global atmospheric circulation Flashcards
what factors affect a places climate?
- high/low latitude
- altitude
- coastal/inland
- east/west
- rural/urban
do places at low latitude near the equator have high or low levels of insolation and why?
- higher levels of insolation
- this is because the rays are spread over a smaller area
do the poles (higher latitude) have high or low levels of insolation and why?
- lower levels of insolation
- this is because the suns rays are spread over a greater distance
warm air ……..
rises because its less dense than cool air
cool air ……..
sinks because its more dense than warm air
rising air creates …
low pressure
sinking air creates …
high pressure
what creates wind?
air particles moving from areas of high pressure to areas of low pressure
how do clouds form?
- warm air rises
- as the air rises it cools
- clouds form and eventually release precipitation
what is the most important factor affecting climate?
latitude
what are the 3 convection cells in the Northern and Southern Hemisphere?
Hadley cell, Ferrel cell, Polar cell
where is the Hadley cell located?
between the tropics and the equator
what are jet streams
high altitude currents of air (wind)
what direction do winds flow and why?
West -> East
because of the spin of the earth
what is global atmospheric circulation
the transfer of hear from the equator to the poles by the movement of air
why does air move
due to differences in air pressure - winds blow from high pressure to low pressure areas
what does each cell have
a warm rising air that creates a low pressure belt and cool sinking air that creates a high pressure belt
how does air move in the cells:
- the sun warms the earth at the equator, causing the air to rise. this creates a low pressure belt
- as the air rises it cools and move away from the equator
- 30 degrees north and south of the equator, the cool air sinks, creating a high pressure belt
- at the ground surface, the cool air moves either back to the equator (as trade winds) or towards the poles (as westerlies). these winds curve because of the earths rotation - this is called the Coriolis effect
- 60 degrees north and south of the equator the warmer surface winds meet colder air from the poles. the warmer air rises, creating low pressure
- some of the air moves back towards the equator, and the rest moves towards the poles
- at the poles the cool air sinks, creating high pressure. the high pressure air is then drawn back towards the equator.
what does global atmospheric circulation influence
climate and weather around the world
climate at equator and explanation:
at the equator the sun is directly overhead - this means the earths surface receives a lot of solar radiation, so its hot. warm, moist air rises and forms clouds, so it rains a lot
climate at 30 degrees north and south of equator and explanation:
by the time air reaches 30 degrees north and south of the equator, it had released most of its moisture as rain. the dry air means there are few clouds and little rainfall, so deserts are often found at this latitude
climate at 60 north of equator and explanation:
the UK lies close to the low pressure zone at 60 degrees north. warm rising air brings lots of cloud cover and rainfall, often as low pressure systems carried from the Atlantic by westerly winds.