1.12. Changes To The Carbon Cycle Flashcards

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1
Q

Fossil fuel extraction and combustion evidence

A
  • Burning of coal, oil and gas releases 90% of Co2 into the atmosphere
  • Annual emissions are 61% higher than 1990 - China (28%), USA (14%) and India (7%)
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2
Q

How does fossil fuel extraction and combustion affect the carbon cycle?

A

The biosphere and hydrosphere are only able to absorb half of this excess, resulting in the atmospheric carbon store swelling by 80ppm since 1960.

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3
Q

Cement manufacturing evidence

A
  • Cement production releases 5% of all Co2 emissions into the atmosphere
  • For each 1000kg of cement produced, 900kg of Co2 is released into the atmosphere
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4
Q

How does cement manufacturing affect the carbon cycle?

A

Calcium carbonate is heated to separate lime and carbon dioxide -> heat often comes from burning fossil fuels

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5
Q

Farming processes evidence

A
  • 44% of agricultural Co2 comes from Asia, 25% from Americas
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6
Q

How do farming processes affect the carbon cycle?

A
  • Animals release Co2 and methane when respiring and digesting food
  • Ploughing can release Co2 -> microbial activities increase in soil layers inverted by ploughing, resulting in increased respiration
  • Growing rice in paddies releases methane
  • Increased population increases food production
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7
Q

Deforestation evidence

A
  • 13 million hectares of forests cleared for agriculture, logging or way to make developments
  • 3% of forests lost between 1990 and 2005 at 200km squared per day
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8
Q

How does deforestation affect the carbon cycle?

A

Clearance reduces the size of the carbon store and if cleared forest is burned, there’s a rapid flow of carbon from biosphere to atmosphere

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9
Q

Land use change evidence

A
  • Urban areas grow by 1.3 million people every week -> more than 50% of the population
  • 2012: cities responsible for 47% of global carbon emissions
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10
Q

How does land use change affect the carbon cycle?

A
  • Come from switch from natural vegetation to urban surfaces
  • Increased energy consumption for transport, industry and domestic use
  • Cement manufacture for urban dwellings
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11
Q

Carbon sequestration evidence

A
  • Power station built in Canada -> burns coal, captures the emissions and powers 100,000 houses in the area
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12
Q

How does carbon sequestration affect the carbon cycle?

A
  • Injecting captured Co2 as a liquid deep underground into a variety of stores
  • Terrestrial sequestration-> use of plants to capture Co2 from the atmosphere, carbon stored as biomass in stems, roots and nearby soils -> stored carbon can be lost through forest fire -> slow growing and not permanent
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13
Q

Natural wildfires evidence

A
  • Negative feedback loop
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14
Q

How do natural wildfires affect the carbon cycle?

A
  • Rapidly transfer large quantities of carbon from biomass to atmosphere
  • Loss of vegetation decreases photosynthesis so less carbon removed from the atmosphere
  • Long term -> fires can encourage growth of new plants, take in carbon from atmosphere for photosynthesis
  • Fires can have a neutral effect on amount of atmospheric carbon
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15
Q

Volcanic activity evidence

A
  • Recent eruptions have released much less Co2 than human activities (1% of total)
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16
Q

How does volcanic activity affect the carbon cycle?

A
  • Releases carbon stored within the earth in magma in the atmosphere
  • There is potential for a very large eruption to disrupt the carbon cycle significantly
  • Intense Co2 release in the geological past caused enough increase in atmospheric Co2 levels to cause a rise in temperature and possible mass extinctions
17
Q

Natural climate change evidence

A
  • Over the last 2.6 million years, global climates have fluctuated between warm and cold periods
  • Milankovitch cycles - every 100,000 years, Earth’s orbit become more elliptical, triggering ice ages
18
Q

How does natural climate change affect the carbon cycle?

A

During cold periods:
- Carbon stored as biomass would have become incorporated into permafrost = less atmospheric Co2
- Increased chemical weathering (cold water holds more Co2). As a result, more Co2 is transferred from the atmosphere
- Oceans are more saline during cold periods. They take up greater amounts of carbon from the atmosphere via the oceanic pump.