I have several questions relating to temperature calibration for anyone that can help me.
My attempt at temp calibration of the thermocline in my lake has been fairly successful. However, during times of rapid air temperature increases (e.g., early summer) the modeled temps in the first 4-5 meters of water consistently lag behind the measured temperatures by 1-1.5 degrees. I have eliminated various physical lake parameters as a cause for this lag (e.g., inflow temp and rate).
Varying the WSC helps match the shape of the hypolimnion/epilimnion but the temp lag in the first 3-4 meters develops remains after very hot spells. Later in the summer when high temps stabilize for longer periods, the match improves.
How can I increase the surface heat exchange system of the model so that the suface water absorbs more heat energy during shorter periods of rapidly increasing air temp (e.g., 2-5 days)?
The cloud cover numbers that I am using are the least precise weather data I have.
I think that the extent of cloudiness has been overestimated. Would a reduction of solar energy to the water surface due to an overestimation of cloudiness explain this lag in the heating rate even if the air temp was correctly measured and used? Would it be legitimate for me to experiment with reducing the cloud cover factor by 10% to see if it improves the match?
Thanks for any help or suggestions.
Jon
Is it appropriate to vary the wind sheltering coeff at the same water body to reflect seasonal variations in vegetation?[addsig]
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