Unit Affiliation: Ocean and Climate Physics, Lamont-Doherty Earth Observatory (LDEO)
Understanding of air-sea boundary layer processes requires a quantitative description of mixing and transport in the ocean. The development and improvement of ocean models rely on results from comprehensive observation programs that capture mid- to small-scale turbulence which is associated with energy transfer from the atmosphere to the ocean. In this project, the role of surface gravity waves in energy transfer is studied by linking the atmosphere and ocean through a unique set of turbulence measurements. These are carried out simultaneously both on the air and water sides. To elucidate air-sea wave driven turbulence, the research teams will measure the vertical structure of the turbulence kinetic energy (TKE) dissipation rate across the air-sea interface from the Air Sea Interaction Tower at Martha's Vineyard Coastal Observatory. The proposed measurements of turbulence will enhance the understanding of coupled boundary layer dynamics and will improve existing and future air-sea interaction parameterizations. The field campaign will also create a data set for the community that we will be shared through an open-access data system. This will accelerate the development of high-resolution wave coupled ocean numerical models and improve both weather and ocean conditions forecasts. Outreach through education is also a focus of this program. In addition to the support and training of a graduate student and a post-doctoral researcher, undergraduate research experiences (REU) will be provided through an existing NSF-REU program (URI) and new collaborations with local schools to expose high school students to earth sciences (UConn).
This study focuses on the energy transfer from the atmosphere to the ocean and how this occurs across the air-sea interface. Indirect and direct observations of the energy flux divergence (wave-induced transport) on the atmospheric side will be used to constrain the magnitude of the air-sea TKE transfer rate and to provide an upper bound to the TKE injection by wave breaking (i.e. the breaker work). Direct estimates of active breaking and the resulting foam on the ocean surface will be used to provide complementary estimates of the subsurface TKE dissipation rate. On the ocean side, measurements of TKE dissipation rate and the TKE production and transport terms throughout the water column will be made using several complementary techniques. Using these measurements, the researchers will explore the expected TKE dissipation rate deficit/surplus at the interface relative to a rigid wall and assess the role of surface gravity waves in the deviations. Furthermore, an attempt will be made to elucidate and differentiate the effects of wave breaking and Langmuir Circulation driven turbulence and define characteristic turbulent scales to improve present and future mixing parameterizations in the upper ocean. On the atmospheric side, deviations from the law-of-the-wall are expected to be correlated to the energy flux divergence, which arises from wave motion creating an energy flux into the wave field. This study will characterize the wave signature on the air velocities and pressure on the atmospheric side, further elucidating the physics of the energy exchange.