Références bibliographiques
Miche, A., Mouvements ondulatoires de la mer en profondeur croissante ou
décroissante. première partie. mouvements ondulatoires périodiques et cylindriques en
profondeur constante, Annales des Ponts et Chaussées, Tome 114, 42–78, 1944.
Miles, J., On the generation of surface waves by shear flows, Journal of Fluid
Mechanics, 3 , 185–204, 1957.
Phillips, O. M., On the generation of waves by turbulent wind, Journal of Fluid
Mechanics, 2 , 417–445, 1957.
Pierson, W., and L. Moskowitz, A proposed spectral form for fully developed wind
seas based on the similarity theory of s. a. kitaigorodskii, Journal of Geophysical
Research, pp. 5181–5190, 1964.
PILKEY O.H., COOPER J.A.G. (2002). Longshore Transport Volumes: A Critical
View. J. of Coast. Res., SI 36, pp 572-580 (ICS 2002 Proceedings).
Référence 1
TOLMAN H.L. (2009). User manual and system documentation of WAVEWATCH
III version 3.14. NOAA/NWS/NCEP/MMAB Technical Note 276, 194 p.
TOLMAN H.L. (2009). User manual and system documentation of WAVEWATCH
III version 3.14. Technical Note 276, NOAA / NWS / NCEP / MMAB.
Tolman, H., B. Balasubramaniyan, L. Burroughs, D. Chalikov, Y. Chao, H. Chen, and
V. Gerald, Development and implementation of wind-generated ocean surface wave
models at NCEP, Weather and Forecasting, 17, 311–333, 2002.
Tolman, H., Distributed-memory concepts in the wave model WAVEWATCH III,
Parallel Comput., 28 , 35–52, 2002.
Weber, J., K. Christensen, and C. Denamiel, Wave induced setup of the mean surface
over a sloping beach, Continental Shelf Research, pp. 1448–1453, 2009.
Whitham, G., Linear and nonlinear waves, 636 p., New York, 1974.
ZACHARIOUDAKI A., PAN S., SIMMONDS D., MAGAR V., REEVE D. E.
(2011). Future wave climate over the west-European shelf seas. Ocean Dynamics, Vol.
6, pp 807-827. doi: 10.1007/s10236-011-0395-6.
Sites internet
[1] www.noaa.gov consulté le 30/08/2012
[2] www.shom.fr consulté le 15/09/2012
Miche, A., Mouvements ondulatoires de la mer en profondeur croissante ou
décroissante. première partie. mouvements ondulatoires périodiques et cylindriques en
profondeur constante, Annales des Ponts et Chaussées, Tome 114, 42–78, 1944.
Miles, J., On the generation of surface waves by shear flows, Journal of Fluid
Mechanics, 3 , 185–204, 1957.
Phillips, O. M., On the generation of waves by turbulent wind, Journal of Fluid
Mechanics, 2 , 417–445, 1957.
Pierson, W., and L. Moskowitz, A proposed spectral form for fully developed wind
seas based on the similarity theory of s. a. kitaigorodskii, Journal of Geophysical
Research, pp. 5181–5190, 1964.
PILKEY O.H., COOPER J.A.G. (2002). Longshore Transport Volumes: A Critical
View. J. of Coast. Res., SI 36, pp 572-580 (ICS 2002 Proceedings).
Référence 1
TOLMAN H.L. (2009). User manual and system documentation of WAVEWATCH
III version 3.14. NOAA/NWS/NCEP/MMAB Technical Note 276, 194 p.
TOLMAN H.L. (2009). User manual and system documentation of WAVEWATCH
III version 3.14. Technical Note 276, NOAA / NWS / NCEP / MMAB.
Tolman, H., B. Balasubramaniyan, L. Burroughs, D. Chalikov, Y. Chao, H. Chen, and
V. Gerald, Development and implementation of wind-generated ocean surface wave
models at NCEP, Weather and Forecasting, 17, 311–333, 2002.
Tolman, H., Distributed-memory concepts in the wave model WAVEWATCH III,
Parallel Comput., 28 , 35–52, 2002.
Weber, J., K. Christensen, and C. Denamiel, Wave induced setup of the mean surface
over a sloping beach, Continental Shelf Research, pp. 1448–1453, 2009.
Whitham, G., Linear and nonlinear waves, 636 p., New York, 1974.
ZACHARIOUDAKI A., PAN S., SIMMONDS D., MAGAR V., REEVE D. E.
(2011). Future wave climate over the west-European shelf seas. Ocean Dynamics, Vol.
6, pp 807-827. doi: 10.1007/s10236-011-0395-6.
Sites internet
[1] www.noaa.gov consulté le 30/08/2012
[2] www.shom.fr consulté le 15/09/2012
