For One cell model (Hadley Cell) we must assume two things:
What is happening aloft?
What is happening at surface?
For multi-cell model we must assume two things:
- a uniform body of water
equatorial low
Subtropical High
found at 30 degrees N and S; sinking motion; deserts found here; horse latitudes; north to the right, south to the left deflection
Subpolar low
60 N and S ex: London
Polar high
created due to the temperature at the poles; sinking motion, “cold deserts”
NE/SE Tradewinds
the most consistent winds that converge at the equator
Westerlies
wind is deflected to right in north and left in south
Easterlies
High to low- left and north high to low-right
Coriolis
windspeed and latitude; less deflection at equator
Overview…
- 6 wind belts
Hadley Cell
cells 30-0 degrees latitude ; thermally direct
Ferrel Cell
cells 30-60 degrees latitude; thermally indirect
Polar cell
cells 60- poles latitude; thermally direct
Thermally Direct
warm air rises; cold air sinks (what we expect to have)
Thermally indirect
cold air rises; warm air sinks (the opposite of what we expect)
Jet Streams
rivers of rapidly moving air flowing within the same general direction:
Polar jet
Subtropical jet
Equatorial jet
Zonal flow pattern of jet streams
straight flow
meridional flow pattern of jet streams
wavy flow
Ocean Current
Temperature profile of an ocean
Absorption of solar radiation heats the ocean and land surfaces; temperature DROPS with DEPTH (opposite of the troposphere)
Mixed Layer