Flash Cards Geography Climate

1
Q

Structure of Atmosphere?

A
  1. Troposphere
  2. Stratosphere
  3. Mesosphere
  4. Thermosphere /Exosphere
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2
Q

Temperature Inversion?

A

Area where temperature changes in reverse direction

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3
Q

Inversion?

A

When temperature increases with altitude

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4
Q

Positive Lapse Rate?

A

When temperature decreases with height

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5
Q

Negative Lapse Rate?

A

When temperature increases with height.

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6
Q

Troposphere?

A
  1. Layer we live in
  2. Contains weather- water vapour/clouds
  3. 17km at equator and 8km at poles
  4. Temperature decreases with altitude
  5. Upper limit-Tropopause
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7
Q

Stratosphere?

A
  1. Characterised by steady increase in temperature, due to high concentration of ozone which absorbs Uv radiation
  2. Upper limit-Stratopause
  3. Protective shield against meteorites
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8
Q

Mesosphere?

A
  1. Temperature drops rapidly with height as there is nothing to absorb it. No ozone or water vapour
  2. Winds extreme
  3. Upper limit-Mesopause
  4. Least understood too high for aircraft and low for spacecraft
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9
Q

Thermosphere?

A
  1. Thickest layer with the lightest gases
  2. Scattered molecule absorb UV propelling them at high speed and temperature causing temperatures like 1500C
  3. ISS orbit
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10
Q

Exosphere?

A
  1. Explains a and contracts causing it too come into contact with solar storm, causing explosive events/ solar flares
  2. Weather satellites
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11
Q

Gases?

A

Permanent- Nitrogen, O2, Argon

Variable- Co2, Methane, Ozone

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12
Q

Solids?

A

Pollution particulate, dust, pollen, plastic, salt, silica

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13
Q

Mass and Weight?

A

Individual molecule have mass therefore weight due to gravity- exerts pressure on surface

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14
Q

Compressibility?

A

Lower layers more compressed. When air is heated it expands reducing compression. Air is cooled it contracts increasing compression

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15
Q

Mobility?

A

Attempts to equalise pressure causing wind. Horizontal-advecation, Vertical-convection

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16
Q

Insolation?

A

Incoming Solar Radiation. The energy the sun gives off as shortwave radiation.

17
Q

Energy Transfer?

A
  1. Terrestrial or Longwave Radiation- warms atmosphere from below
  2. Conduction- heat is passed from one molecule to another or from surface to air by direct contact.
  3. Convection- heater air become less dense and rises and cool air sinks in to replace it.
  4. Latent Heat- energy is water vapour that is radiated when it condenses.
18
Q

How is insolation lost?

A
  1. Absorption- upper layers absorb deadly radiation. Ozone, vapour, dust.
  2. Scattering- dust scatters radiation and cause sunsets by scattering visible light.
  3. Reflection or Surface Albedo- reflect sunlight back , lighter reflects better.
19
Q

Greenhouse Effect?

A

Natural process made possible by gases in Earths atmosphere. They trap heat and reflect it back down to Earths surface. Prevents Earth from cooling too much.

20
Q

Greenhouse?

A

Sunlight enters glass as shortwave radiation. Converted to longwave and traps heat.

21
Q

What caused large amounts of greenhouse gases to be released?

A

Industrial Revolution in 1700s and 1800s

22
Q

Uses for Greenhouse Gases?

A

Co2- fossil fuels burned
Methane-livestock farming
CFCs- Aerosols and Polystyrene
Ozone-Smog reacting with organic compounds
Nitrous Oxide-Agriculture

23
Q

Global Warming?

A

The increase of the Earths surface temperature due to the emissions of greenhouse gases.

24
Q

Carbon Cycle?

A

Carbon is essential for life. It is stored in oceans, plants, atmosphere and rocks. Carbon is recycled for photosynthesis and when ingested. When they die their remains deconpose and turn into rocks, minerals and fossil fuels. Released back into atmosphere when burnt.

25
Enhance Greenhouse Effect?
Man-made influence on Earths greenhouse gases.
26
Evidence of Greenhouse Effect?
Co2 concentration higher over pure sea air Antarctic sea ice diminishing Earths 1C warmer than 100yrs ago Glaciers retreating
27
Causes of Global Warming?
Increased industrialisation- fossil fuels being burnt Deforestation- fewer trees to absorb CO2 Increased populatio. more resources used Increased cattle herds- emits more methane Increased rice production- grown in flooded field, anaerobic conditions ideal for bacteria breaking decomposing organic matter, releasing methane Reduction of oceans absorb too of CO2
28
Global Warming impact of Environment?
Intense heatwaves Melting of Artic ice Coral Bleaching Unreliable weather Reduction of habitat
29
Effects of Ozone Depletion?
Human- skin cancer, eye cataracts, lowered immune system Environment- altered weather, surface temperature and reduction of crop yields
30
Chlorofluorocarbons?
Aerosols and polystyrene 1. UV causes chlorine to break from CFC molecule 2. Chlorine hits ozone molecule 3. Chlorine pulls 1 oxgen atom away 4.Another free oxygen atom hits chlorine monoxide molecule 5. Results in free chlorine atom that continues to deplete ozone