Title: Components of the Climate System
1Components of the Climate System
Image from NASA
2Atmosphere Ocean Circulation
- Atmospheric Circulation
- Depends on density
- Ocean Surface Circulation
- Depends on the wind
- Deep Ocean Circulation
- Depends on density
3Why is Ocean Circulation Important?
- Transport 20 of latitudinal heat
- Equator to poles
- Transport nutrients and organisms
- Influences weather and climate
- Influences commerce
4Temperature Structure of Ocean
thermocline
5Ocean Circulation
6Wind-drive ocean surface currents
Wind driven 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).
7Atmosphere Ocean Circulation
- Atmospheric Circulation
- Depends on density
- Ocean Surface Circulation
- Depends on the wind
- Deep Ocean Circulation
- Depends on density
8Sea Surface Temperature
http//www.ldeo.columbia.edu/dees/ees/climate/slid
es/sst_march.gif
9Ocean Salinity
- http//www.ldeo.columbia.edu/dees/ees/climate/slid
es/sal_march.gif - http//ingrid.ldgo.columbia.edu/
10Temperature-Salinity (density) Diagram
11Thermohaline Circulation
North Atlantic Deep Water (NADW
15 million m3 of near surface water descend into
the deep ocean each second.
12Thermohaline Circulation - The Ocean Conveyor
13Equatorial to polar heat transport and water flow
14Ocean Atmosphere Circulation
15UNEQUAL HEATING OF EARTH
BUT Outgoing solar radiation is not as uneven