1.1 Atmosphere As A Global System Flashcards
1
Q
Explain why low latitude locations receive more heat than places close to the poles.
A
- Radiation from the Sun
- Hits Earth
- Earth is sphere
- Radiation is more spread out at the edges (poles) due to the angle of incidence
- Colder
- Radiation is more concentrated at the centre (low latitude) due to the direct trajectory of the rays hitting the Earth
- Hotter
2
Q
How is a high pressure area different to a low pressure area? How does the weather differ?
A
High pressure - air is cooled and so descends - there is more air at the surface ('high' concentration) - good weather (e.g. clear skies) Low pressure - air is warmed and so rises - there is less air at the surface ('low' concentration) -bad weather (e.g. rain)
3
Q
What are atmospheric circulation cells called?
A
Polar cell
Ferrel cell
Hadley cell
4
Q
Where is heat moved from and to? (think poles and equator)
And
How do atmospheric circulation cells move heat around the world?
A
- From Equator to Poles
- Sun heats unevenly causing air to heat and rise in different places (winds)
- Low pressure zone on equator hot air rises and moves to poles
- Wind travels from high pressure belts to low
5
Q
How do ocean currents move heat from the equator to the poles? How does the Gulf Stream work?
A
- warm region to cold region
- winds help transfer heat from equator
- heated water rises whilst cooled water descends
- cycle created (thermohaline circulation)
- deep currents (cold) driven by different densities
- shallow currents (Gulf stream) are warm
- Gulf stream…hot Labrador current…cold
6
Q
Explain how atmospheric circulation causes high pressure areas (dry) places like Tindouf.
A
- cool air sinking from Hadley and Ferrel cell
- creates warm and dry climates with lots of sun
- very arid areas are created
- no moisture and dry surface means little or no rain
- fairly large and direct amount of radiation from the sun so it has high temperatures creating more dryness
7
Q
Explain how atmospheric circulation causes low pressure areas (wet) places like Singapore
A
- located on a Inter-Tropical Convergence Zone
- lots of air is heated as it is on the equator (receives lots of radiation from sun)
- lots of air rises and expands
- rising air is very moist so it condenses when it rises creating cumulonimbus clouds
- lots of extreme rainfall creating wet and moist climate