Lec 2 - Atmosphere, CO2, Tectonics, Climate Flashcards

1
Q

How thick is the atmosphere?

A

200-400km
relatively thin compared to Earth diameter!

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2
Q

What are the layers of the atmosphere, from the ground up?

A
  • troposphere
  • stratosphere
  • mesosphere
  • thermosphere
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3
Q

What defines the layers of the atmosphere?

A
  • the Temperature Profile (change in temperature with height)
  • pauses in temp profile at the start of each layer
  • ‘inversions’ in the direction of temperature change
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4
Q

In what atmospheric layer does most weather occur?

A

troposphere

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5
Q

How does the thickness of the troposphere vary?

A
  • 8-10km at poles, 16km over tropics
  • due to thermal expansion
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6
Q

What causes the inversion in the temperature profile of the Stratosphere?

A

absorption of UV radiation by ozone, causing hot air to rise

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7
Q

What is the coldest atmospheric layer?

A

mesosphere - radiation absorption only occurs in the bottom layer

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8
Q

What is the atmosphere made of?

A
  • gases
  • suspended particles (aerosols)
  • liquid/solid water
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9
Q

How well are gases mixed in the atmosphere?

A
  • <80km = well-mixed (homosphere)
  • > 80km - separated by gravity (heterosphere)
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10
Q

What are the permanent gases of the atmosphere?

A
  • N
  • O
  • Ar
  • Ne
  • He
  • K
  • Xe
  • H
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11
Q

What are the main variable gases of the atmosphere?

A
  • water
  • CO2
  • O3
  • methane
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12
Q

What classifies a gas as permanent/variable?

A

residence time = reservoir size/flux rate

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13
Q

How abundant is water in the atmosphere?

A
  • ranges from 0-5% of air
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14
Q

How much of the atmosphere is CO2?

A

0.039%

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15
Q

How is CO2 added to the atmosphere?

A

respiration, volcanic activity, decay, combustion

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16
Q

How is CO2 removed from the atmosphere?

A
  • photosynthesis
  • long term: weathering
17
Q

What does ozone do in the atmosphere?

A
  • pollutant in lower atmosphere
  • absorbs UV radiation in upper atmosphere
18
Q

How is methane released into the atmosphere?

A

fossil fuels, livestock, digestion, agriculture (esp rice)

19
Q

What are the two main types of continental chemical weathering?

A
  • hydrolysis
  • dissolution
20
Q

What controls chemical weathering rates?

A
  • temp increases
  • precipitation increases
  • temp/precipitation impact vegetation/productivity
21
Q

What kind of feedback is chemical weathering?

A

negative loop

22
Q

What kind of feedback loop does water vapour cause?

A
  • positive feedback!
  • more water = GHG Effect, so more heating = more evaporation = more water in atmosphere
23
Q

What is the Gaia hypothesis?

A
  • living things regulate climate
  • based on CO2 cycle, photosynthesis affecting weathering, and plankton storing CO2 in shells
24
Q

What is the polar position hypothesis?

A
  • the position of continents determine ‘ice house’ intervals
  • suggests ice sheets should appear on continents near polar latitudes, and no ice sheets should appear outside of these latitudes
  • BUT - based on records, not all continents in polar positions develop ice sheets (ex Pangaea - CO2 compensates for weaker sun, no ice!)
25
Q

How could tectonics control CO2?

A
  • Volcanoes - add CO2
  • weathering - remove CO2
26
Q

What is the BLAG Hypothesis?

A
  • most CO2 in atmosphere is expelled from margins of converging plates (volcanoes), and divergent plates (ocean ridges)
27
Q

Why is there more weathering with more uplift?

A
  • mass wasting
  • earthquakes
  • steep slopes
  • heavy precipitation
  • glaciers
28
Q

How might uplift weathering be a feedback?

A

more uplift weathering means more CO2 removal, but as rocks in other areas age, they remove less and less CO2. Maybe these two effects balance out?