wind belts
alternate direction
primary wind belts
wind belt (0-30)
northeast trades
wind belt (30-60)
westerlies
wind belt (60-90)
polar easterlies
wind belt (0-30 S)
southeast trades
wind belt (30S - 60S)
westerlies
wind belt (60S - 90)
polar easterlies
ocean surface temperature
Atlantic ocean temperature at depth
ocean surface salinity
Atlantic Ocean salinity at depth
- deep ocean salinity more uniform
rotation of subtropical gyres
- counter-clockwise in the southern hemisphere
subpolar gyres
- absent in the southern hemisphere
Antarctic circumpolar current
moves eastward around the Antarctic continent
Why is the Coriolis force needed?
needed to account for the acceleration of the reference coordinate system (Newton’s law F=ma doesn’t apply anymore)
material is warmed when
it absorbs radiant energy (ie. solar energy)
visible radiant energy from the sun
- passes through the atmosphere without being heated
Earth’s surface
- warm surface radiates infrared radiation (long) which is absorbed by the atmosphere
atmosphere is heated from
below
atmospheric convection and precipitation is strongest
along the equator
air column with high amounts of water vapor
weighs less (creates lower sea level pressure underneath it)
sea level pressure at Pole (90 degrees)
high SLP
SLP at 60 N/S
low SLP