Wind Sea and Swell Delineation for Numerical Wave Modeling
Wind Sea and Swell Delineation for Numerical Wave Modeling
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发表时间:
2007
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通讯作者:
B. Tracy;E. Devaliere;J. Hanson
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作者:
B. Tracy;E. Devaliere;J. Hanson
Numerical wave modeling in the fields of hindcasting and forecasting produces output in the form of an energy spectrum. This energy spectrum is usually assigned a significant wave height calculated from the amount of energy in the spectrum, and a wave period and direction are assigned to this significant wave height from analysis of the energy spectrum. These definitions describe the overall situation but do not give a detailed picture of the spectrum. A spectrum is made up of an area of wind sea resulting from the prevailing winds at the same location as the spectrum in addition to many swell wave trains that have moved into the area from directions far from the site. It is helpful to know details of all the components of the spectrum to make judgments on the skill of a numerical model or to analyze wave conditions for navigation or a coastal process. A spectral partitioning method derived from the field of digital imaging (Vincent and Soille, 1991) has been adapted to produce wave partitions from a directional wave energy spectrum. This approach will be referred to as the Wave Spectrum Energy Partitioning (WaveSEP) method. A FORTRAN version of this algorithm was developed and tested at the Coastal and Hydraulics Laboratory and High Performance Computing Center at the Engineer Research and Development Center in Vicksburg, MS. This paper will discuss the implementation of the WaveSEP FORTRAN algorithm.