Abstract
Based on the complete Stokes wave model with the bias term and using a simple mapping approach and an iteration solution method, we established a formula for the joint probability density function of the surface slope elevation of a nonlinear random wave field. The formula requires three parameters to define the whole density function; the rms surface elevation and slope values and the significant slope. This model represents the dynamics of the wave in a more direct way than the Gram-Charlier approximation.-from STAR, 22(17), 1984
Original language | English |
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Title of host publication | Frontiers of remote sensing of the oceans and troposphere from air and space platforms. Symposium, Shoresh, 1984, (US NASA, Marshall Space Flight Center, Huntsville, AL; NASA-CP-2303) |
Pages | 247-255 |
Number of pages | 9 |
State | Published - 1984 |