Wind-Driven Circulation in a Stratified Ocean Consider the ocean in several isopycnal layers that can be separated into two groups: Layers that outcrop.
Thermohaline circulation ●The concept of meridional overturning ●Deep water formation and property Antarctic Bottom Water North Atlantic Deep Water Antarctic.
Regional Ocean Modeling System Free surface, hydrostatic ocean model Finite-difference 3D Reynolds-averaged Navier-Stokes equations Horizontal orthogonal.
Lecture 2 - Major Ions in Sea Water What is the composition of seawater? What defines Major Ions? What are their concentrations? What are their properties?
Characterizing Future Climate – Information Needs.
Multiscale ensemble filtering, with replicates conditioned on satellite cloud observations, is both realistic and efficient 2) Multiscale Data Assimilation.
Main Objective
7 th Annual Summer Institute and Friday Harbor Laboratory Centennial Symposium
Argo observes global variability in the oceans Dean Roemmich and John Gilson Scripps Institution of Oceanography, USA IUGG Perugia, July 2007.
GE0-3112 Sedimentary processes and products Lecture 8. Lakes Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder 1999. Ch.
General Circulation of the Ocean
Some Mathematics: The Equations of Motion Physical oceanography Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of Earth Sciences National Cheng.
