Presentation is loading. Please wait.

Presentation is loading. Please wait.

The Restless Oceans 23.5.

Similar presentations


Presentation on theme: "The Restless Oceans 23.5."— Presentation transcript:

1 The Restless Oceans 23.5

2 Explain how the properties of ocean water change with depth.

3 Atmosphere & Ocean Circulation
Atmospheric Circulation Depends on density Ocean Surface Circulation Depends on the wind Deep Ocean Circulation

4 Why is Ocean Circulation Important?
Transport ~ 20% of latitudinal heat Equator to poles Transport nutrients and organisms Influences weather and climate Influences commerce 4 th century BC ,Pytheas of Massalia, a Greek ship captain, explored eastern Atlantic Okeanos (Greek for “Great River”) because he found the ocean flowing south (Canary Current) and thought it was a river too wide to cross.

5 Ocean Circulation

6 Distinguish between surface currents, deep currents, and upwelling.

7 Wind-drive ocean surface currents
Wind driven surface currents Wind-drive ocean surface currents London = 51 deg N James Bay = 51 deg. N Edinburgh = 55deg N, same latitude as Ontario’s Polar Bear Provincial Park Total water in ocean surface circulation = about 100 Amazon Rivers (20 million m3/s). It requires years to complete cycle. How fast? A few miles/hr (Gulf Stream off of Miami = 4.5 mph) How much? Total water in ocean surface circulation = about 100 Amazon Rivers (20 million m3/s).

8 Sea Surface Temperature

9 Ocean Salinity AVERAGE = 35 ppm or 3.5% denser

10 Equatorial to polar heat transport and water flow

11 Ocean – Atmosphere Circulation


Download ppt "The Restless Oceans 23.5."

Similar presentations


Ads by Google