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Components of the Climate System

• Atmosphere
• Ocean

• Biosphere
• Geosphere

Image from NASA
Atmosphere & Ocean Circulation
• Atmospheric Circulation
– Depends on density

• Ocean Surface
Circulation
– Depends on the wind

• Deep Ocean Circulation
– Depends on density
Why is Ocean Circulation
Important?
• Transport ~ 20% of
latitudinal heat
– Equator to poles
• Transport nutrients and
organisms
• Influences weather and
climate
• Influences commerce
Temperature Structure of Ocean

thermocline
Ocean Circulation
Wind driven surface currents
Wind-drive ocean surface currents

• 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).
Atmosphere & Ocean Circulation
• Atmospheric Circulation
– Depends on density

• Ocean Surface
Circulation
– Depends on the wind

• Deep Ocean Circulation
– Depends on density
Sea Surface Temperature

http://www.ldeo.columbia.edu/dees/ees/climate/slides/sst_march.gif
Ocean Salinity

http://www.ldeo.columbia.edu/dees/ees/climate/slides/sal_march.gif
•http://ingrid.ldgo.columbia.edu/
Temperature-Salinity
(density) Diagram
Thermohaline Circulation
North Atlantic
Deep Water
(NADW

15 million m3 of near surface water descend into the deep ocean each second.
Thermohaline Circulation - The Ocean Conveyor
Equatorial to polar heat transport and water flow
Ocean – Atmosphere Circulation
UNEQUAL HEATING OF EARTH

BUT – Outgoing solar radiation is not as uneven
End of Report in Ocean
Circulation…

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Agricultural, Industrial and Domestic use

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Ocean circulation

Editor's Notes

  1. 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.
  2. 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 500-2000 years to complete cycle.
  3. AVERAGE = 35 ppm or 3.5% denser
  4. M&M fourth edition, solar constant = rate of solar radiation on surface perpendicular to the sun’s rays at the top of the atmosphere, 1.97 cal/cm2/min or 1372 watts/m2 Difference between perihelion (2.04 cal/me/min) vs 1.91 cal/m2/min at aphelion 1 watt/hr = 860 cal