Climate Dynamics Lecture 08 Ocean Dynamics

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Ocean Dynamics
- Balanced flow in the ocean
- Taylor-Proudman theorem
- Near-surface flow and flow at depth
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The discussion on sea surface height anomaly don't take into account the effect of wind thas can displace water : by geostrophic way, if you put a westely wind over the ocean at mid-latitudes, you will induce an se surface height gradient. No T or S effects here.

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