On Detection of a Wave Age Dependency for the Sea Surface Roughness

2004 ◽  
Vol 34 (6) ◽  
pp. 1441-1458 ◽  
Author(s):  
B. Lange ◽  
H. K. Johnson ◽  
S. Larsen ◽  
J. Højstrup ◽  
H. Kofoed-Hansen ◽  
...  
Author(s):  
Dag Myrhaug ◽  
Muk Chen Ong

This paper considers the effect of wave age on wind gust spectra over wind waves. Here, two wind gust spectra based on maritime data are used to serve the purpose of demonstrating the effect of wave age; the spectra according to Wills et al. (1986 “Offshore Mean Wind Profile,” Department of Energy, Offshore Technical Report No. OTH86226) and Ochi and Shin (1988, “Wind Turbulent Spectra for Design Considerations of Offshore Structures,” Proceedings of the 20th Offshore Technology Conference, Houston, TX, Paper No. 5736, pp. 461–467). The effect of wave age is taken into account by using the Volkov (2001, “The Dependence on Wave Age,” in Wind Stress Over the Ocean, Cambridge University Press, Cambridge, UK, pp. 206–217) sea surface roughness formula. The wave age independent Charnock (1955, “Wind Stress on a Water Surface,” Q. J. R. Meteorol. Soc., 81, pp. 639–640) sea surface roughness is used as a reference. The results are valid for wind waves in local equilibrium with steady wind in laterally homogeneous flow. An example of results demonstrates a clear effect of wave age on the wind gust spectra; also, distinct differences between the two spectra for a given wave age are demonstrated. Finally, an example of application is provided, demonstrating clear effects of the two spectra and the sea surface roughness on slowly varying surge motion of a marine structure due to wind gust.


Author(s):  
Bernt J. Leira ◽  
Dag Myrhaug ◽  
Jarle Voll

The paper considers the surge-motion of a simplified dynamic system representing a FPSO exposed to wind load. The Ochi and Shin wind gust spectrum, [12], is used together with two sea surface roughness formulas: the wave age independent Charnock formula, [4], that is frequently used, and the wave age dependent Volkov formula, [16]. An example of results demonstrates the effect of the sea surface roughness on the dynamic wind response of the system.


2021 ◽  
Vol 9 (3) ◽  
pp. 246
Author(s):  
Difu Sun ◽  
Junqiang Song ◽  
Xiaoyong Li ◽  
Kaijun Ren ◽  
Hongze Leng

A wave state related sea surface roughness parameterization scheme that takes into account the impact of sea foam is proposed in this study. Using eight observational datasets, the performances of two most widely used wave state related parameterizations are examined under various wave conditions. Based on the different performances of two wave state related parameterizations under different wave state, and by introducing the effect of sea foam, a new sea surface roughness parameterization suitable for low to extreme wind conditions is proposed. The behaviors of drag coefficient predicted by the proposed parameterization match the field and laboratory measurements well. It is shown that the drag coefficient increases with the increasing wind speed under low and moderate wind speed conditions, and then decreases with increasing wind speed, due to the effect of sea foam under high wind speed conditions. The maximum values of the drag coefficient are reached when the 10 m wind speeds are in the range of 30–35 m/s.


Author(s):  
Lianxin Zhang ◽  
Xuefeng Zhang ◽  
William Perrie ◽  
Changlong Guan ◽  
Bo Dan ◽  
...  

AbstractA coupled ocean-wave-sea spray model system is used to investigate the impacts of sea spray and sea surface roughness on the response of the upper ocean to the passage of the super typhoon Haitang. Sea spray mediated heat and momentum fluxes are derived from an improved version of Fairall’s heat fluxes formulation (Zhang et al., 2017) and Andreas’s sea spray-mediated momentum flux models. For winds ranging from low to extremely high speeds, a new parameterization scheme for the sea surface roughness is developed, in which the effects of wave state and sea spray are introduced. In this formulation, the drag coefficient has minimal values over the right quadrant of the typhoon track, along which the typhoon-generated waves are longer, smoother, and older, compared to other quadrants. Using traditional interfacial air-sea turbulent (sensible, latent, and momentum) fluxes, the sea surface cooling response to typhoon Haitang is overestimated by 1 °C, which can be compensated by the effects of sea spray and ocean waves on the right side of the storm. Inclusion of sea spray-mediated turbulent fluxes and sea surface roughness, modulated by ocean waves, gives enhanced cooling along the left edges of the cooling area by 0.2 °C, consistent with the upper ocean temperature observations.


2005 ◽  
Author(s):  
G.D. Sandlin ◽  
L.A. Rose ◽  
G.L. Geernaert ◽  
J.P. Hollinger ◽  
F.A. Hansen

2020 ◽  
Vol 125 (8) ◽  
Author(s):  
Nicolas Rascle ◽  
Bertrand Chapron ◽  
Jeroen Molemaker ◽  
Frédéric Nouguier ◽  
Francisco J. Ocampo‐Torres ◽  
...  

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