Hawaiian Ocean Mixing Experiment: Farfield Component: SIO Contribution to Observation of the Barotropic Ocean Tides: A Cooperative Program with the University of Hawaii and WHOI

Chave/ filloux提供资金在夏威夷海脊附近进行一项大型协调实验，以确定地形粗糙的地点是否对全球海洋的混合负责。目标是确定海洋混合的主要能量途径，并实现该区域的大致能量收支。一个配套的建模工作将主要集中在潮汐散射作为海洋混合的能量来源的问题上，而对夏威夷群岛附近收集的数据的历史分析将有助于指导调查计划，以确定强烈混合活动发生的区域的位置和普遍性。在Farfield实验的这个特殊组成部分中，一组水平静电计和底部压力记录仪将部署在夏威夷山脊的两侧，以补充层析成像阵列。目的是量化脊上正压能量通量辐合和与低模斜压波辐射相关的通量散度。这一差异是用来衡量在海脊进行混合的潮汐能。

Chave/ FillouxFunding is provided to conduct a large coordinated experiment near the Hawaiian Ridge to determine whether sites with rough topography are responsible for the mixing of the global ocean. The goals are to identify the major energy pathways for ocean mixing and achieve an approximate energy budget for the region. A companion modeling effort will focus primarily on the issue of tidal scattering as an energy source for ocean mixing while a historical analysis of data collected in the vicinity of the Hawaiian Islands will help guide the survey program in determining the location and ubiquity of regions where strong mixing activity takes place. Under this particular component of the Farfield experiment, an array of horizontal electrometer and bottom pressure recorders will be deployed on either side of the Hawaiian Ridge to complement a tomographic array. The objective is to quantify the barotropic energy flux convergence at the Ridge and the flux divergence associated with low mode baroclinic waves radiation. The difference is a measure of the tidal power available for mixing at the Ridge.