EAE 15 - Climate Change Flashcards
How do volcanoes affect climate?
2 points.
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
EAE 18aa
What are aerosols?
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
EAE 18ab
What affect do anthropogenic aerosols have?
Anthropogenic aerosols have had an overall cooling effect since pre-industrial
EAE 18ac
What is the impact of ozone?
2 points.
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
EAE 18ad
What is the ozone hole?
- 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
EAE 18ae
What is ther impact of the ozone hole?
2 points.
- 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
EAE 18af
What is the impact of natural variablility?
3 points.
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
EAE 18ag
What is the observed termperature increase?
- 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
EAE 18ah
What are the observations in Australia?
2 points.
- 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
EAE 18ai
Is human influence on the climate system clear?
2 points.
- 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
EAE 18aj
How do we project future climate?
3 points.
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
EAE 18ak
Why do we need more than one model?
3 points.
- 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
EAE 18al
What are some of the changes in quality of climate models?
6 points.
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.
EAE 18am
How do scenarios change over time?
2 points.
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
EAE 18an
What are carbon budgets?
5 points.
- 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
EAE 18ao