Lecture 5 Part 1 Flashcards
Where does energy come from to initiate ocean motion
The sun and the rotation of the earth
Intertia
Frictional coupling
Weather, marine life, circulation, ice melt and formation
Oceanic motion, earth rotation, changes in direction
Coriolis force or Coriolis effect
Deflection
Curved pathways
Ocean balance radiation
Radiation balance
Short wave and long wave
Terrestrial and solar radiation
Ocean balance
How heat is distributed
Due to an imbalance in net surface heat flux, global circulation has to redistribute heat from the equator to the poles
Winds
Surface currents
Deep ocean circulation
Ocean currents
Poleward transfer of energy
Complex 3D structure
Frictional coupling
Global fluxes
Oceanic heat budget
Albedo