L7 - Water and Temperature

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9 Terms

1
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How does zircon show evidence for liquid water?

  • Zircon is typically formed when granitic magma is solidified

  • This is formed when basalt or mantle material is melted in the presence of water. This proves water must have been present at this time.

  • Zircon = 4.4 billion years old

2
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How does stable isotope fractionation show past climates?

  • As water evaporates, the light 16O molecules evaporate more easily than the heavier 18O molecules.

  • Over time, the water that is evaporating will be enriched in 16O. The water left behind will be enriched in 18O.

  • There is lots of fractionation at low temperatures; less at higher temperatures because molecules in water get more energy rich so it is easier for them to escape into the water vapour phase.

3
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Why does water not escape the atmosphere like other volatiles?

  • As the water moves up through the atmosphere, you would expect UV to break that into H and O2.

  • They are relatively volatile and would be lost from the atmosphere.

  • This does not happen because the ozone layer reacts with UV, absorbs it, and dissipates the energy.

  • UV does not reach water so is not evaporated

4
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How does the water trap prevent water from escaping?

  • Water trap exists in the lower levels of the atmosphere

  • Water freezes and falls as ice and rain as it rises up through the atmosphere

  • Therefore, water is very difficult to lose because water can’t get through the atmosphere: it comes out of the vapour phrase before it gets very high.

5
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How are volatiles recycled?

  • The ocean crust becomes subjected beneath the continental crust - some water will be carried with it.

  • Some of it will have reacted with minerals, and these water-bearing minerals also will have been carried down.

  • Water is released back to the atmosphere through volcanic eruptions.

6
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What is the negative feedback loop that controls temperature?

Higher CO2 (solar luminosity) → higher temperature → increased weathering → reduced CO2 → lower temperature

7
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How did the weathering of the Himalayas act as a temperature control?

  • India collided with the Eurasian plate causing mountain building and the exposure of the continental crust which was weathering, consumed a lot of CO2, and cooled the planet.

8
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What is the ‘snowball earth’ theory?

  • There is evidence of glaciers at the earth’s equator and glacial sediment overlaying warm marine sediments.

  • This happens when continents are located around the earth’s equator.

  • The oceans at the poles freeze quickly and easily, increase the reflectivity of the planet, causing the snowball effect.

  • The earth will continue to degass CO2; eventually, CO2 levels will accumulate, the greenhouse effect will be accentuated, and the ice will melt.

9
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How is earth protected from the sun’s solar wind?

  • Liquid outer core generates the earth’s magnetic field which deflects solar wind

  • This prevents the stripping of volatiles from the earth’s surface

  • Ozone layer absorbs UV, stopping UV reaching the earth’s surface.