4.a Climate Modelling

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22 Terms

1
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What is a representative concentration pathway (RCP)

A method for GHG scenarios from 2013 onwards

2
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What is the worst case RCP?

8.5

3
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What is the second worst case RCP?

6

4
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What is the second best case RCP?

2.6

5
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What is the best case RCP?

2.6

6
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What was the claim in 2007 made by the IPCC?

The Himalayan glaciers may dissappear by 2035

7
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Why is the IPCC making a false claim bad?

  1. Countries rely on them for information to make climate decisions

  2. Fuels the climate change debate


8
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What do the temps range between for the rise in tem in the next 70-80 years?

0.3C to 4.8C

9
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What is the most likely temp rise?

2C

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What was the level that oceans rose between 1901 and 1990?

1.5mm/year

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What does RPC2.6 say the sea is going to rise by?

0.28m (by end of century)

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What does RPC 8.5 say the sea is going to rise by?

0.98m (by end of century)

13
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Pos Declining forest cover

  • Global temps rise

  • Tropical forests trees become stressed

  • So die

  • Releasing CO2 - trees are a store

  • Resulting in higher temps

  • Which puts more stress on trees


14
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Pos Increased evaporation

  • Warming increases from ocean and land surfaces

  • Atmospheric WV increases

  • Raises global temps

  • Creating further evaporation


15
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Pos Melting permafrost

  • High temps

  • Thawing of permafrost

  • CH4 and CO2 are released

  • Enhanced greenhouse effect

  • Results in more thawing


16
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Pos Increased cloudiness

  • More water in the atmosphere

  • Increases the cover of high altitude cirrus clouds

  • Help to radiate heat from the earth

  • So contribute to temp rises

  • More evaporation


17
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Pos Increased ocean acidity

  • Oceans absorb CO2

  • They become more acidic

  • Increased acidity means that oceans reduce their ability to absorb CO2

  • So more CO2 in the atmosphere


18
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Pos Release of methane hydrates

  • Oceans warm

  • Release of methane hydrates (found in ocean sediments)

  • Methane is 20x more potent than CO2


19
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Pos Reduced albedo

  • High temps

  • Melting of glaciers/ice/snow

  • Reduced albedo

  • More solar radiation absorbed at the surface

  • Temps increase

  • More melting


20
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Neg Increased cloudiness

  • High rates of evaporation and levels of atmospheric EV

  • Incerases cloud cover

  • Leads to an increase in reflection of solar radiation back into space

  • Lower temps occur


21
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Neg Increased aerosols in the atmosphere

  • Burning fossil fuels releases aerosols of smoke/dust/sulphur

  • Aerosols reflect solar radiation back into space

  • Which lowers global temperatures

  • This is known as global dimming


22
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Neg Expansion of forest

  • Temps rise

  • Tree line advances forwards

  • Expansion of forests helps to absorb more CO2

  • Decreases CO2 in the atmosphere

  • Temps decrease