Atmosphere: The Global Heat Budget Flashcards
most significant layers of atmosphere (2)
- troposphere
- stratosphere
troposphere
- contains most atmospheric moisture
- most air, water vapour and dust
stratosphere
- contains ozone gas which filters out the most harmful UV radiation
total insolation reflected
30%
total insolation absorbed
70%
total insolation absorbed by the earth
51%
insolation can be reflected/absorbed by… (3)
- clouds
- atmospheric particles
- earth’s surface
different rates of reflection can be explained by… (3)
- different cloud cover
- whiteness of snow/ice in polar areas
- deserts
different rates of absorption can be explained by… (2)
- smog over cities
- dark surfaces of ocean and rainforest in tropical areas
how does earth’s curvature affect the angle of insolation?
- at the equator, insolation hits the earth at a right angle and is more intense
- at the poles, insolation hits the earth at an oblique angle and is weaker
how does earth’s curvature affect the area of insolation?
- at the equator, insolation is concentrated on a smaller area
- at the poles, insolation is spread out over a larger area
how does earth’s curvature affect the amount of atmosphere that insolation has to travel through?
- at the poles, insolation has to travel through more atmosphere, so more energy is lost
- at the equator, insolation has to travel through less atmosphere, so less energy is lost
how does the Albedo effect affect the amount of insolation received by the poles/equator?
- at the poles, the whiteness of ice and snow reflect the solar radiation
- at the equator, the dark colour of the oceans and rainforest absorb solar radiation
how does seasonal variation affect the amount of insolation received by high/low latitudes?
- at lower latitudes in the tropics, the sun is high in the sky all year, so high amounts of insolation are received all year
- at higher latitudes, there are distinct hot and cold seasons, so some areas receive less insolation for several months a year