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Surface temps seem to be more useful in the Spring and late Fall when there isn't a pronounced thermocline present. Once the thermocline is established the surface temps (other than looking at temperature inversions or "turnovers" in the lake) are less relevant during the summer. The "down" temps and location of the thermocline in the water column (changes with wind and currents) are the more important factors then. At least that is the way I look at it.

Edited by Sk8man
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