Baits: Stripers will suspend over deep flats (30 to 45 feet) rather than holding tight to river channel ledges. Dead-sticking 5-inch soft swimbaits or trolling multi-arm umbrella rigs through suspended bait balls outproduces jigging spoons.
- Watch the Birds: As dying shad struggle with sudden temperature shocks, gulls and terns provide aerial beacons pointing directly to feeding striper schools.