| contributor author | Lin, Ray Q. | |
| contributor author | Perrie, Will | |
| date accessioned | 2017-06-09T14:52:44Z | |
| date available | 2017-06-09T14:52:44Z | |
| date copyright | 1997/10/01 | |
| date issued | 1997 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-28778.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4165931 | |
| description abstract | The authors study the action flux associated with three-dimensional wave?wave interactions of ocean surface waves. Over deep water, two-dimensional wave?wave interactions are dominant: the three-dimensional five-wave interactions are two orders of magnitude smaller than the two-dimensional four-wave interactions. However, the five-wave interactions become increasingly important as the water depth decreases. Because of the effects of finite depth, three-dimensional five-wave interactions, involving steep finite-amplitude waves, dominate over two-dimensional four-wave interactions. Specifically, when the water depth h is less than 10 m, or nondimensionalizing with the spectral peak wavenumber Kp when Kph ≤ 3.6 and nonlinearity, ? = Ka(3 + tanh2Kh)/4 tanh3Kh ≥ 0.3, the five-wave interactions completely dominate. Results are consistent with the instability study by McLean. | |
| publisher | American Meteorological Society | |
| title | A New Coastal Wave Model. Part V: Five-Wave Interactions | |
| type | Journal Paper | |
| journal volume | 27 | |
| journal issue | 10 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1997)027<2169:ANCWMP>2.0.CO;2 | |
| journal fristpage | 2169 | |
| journal lastpage | 2186 | |
| tree | Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010 | |
| contenttype | Fulltext | |