Green-Naghdi dynamics of surface wind waves in finite depth

被引:3
|
作者
Manna, M. A. [1 ,2 ]
Latifi, A. [3 ]
Kraenkel, R. A. [4 ]
机构
[1] Univ Montpellier, F-34095 Montpellier, France
[2] CNRS, Lab Charles Coulomb, UMR 5221, F-34095 Montpellier, France
[3] Qom Univ Technol, Dept Phys, Fac Sci, Qom, Iran
[4] UNESP Univ Estadual Paulista, Inst Fis Teor, Rua Dr Bento Teobaldo Ferraz 27,Bloco 2, BR-01140070 Sao Paulo, Brazil
关键词
surface waves; wind-waves; Miles' mechanism; nonlinear Green-Nagdhi model; waves in finite depth; FETCH LIMITED WAVES; WATER-WAVES; EQUATION; GROWTH; DERIVATION; MODELS;
D O I
10.1088/1873-7005/aaa739
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
The Miles' quasi laminar theory of waves generation by wind in finite depth h is presented. In this context, the fully nonlinear Green-Naghdi model equation is derived for the first time. This model equation is obtained by the non perturbative Green-Naghdi approach, coupling a nonlinear evolution of water waves with the atmospheric dynamics which works as in the classic Miles' theory. A depth-dependent and wind-dependent wave growth. is drawn from the dispersion relation of the coupled Green-Naghdi model with the atmospheric dynamics. Different values of the dimensionless water depth parameter delta = gh/U-1, with g the gravity and U-1 a characteristic wind velocity, produce two families of growth rate gamma in function of the dimensionless theoretical wave-age c(0): a family of gamma with h constant and U-1 variable and another family of gamma with U-1 constant and h variable. The allowed minimum and maximum values of gamma in this model are exhibited.
引用
收藏
页数:9
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