1987
DOI: 10.1029/jc092ic06p06488
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A comparison of methods for estimating u* from given uz and air‐sea temperature differences

Abstract: This paper presents an objective assessment of four methods for estimating sea surface friction velocity u* from wind speed at height z, uz, and air‐sea temperature difference. The methods are compared by using the computed friction velocity as the normalization factor in parametric correlations of wind‐wave parameters with the wind and wave measurements made by NOMAD buoys in the Great Lakes. The results show that (1) wind profile parameters obtained from the four methods are generally comparable, (2) paramet… Show more

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Cited by 39 publications
(26 citation statements)
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References 16 publications
(8 reference statements)
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“…For comparison with other data, we normalized our measured wind speeds to wind speed at a height of 10 m above the lake. We assumed a neutrally stable boundary layer and a logarithmic wind profile with a drag coefficient of 1.3 X 10m7 (Liu and Schwab 1987;Clark et al 1995).…”
Section: Methodsmentioning
confidence: 99%
“…For comparison with other data, we normalized our measured wind speeds to wind speed at a height of 10 m above the lake. We assumed a neutrally stable boundary layer and a logarithmic wind profile with a drag coefficient of 1.3 X 10m7 (Liu and Schwab 1987;Clark et al 1995).…”
Section: Methodsmentioning
confidence: 99%
“…This algorithm will hereafter be referred to as J99 hereafter (i.e., Jordan et al, 1999). The other algorithm, 30 hereafter referred to as LS87 (Liu and Schwab, 1987) was originally developed at NOAA's Great …”
Section: Flux Algorithmsmentioning
confidence: 99%
“…To calculate momentum flux, the profile theory described above [Liu and Schwab, 1987] for anemometer height adjustment is used at each grid square at each time step to estimate surface stress, using the surface water temperature from the circulation model. This procedure provides estimates of bulk aerodynamic transfer coefficients for momentum and heat, which depend on the stability of atmospheric boundary layer.…”
Section: Momentum Fluxmentioning
confidence: 99%