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Components of the Climate System

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Presentation on theme: "Components of the Climate System"— Presentation transcript:

1 Components of the Climate System
Atmosphere Ocean Biosphere Geosphere Image from NASA

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

3 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.

4 Temperature Structure of Ocean
thermocline

5 Ocean Circulation

6 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).

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

8 Sea Surface Temperature

9 Ocean Salinity AVERAGE = 35 ppm or 3.5% denser

10 Temperature-Salinity (density) Diagram

11 Thermohaline Circulation
North Atlantic Deep Water (NADW 15 million m3 of near surface water descend into the deep ocean each second.

12 Thermohaline Circulation - The Ocean Conveyor

13 Equatorial to polar heat transport and water flow

14 Ocean – Atmosphere Circulation

15 UNEQUAL HEATING OF EARTH
BUT – Outgoing solar radiation is not as uneven 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


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