Dynamics 2 Flashcards
What are the three different types of meridional circulations?
Hadley Cell (important) - hot air rises in the inter-tropical convergence zone (ITCZ) due to shortwave absorption, sensible and latent heating, spreads poleward and cools by longwave emission and sinks over the sub-tropical high
Ferrel Cell
- warm subtropical air moves poleward, rises over cold polar air at polar front and spreads equatorward in the upper atmosphere
Polar Cell
- surface cold-air outbreaks
What are the distribution of surface winds?
Tropics - low pressure, inflows of air from the subtropic at lower atmosphere. Air rises and diverges to the subtropics
Subtropics - high pressure, air converges in the upper atmosphere and sinks towards the lower atmosphere. Outflow of air in the lower atmosphere towards the tropics and the polar fronts
What is the Coriolis Effect?
The deflection of winds that is caused by the Earth’s rotation. Namely, the Earth rotates faster at the equator than at higher latitudes.
- Wind bends towards the right in the Northern Hemisphere
- Wind bends towards the left in the Southern Hemisphere
(Zonal Winds)
What are trade winds?
What are moonsoons?
Trade winds are winds the blow from east to west at the equator. They are caused by the Coriolis effect.
Monsoons are winds that blow in one direction for half a year and in the opposite direction for the other half of the year. They are caused by unequal heating of continents and oceans. (usually refers to Asian monsoon)
(Zonal Winds)
What is the Walker Circulation?
What is the ENSO?
- east-west atmospheric circulation along the equator
- over the pacific ocean
- undergoes interannual oscillations known as the El-Nino Southern Oscillation (ENSO)
La-Nina
- high pressure air from Tahiti flows to low pressure air in Australia
- low pressure air in Australia caused by strong uplifting and evaporation from the indo-Pacific warm pool
- droughts in Peru and Chile
El-Nino:
- High pressure air from Australia flows towards Tahiti
- draughts in Papua New Guinea and Eastern Indonesia
(Zonal Winds)
What are the cyclones formed at the mid-latitudes and the polar front?
Anti-cyclones:
- usually formed closer to the poles
- cold air moves equatorwards and downwards
- surface wind spins outwards
- rotates clockwise in the North (anti-clockwise in the South)
Cyclones:
- usually formed closer to the mid-latitudes
- warm air moves polewards and upwards
- surface wind spins inwards
- rotates anti-clockwise in the North (clockwise in the South)