Lecture 11 Flashcards
atmosphere and oceans move due to unequal heating
3-cell model
oceans constantly in motion
- transfer heat from warmer to colder areas
- influences abundance of life in surface waters by affecting nutrients
2 types of ocean circulation
surface circulation (above 400m) deep ocean circulation (below 400m)
surface circulation
driven by winds
deep circulation
driven by density
direct methods of measuring ocean circulation
floating devices released and tracked through time
fixed propeller flow meter
indirect methods
satellite measurement
doppler flow meters
tracking t, s or other chemical tracers
what causes gyres to form
continent positions and wind patterns
southern gyres- flow counter clockwise
ekman spiral
looking vertically down at the currents, they spiral
ekman transport
avg flow of water throughout the serial is 90 degrees to the right/left