Earth's atmosphere Flashcards

1
Q

define atmosphere

A

a layer of gases surrounding Earth or another planet held in place by the planet’s gravity

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2
Q

air is …

A

compressible and one can determine its density

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3
Q

where is the atmosphere at its densest and lowest?

A

densest - sea level

higher altitudes- lower

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4
Q

why is it important for life on earth ?

A

1) it absorbs the sun’s energy
2) recycles water and other chemicals
3) moderates climate
4) protects life from high energy radiation

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5
Q

properties change with height

A

thinner with height with no definite boundary between atmosphere and outerspace
oxygen decreases with height

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6
Q

Name the 5 atmospheric layers

A

1) the troposphere
2) stratosphere
3) mesosphere
4) thermosphere
5) exosphere

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7
Q

the troposhpere

A

1) the air we breathe
2) extends to 15 km high
3) temperature falls with altitude of -50 degrees Celsius
4) all weather is in this region
5) tropopause - separates the troposphere from stratosphere

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8
Q

the stratosphere

A

1) starts above the troposphere and extends 50km above Earth’s surface
2) less water vapour and less dense
3) temperature increases with height -3 degrees Celsius =absorption or radiation
4) ozone layer - absorbs and scatters uv rays
5) the stratopause separates from the mesosphere

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9
Q

The mesosphere

A

1) Just above the stratosphere -extents to 85km
2) temperature falls with increases altitude to about -90 degrees celsius
3) mesospause separates the mesosphere from the thermosphere

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10
Q

the thermosphere

A

1) extends to an altitude of 600 km
2) highly ionized with gases
3) temperatures increasing with altitude up to 1700 degrees celsius

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11
Q

the exosphere

A

1) outermost layer
2) extremely dilute gases ; hydrogen and helium with atoms escaping
3) sometimes considered as the interface between atmosphere and space as it gradually merges into space with no clear boundary

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12
Q

composition of the atmosphere

A
nitrogen 
oxygen 
carbon dioxide 
other gases 
water vapour is also present but varies because warmer air holds more
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13
Q

solar budget

A

The total solar energy received by Earth and the total energy radiated back to space must be equal because Earth’s overall temperature changes

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14
Q

solar constant

A

the amount of solar energy received at the top of Earth’s atmosphere (varies due to slight changes in distance between earth and sun

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15
Q

where does the sun’s energy go ?

A

Half of it is absorbed by the atmospheric gases(ozone and water vapour ) or reflected and scattered by clouds and dust - the rest is absorbed by Earth’s surface

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16
Q

Global circulation

A

Energy transfer with the earth’s atmosphere system - not all parts of earth received the same amount of solar energy ex the poles receive far less than the equator

17
Q

how is heat transferred?

A

heat transfers form warmer to colder areas - the uneven distribution of heat produces convention currents which redistribute heat energy - these convention currents are experienced as winds and ocean currents (otherwise the tropics would get warmer and the poles would get colder )

18
Q

how does it happen exactly ( heat transfer )

A

intense heating at the equatorial region initiates convention currents - this warm air rises at troposphere - flows horizontally towards poles and eventually returning to earth’s surface (30 north and 30 south )
this massive convention current is called the Hadley Cell

19
Q

the 2 other cells

A

the polar cell and the Ferrel cell

20
Q

The albedo

A

the proportion of incident light that is reflected by a surface - depends on the albedo of the surface receiving sunlight

21
Q

what affects the albedo ?

A

1) different colour and texture - clean snow ( high reflectivity ) - forest ( low reflectivity )
clouds - high reflectivity

22
Q

what happens if the planet’s albedo changes

A

increases- cooling of global temperature

decreases - warmer planet

23
Q

The greenhouse effect

A

incoming and outgoing radiation balance out however they have different properties

1) the incoming radiation is a mixture of ultraviolet , visible and infra-red radiation- these radiation are of a short wavelength
2) Earth radiates back heat with a longer wavelength of infra-red radiation
3) Earth’s atmosphere contain gases that absorb some of this thermal radiation emitted - re-radiate energy in all direction - warming effect - greenhouse effect

24
Q

Greenhouse gas

A

a gas that absorbs thermal infrared radiation and therefore contributes to the greenhouse effect

25
Q

Greenhouse effect definition -

A

the warming effect of the atmosphere that occurs when infrared energy is emitted by earth’s surface is absorbed by gases in atmosphere - a fundamental natural phenomenon to life on earth - temperature which sustains life

26
Q

name the greenhouse gases

A

1) water vapour
2) carbon dioxide
3) methane
4) ozone
5) nitrous oxide
6) chlorofluorocarbons

27
Q

sources of greenhouse gases

A

landfills- methane emissions
deforestation - a large amount of carbon dioxide
combustion of fossil fuels - carbon dioxide

28
Q

The ozone layer

A
  • the stratosphere zone -
    protects life from the damaging uv rays
  • the ozone is constantly created and destroyed but because of human activity the increasing rate of destruction is resulting in the disruption of balance - will lead to ozone depletion