EAE 15 - Climate Change Flashcards

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1
Q

How do volcanoes affect climate?

2 points.

A

Volcanic eruptions can affect climate but primarily act to cool the surface

  • CO₂ emissions from volcanoes currently about 60-100 times smaller than those from fossil fuels
  • Primarily a negative forcing in the short term due to aerosol release

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2
Q

What are aerosols?

A

Aerosols are small liquid or solid particles suspended in the atmosphere

They have a lifetime in the troposphere of 1 day - 2 weeks and their impact on climate depends on many factors

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3
Q

What affect do anthropogenic aerosols have?

A

Anthropogenic aerosols have had an overall cooling effect since pre-industrial

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4
Q

What is the impact of ozone?

2 points.

A

Impacts of ozone variations depend on location

  • Ozone abundance is greatest in the stratosphere
  • Ozone blocks between 97-99% of UV-B and UV-C radiation from reaching the surface

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5
Q

What is the ozone hole?

A
  • Ozone depletion over Antarctica of more than 50% compared to 1980, plateauing during 2000s
  • Stratospheric ozone depletion has only a minor impact on global surface temperatures (lets in more UV but also reduces the infrared trapped)
  • Depletion occurs predominantly in austral spring months
  • Recovery of the ozone hole is projected by mid-late 21st Century

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6
Q

What is ther impact of the ozone hole?

2 points.

A
  • Little direct impact on global surface temperatures from the ozone hole
  • But there is an indirect impact through changes on the Southern Hemisphere atmospheric circulation

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7
Q

What is the impact of natural variablility?

3 points.

A

Natural internal variability of the climate system can change the rate of surface warming

  • Natural cycles like El Niño only move heat from the atmosphere to the ocean or vice versa, otherwise they would violate conservation of energy.
  • We know the atmosphere is warming so to balance that the ocean would need to be cooling
  • But BOTH the atmosphere and ocean are warming

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8
Q

What is the observed termperature increase?

A
  • Global surface temperatures incr by ~1.0ºC since 1900
  • Almost the entire globe warmed between 1901 and 2012
    Multiple lines of robust and compelling evidence support the conclusion that many aspects of the climate system have changed

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9
Q

What are the observations in Australia?

2 points.

A
  • Australian temperatures have risen by a about 1ºC, a similar amount to that of global temperatures
  • Rainfall has declined in the south and increased in the north during their rainy seasons

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10
Q

Is human influence on the climate system clear?

2 points.

A
  • It is extremely likely that human influence has been the dominant cause of the observed warming since the mid-20th century (IPCC AR5)
  • Increased certainty since the IPCC AR4 from a combination of improved observations, models and scientific understanding

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11
Q

How do we project future climate?

3 points.

A

Future climate depends on:

  • inherent variability
  • social & economic choices
  • response of the Earth system

→ use a scenario approach where a variety of potential pathways are examined

→ use comprehensive climate models as they are the best tools available for future projections

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12
Q

Why do we need more than one model?

3 points.

A
  • Diversity of equally plausible approaches to modelling the climate system → no best model!
  • Numerous modelling centres worldwide
  • Attempts to link model performance to projections, for the most part, have proven difficult so multimodel distribution required

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13
Q

What are some of the changes in quality of climate models?

6 points.

A

Compare 1980s, 1990s & mid 2000s

Resolution:

  • 1980s = 500 km
  • 1990s ≈ 200 km
  • 2000s = 110 km

Factors:

  • 1980s = Land, Clouds, Ice
  • 1990s = add Volcanic activity, Sulphates & Ocean
  • 2000s = add Chemisty and Interactive vegetation.

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14
Q

How do scenarios change over time?

2 points.

A

By the end of the 21ˢᵗC

  • Global temperatures are likely to exceed 1.5°C for all RCPs (except RCP2.6)
  • Global temperatures are likely to exceed 2°C for RCP6.0 and RCP8.5

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15
Q

What are carbon budgets?

5 points.

A
  • Every ton of CO₂ causes about the same amount of warming, no matter when and where it is emitted
  • To limit warming to likely less than 2°C from CO₂ alone, total emissions since preindustrial need to be limited to less than 1000 GtC
  • Accounting for non-CO₂ forcing as in RCP2.6 reduces the allowed cumulative emissions to about 800 GtC
  • About 530 GtC were emitted by 2011
  • CO₂ emissions from permafrost or a higher likelihood require a lower budget

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16
Q

What was the average CO₂ in the atmosphere in 2017?

A

The global annual mean concentration of CO2 in the atmosphere in 2017 was ~405 parts per million

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17
Q

What is the increase in CO₂ by 2017?

A

A 46% increase since 1750 and higher than at any time in at least the past 2 million years

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18
Q

What is the dominant contributor to CO₂?

A

Emissions from burning fossil fuels continue to increase and are the dominant contributor to the observed growth in atmospheric CO₂

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19
Q

What was the Impact of COVID-19 pandemic on CO2 emissions?

A

Liu et al found that emissions dropped by 8.8% over the first six months of 2020 in comparison to 2019

COVID-19 is projected to lead to a 0.4 ppm drop in CO₂ concentrations in the atmosphere this year compared to previous projections for 2020 UK Met

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20
Q

What is the projection of CO₂ concentrations as emissions change?

3 points.

A
  • Zero CO₂ emissions lead to near constant surface temperature
  • A large fraction of climate change persists for many centuries
  • Depending on the scenario, about 15-40% of the emitted carbon remains in the atmosphere for 1000 years

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21
Q

What is the impact of COVID-19 pandemic on temperatures?

2 points.

A
  • Along with a decrease in GHG emissions, COVID-19 has also led to a drop in SO₂ emissions, which would normally cool the atmosphere.
  • The net effect results in a negligible impact on global temperatures.

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