Global Atmospheric Circulation. Flashcards
1
Q
Definition:
A
How air CIRCULATES between low and high pressure belts as a result of differing conditions at different LATITUDES.
2
Q
High-pressure belts of wind: what is the cause?
A
- Cool sinking air.
- MINIMAL rainfall and no clouds.
- this is because the less DENSE air is further from the equator.
- MINIMAL rainfall and no clouds.
3
Q
Low-pressure belts of wind: what is the cause?
A
- Hot rising air.
- Cold air blown from POLES meet warm air surface winds.
- Air SPLITS with some returning back to equator or poles
4
Q
Process: 1st Step.
A
- Earth’s SURFACE warmed by the sun at the equator, transmitting this heat to a nearby air. Air gets hotter and rises forming a LOW-pressure belt
5
Q
Process: 2nd Step.
A
- Rising air COOLS and moves towards 30 degrees north and south.
- (More DENSE) High pressure belt = MINIMAL rainfall and no clouds.
6
Q
Process: 3rd Step.
A
- When cool air reaches the earth’s surface, SURFACE WINDS blow air towards equator OR POLES.
7
Q
Process: 4th Step.
A
- At 60 degrees north and south, cold air blown from poles meet warm air SURFACE WINDS.
- (Less DENSE) Low pressure belt = air begins to cool with water vapour CONDENSING to create RAIN CLOUDS.
8
Q
Process: 5th Step.
A
Air SPLITS - some return back towards equator or to the POLES.