Grant Number: N000140010067 http://newark.cms.udel.edu/~brucel/hrd.html
LONG-TERM GOALSOur long-term goal is to quantify submesoscale processes in order to improve our understanding of ocean interactions at various space and time scales. Our current effort focuses on the following four tasks:1.Understanding small-scale coastal ocean processes;
2.Understanding small-scale advective exchange and stirring;3. Model assessment, enhancement, and assimilation;4. Using high-resolution disparate (HRD) ocean surface data to infer subsurface flow conditions.
OBJECTIVESOur objective is to develop dynamically consistent nowcasts of the surface velocity field by combining disparate observations from a variety of sensors, including HF radar, Lagrangian drifters, current meters, ADCPs, and passive remote sensing. We can incorporate normal flow information at open boundaries from any source (observations, models, climatology, etc.).These nowcasts can be used to study the evolution of coastal processes including mixing and exchange. When assimilated into a numerical model, the nowcasts can also be used to infer aspects of the subsurface flow.
APPROACHOur nowcasts employ an objective mapping technique that is a generalization of a method first described by Rao and Schwab (1981) in an analysis of currents in Lake Ontario. The technique, called normal 1