Description Usage Arguments Value References See Also Examples
uStar is the water friction velocity due to wind stress at the lake surface, it is calculated following the methods of Imberger (1985) as a function of the shear stress of air (Fischer et al., 1979), drag coefficient for momentum (Hicks, 1972), and a dimensionless constant (von Karman constant) that decribes the logarithmic velocity profile at the air-water interface
1 | uStar(wndSpeed, wndHeight, averageEpiDense)
|
wndSpeed |
a numeric vector of wind speed in m s-1 |
wndHeight |
a numeric vector of wind measurement height in m |
averageEpiDense |
a numeric vector of epilimnion density in kg m-3 |
a numeric vector of uStar
Hicks, B.B., 1972. A procedure for the formulation of bulk transfer coefficients over water bodies of different sizes. Boundary-Layer Meterology 3: 201-213.
Amorocho, J., DeVries, J.J., 1980. A new evaluation of the wind stress coefficient over water surfaces. Journal of Geophysical Research 85: 433-442.
Fischer, H.B., List, E.J., Koh, R.C.Y., Imberger, J., Brooks, N.H., 1979. Mixing in inland and coastal waters. Academic Press.
Imberger, J., 1985. The diurnal mixed layer. Limnology and Oceanography 30: 737-770.
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