Lecture 8: Climate Change Flashcards
1
Q
How is the climate changing?
A
- Always undergone periods of stability and change.
- Climate has generally been warmer than it is today, but ecosystems adapted for current conditions.
- Life likely to go on even with extreme climate change, just may have extinctions.
- Many previous period’s of rapid climate change are associated with mass extinctions.
1. Ordovician - rapid cooling & sea level change
2. Devonian - changes in sea level & ocean hypoxia, possibly triggered by global cooling
3. Permian - a large meteor impact, massive volcanism, & rapid warming
4. Triassic - climate change, flood basalt eruptions, and an asteroid impact
5. Cretaceous - asteroid impact (odd one out)
6. Now
2
Q
How is the climate changing?
A
- After period of being relatively cool, we experiencing rapid warming, this happened since the 1780s (start of Industrial Revolution - burning fossil fuels).
- Past warming has been much slower: 4 - 7 ˚C over ~5000 years when moving out of ice ages.
- Now ~ 10 times faster
- Now at ~1.2 ˚C above pre-industrial levels.
3
Q
Causes of climate change: anthropogenic
A
- The Greenhouse Effect (when light from the sun hits a planet e.g. earth, some goes to warming the surface but a lot is reflected back into space, in the atmosphere (around earth) have greenhouse gases that prevents heat from escaping into space, making temperature more stable over night). But anthropogenic-related increases in greenhouse gases are leading to rapid increases in global temperatures.
4
Q
Causes of climate change: anthropogenic
A
- Extensive climate modelling has shown humans are driving rapid warming.
- When looking at natural drivers (solar radiation, volcanic activity) wouldn’t expect much change in temp. If add human drivers (changes in green house gases) would increase temp.
5
Q
Causes of climate change: anthropogenic
A
- Main greenhouse gas driving temp rise is CO2.
- In past couple hundred years CO2 risen hugely.
- Now average ~419ppm April-June 2021.
- Almost entirely from burning fossil fuels. (Some from land use e.g. cutting down / burning forests).
6
Q
Causes of climate change: anthropogenic
A
- Methane is next largest contributor.
- atmospheric concentration increased by ~ 150% since 1750.
- Sources include: livestock production - belch methane (there’s work to see if we can create foods for livestock that reduces this) , waste management (produced as part of the decaying process), release from sediments e.g. (as areas of Artic warm and the ground defrosts its realising methane) in Artic, previously encased permafrost.
7
Q
Environmental consequences
A
- Warming is not occurring evenly across globe.
- Most warming is on land rather than at sea.
- Certain areas warming particularly fast.
8
Q
Environmental consequences
A
- Doesn’t just affect temp, patterns of rainfall also changing rapidly.
- Some areas getting wetter (prone to flooding), some dryer (desertification).
9
Q
Environmental consequences
A
- Sea ice is melting, especially in Artic.
- Nearly halved in just 100 years.
- Polar bears not able to find enough food so starving.
- Hasn’t reduced so much in the Antarctic, but is mostly land.
10
Q
Environmental consequences
A
- Sea levels are rising. Low lying areas vulnerable, some islands may disappear completely.
- ## oceans becoming more acidic. (CO2 reacts with the water)
11
Q
Environmental consequences
A
- An increase in extremes of heat, heavy rainfall & agricultural / ecological drought.
12
Q
Future climate change
A
- Climate depends on what we do now.
- currently at 1.2 ˚C above preindustrial levels.
- Could reach 4 ˚C by end of century unless large changes are made on a global level.
- Isn’t distributed evenly so will have a huge impact in certain areas.
- Same with precipitation.
13
Q
Responses to climate change
A
- Environmental change alters the adaptive peak of high fitness.
- Species need to change accordingly or risk extinction.
- To get there can change: a) Spatial distribution (move to diff area) b) Local phenotype (behaviour, physiology) c) Phenology (timing of life events).
14
Q
Responses to climate change: Extinction
A
- If species unable to change rapidly.
- Future extinctions depend on extent of climate change. a) ‘Business as usual’ approach (don’t change) will lead to 4 - 4.5 ˚C changes. b) assumptions made when making predictions.
- Many predictions come from models of species distributions under predicted future climatic conditions.
- As temp increases more species at risk of extinction.
- If does reach over 4 ˚C then is likely 15% of species extinct.
- Mean extinction risk is 7.9% with a 95% confidence interval.
15
Q
Responses to climate change: Extinction
A
- Some taxonomic groups & locations more vulnerable than others.
- Amphibians & reptiles particularly vulnerable. (Probs because they terrestrial endotherms - regulate body temp based on environment so more vulnerable to temp changes).
- Many have temp-dependent sex determination.
- Areas with many endemic species that have small ranges are vulnerable (e.g. Africa).