Turbulent Mixing in the Ocean by Non-Breaking Wind Waves
Few operational forecasting models account for the effect of non-breaking wind- generated surface waves on the turbulent mixing of the upper ocean.Numerous studies have shown that the effect not only exists,but that its absence from the models can in many situations lead to an under-mixed upper ocean and sea surface temperatures which are too high.By assuming that wave-induced turbulence is the primary mechanism responsible for swell dissipation,we have applied a parameterisation based on swell dissipation measurements to a one-dimensional mixing model which suggests that this source of turbulence could be responsible for a significant portion of near-surface mixing in the ocean.
wave-induced turbulence mixed layer sea-surface temperature
Malek Ghantous Alexander V.Babanin Dmitry Chalikov
Centre for Ocean Engineering, Science and Technology, Swinburne University of Technology, Hawthorn, VIC, Australia, 3122
国际会议
The 17th Pacific -Asian Marginal Seas Meeting(第十七届太平洋与亚洲边缘海国际会议)
杭州
英文
88-92
2013-04-23(万方平台首次上网日期,不代表论文的发表时间)