I am having a difficult time calibrating the development of a thermocline in the lake I am studying without varying the WSC coefficient substantially over the spring summer and early Fall. The epilimnion is restricted to the upper 7-9 meters of the lake and unless I reduce the WSC to .32 to .45 during the hottest Months (July, Early Aug) the warm temps migrate too deep.
I am using a vertical viscosity coeff of 0.001. It appears to me that in reality, the vertical viscosity coefficient is varying substantially as the epilimnion warms up and the temp gradient increases.
Is it legitimate to use a lower visc coefficient than 0.001 and would this tend to keep the heat from migrating downward into the hypolimnion as quickly?
Is there a way to vary this coeff over time?
Jon
[addsig]
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