Lecture 12- Ocean Circulation 4 Flashcards
speed of circulation
- from 14C radioactive decay tracer
- cold dense water sinks in the North Atlantic and around Antarctica to form deep water
14C levels
high in the north but gets lower as you go south
oldest deep waters (2000 years) are in
the deep Pacific
locations of deep water formation in the North Atlantic
- Labrador
- Irminger Sea
- Greenland
- Norwegian Seas
locations of deep water formation around Antarctica
- Ross
- Weddell Sea
speed of deep ocean circulation
- slow
- hundreds to thousands of years
speed of surface current
- fast
- decades
conveyor belt circulation
- combination of deep ocean currents and surface currents
- super idealized pattern
example of conveyor belt circulation
Gulf Stream in Europe
conveyor belt circulation and temperature
acts to pull heat away from the equator and give it to the atmosphere/high latitudes
more water vapor means
less density
pressure from warm, moist air
creates low pressure at the equator