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Lecture 4b (Ch. 5 of text) Properties of Seawater (Part II)

Lecture 4b (Ch. 5 of text) Properties of Seawater (Part II)

Lecture 4b (Ch. 5 of text) Properties of Seawater (Part II). Density and Pressure. Why is the deep ocean cold?. Vertical Structure of Temperature. Thermocline. Thermocline is a permanent hydrographic feature of temperate and tropical oceans.

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837 views • 73 slides
Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia

Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia

12 years of Palmer LTER: Physical Oceanography, Spatiotemporal Variability & Ventilation of Ocean Heat Along the Western Antarctic Peninsula. LDEO/Columbia University. Martinson. Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia.edu.

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482 views • 25 slides
Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia

Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia

12 years of Palmer LTER: Physical Oceanography, Spatiotemporal Variability & Ventilation of Ocean Heat Along the Western Antarctic Peninsula. LDEO/Columbia University. Martinson. Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University dgm@ldeo.columbia.edu.

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253 views • 25 slides
Ice mass balance buoy network: Coordination with DAMOCLES

Ice mass balance buoy network: Coordination with DAMOCLES

Ice mass balance buoy network: Coordination with DAMOCLES. Jackie Richter-Menge and Don Perovich. Sea ice mass balance. Simple concept snow accumulation snow melt ice growth surface melt bottom melt Powerful tool: shows how changes occur growth or decay Difficult logistics.

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191 views • 6 slides

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