History of Climate Change Flashcards

1
Q

What are the importance’s of understanding geological history?

A
  • Establishing a link between CO2 and temperature
  • Provides context for current climate crisis
  • Allows sensitivity of climate models to be studied
  • Demonstrates the central role of life in the earth system
  • Shows how earths environment was different in the past
  • Suggests how life adapts to the environment
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2
Q

How is the link between CO2 and temperature established?

A

Palaeo-temperature proxies: biological (tree rings, fossils) and geochemical (oxygen isotope ratios)
Palaeo-CO2 proxies: biological (phytoplankton, liverworts) and geochemical (boron proxies)

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3
Q

How does knowledge of geological history provide context for the current climate crisis?

A

Can compare with past climatic events, such as the Paleocene-Eocene thermal maximum (PETM)

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4
Q

What was the Palaeo-Eocene Thermal Maximum (PETM)?

A

Happened 56 million years ago
Doubled atmospheric CO2.
Causes warming of 5.C
Decreased phytoplankton abundance

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5
Q

How can equilibrium climate sensitivity be inferred?

A

Using past climates, comparing the temperature between the last glacial maximum and the Holocene using isotope proxies.
Can show expected sea level rise: complete loss of Greenland and West Antarctic ice sheets.

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6
Q

How is life a central role of the earth system?

A

It plays roles in oxygen and carbon cycles.
Photosynthesis has oxygenated the atmosphere.

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7
Q

What was the ‘Green Sahara’?

A

Events during the Holocene and Pleistocene, humid conditions.
Formed lakes, grasslands, forests.

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8
Q

What was ‘Hot house earth’?

A

Ice free Antarctica during Mesozoic.

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9
Q

What are ‘Snowball Events’?

A

When the earth is frozen solid, covered in ice.

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10
Q

What was earths Archaean atmosphere?

A
  • No O2
  • 10 times less CO2 than now
  • High methane concentrations
  • Weak sun
  • Greenhouse effect prevented the earth from freezing
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11
Q

What happened when photosynthesis first occurred?

A

First photosynthetic organisms were prokaryotic cyanobacteria.
Oxygenated the atmosphere, oxygen destroyed earths methane greenhouse effect
Led to an ice-albedo-temperature feedback loop. Earth freezed.

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12
Q

What are some past snowball events?

A
  • Huronian: oxygenation of earth caused drop in methane
  • Sturtian: drop in CO2 due to increased sequestration in the ocean
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13
Q

How have each snowball event thawed?

A

Volcanic CO2 production strengthens the greenhouse effects and thaws the earth.

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