diff options
Diffstat (limited to 'source/blender/blenkernel/intern/ocean_spectrum.c')
| -rw-r--r-- | source/blender/blenkernel/intern/ocean_spectrum.c | 17 |
1 files changed, 0 insertions, 17 deletions
diff --git a/source/blender/blenkernel/intern/ocean_spectrum.c b/source/blender/blenkernel/intern/ocean_spectrum.c index c5504b22b43..43e0f399213 100644 --- a/source/blender/blenkernel/intern/ocean_spectrum.c +++ b/source/blender/blenkernel/intern/ocean_spectrum.c @@ -128,11 +128,6 @@ static float jonswap(const Ocean *oc, const float k2) return val; } -/** - * Pierson-Moskowitz model, 1964, assumes waves reach equilibrium with wind. - * Model is intended for large area 'fully developed' sea, where winds have been steadily blowing - * for days over an area that includes hundreds of wavelengths on a side. - */ float BLI_ocean_spectrum_piersonmoskowitz(const Ocean *oc, const float kx, const float kz) { const float k2 = kx * kx + kz * kz; @@ -159,10 +154,6 @@ float BLI_ocean_spectrum_piersonmoskowitz(const Ocean *oc, const float kx, const return val; } -/** - * TMA extends the JONSWAP spectrum. - * This spectral model is best suited to shallow water. - */ float BLI_ocean_spectrum_texelmarsenarsloe(const Ocean *oc, const float kx, const float kz) { const float k2 = kx * kx + kz * kz; @@ -195,14 +186,6 @@ float BLI_ocean_spectrum_texelmarsenarsloe(const Ocean *oc, const float kx, cons return val; } -/** - * Hasselmann et al, 1973. This model extends the Pierson-Moskowitz model with a peak sharpening - * function This enhancement is an artificial construct to address the problem that the wave - * spectrum is never fully developed. - * - * The fetch parameter represents the distance from a lee shore, - * called the fetch, or the distance over which the wind blows with constant velocity. - */ float BLI_ocean_spectrum_jonswap(const Ocean *oc, const float kx, const float kz) { const float k2 = kx * kx + kz * kz; |