Hurricane Wind Power Spectra, Cospectra, and Integral Length Scales

Atmospheric turbulence is an important factor in the modelling of wind forces on structures and the losses they produce in extreme wind events. However, while turbulence in non-hurricane winds has been thoroughly researched, turbulence in tropical cyclones and hurricanes that affect the Gulf and Atlantic coasts has only recently been the object of systematic study. In this paper, Florida Coastal Monitoring Program surface wind measurements over the sea surface and open flat terrain are used to estimate tropical cyclone and hurricane wind spectra and cospectra as well as integral length scales. From the analyses of wind speeds obtained from five towers in four hurricanes it can be concluded with high confidence that the turbulent energy at lower frequencies is considerably higher in hurricane than in non-hurricane winds. Estimates of turbulence spectra, cospectra, and integral turbulence scales presented can be used for the development in experimental facilities of hurricane wind flows and the forces they induce on structures.

[1]  H. W. Teunissen,et al.  Structure of mean winds and turbulence in the planetary boundary layer over rural terrain , 1980 .

[2]  Jon Wiernga Representative roughness parameters for homogeneous terrain , 1993 .

[3]  J. Højstrup,et al.  Modelling velocity spectra in the lower part of the planetary boundary layer , 1984 .

[4]  D. M. Deaves,et al.  Terrain-dependence of longitudinal R.M.S. velocities in the neutral atmosphere , 1981 .

[5]  J. Schroeder,et al.  Hurricane Bonnie wind flow characteristics as determined from WEMITE , 2003 .

[6]  J. Bendat,et al.  Random Data: Analysis and Measurement Procedures , 1987 .

[7]  J. Bendat,et al.  Random Data: Analysis and Measurement Procedures , 1971 .

[8]  T. Foken,et al.  Methods and limitations in validation of footprint models , 2004 .

[9]  T. W. Horst,et al.  Footprint estimation for scalar flux measurements in the atmospheric surface layer , 1992 .

[10]  K. McKee Book Reviews : Wind Effects On Structures: E. Simiu and R.H. Scanlan John Wiley & Sons, New York, New York 1980, $33.50 , 1981 .

[11]  I. V. D. Hoven POWER SPECTRUM OF HORIZONTAL WIND SPEED IN THE FREQUENCY RANGE FROM 0.0007 TO 900 CYCLES PER HOUR , 1957 .

[12]  H. W. Tieleman,et al.  Universality of velocity spectra , 1995 .

[13]  H. Teunissen Characteristics of the Mean Wind and Turbulence in the Planetary Boundary Layer , 1970 .

[14]  J. Kaimal,et al.  Spectral Characteristics of Surface-Layer Turbulence , 1972 .

[15]  Franz Fiedler,et al.  Atmospheric Scales and Spectral Gaps , 1970 .

[16]  Peter Hauge Madsen,et al.  Power Spectra of Horizontal Wind Components in the Neutral Atmospheric Surface Layer , 1989 .

[17]  S. Larsen,et al.  On the Dependence of Sea Surface Roughness on Wind Waves , 1998 .

[18]  R. Stull An Introduction to Boundary Layer Meteorology , 1988 .

[19]  E. W. Peterson,et al.  Modification of mean flow and turbulent energy by a change in surface roughness under conditions of neutral stability , 1969 .

[20]  John L. Lumley,et al.  The structure of atmospheric turbulence , 1964 .