p11 Flashcards
an uncertain future - Factors affecting Certainty
Physical factors
Human factors
Feedback mechanisms
Physical Factors
Oceans and forests act as carbon sinks.
Their response to increased GHG emissions and higher temperatures will continue to affect the global climate for possible hundreds of years.
Deforestation - overall the amount of forested land is on a global decline.
Human factors
These factors include:
- economic growth
- population growth
- energy sources used.
The IPCC has identified some key factors driving anthropogenic GHG emissions, shown in Figure 6.9.
Economic growth:
After economic crashes, e.g. the 2008 Financial Crash, there is an expectation that they’ll be a rise in emissions during recovery of global GDP. Fortunately after 2008, emissions fell to 1% by 2012-13 down from 4%, then fell to 0.5% in 2014. Total carbon emissions still reached a record high.
Human Factors – Example Economic growth
By 2014 the three largest CO2 emitters were China, the USA and India. In 2000, China overtook the USA because of a global shift in manufacturing projections and its rapid urbanisation and industrialisation.
In terms of CO2 per capita, China is ranked 55th at 6.23 metric tonnes per capita; the USA 8th at 17.6 and India 127th at 1.7 – reflecting the level of economic development, with a positive relationship between economic growth and CO2 emissions.
However, the Kuznet Curve suggests it’s not as straight forward!
Energy Source:
Energy consumption grew by 2% between 2008-2014. However renewables made up two-thirds of the increase in electricity production in 2015.
Population Change:
Increasing affluence means a potential extra billion consumers by 2050. Changing diets and increase mobility means more emissions.
Feedback Mechanisms
Feedback mechanisms can either dampen (negative feedback) or amplify (positive feedback) responses to a changing climate.
includes Peatlands: Permafrost:
Peatlands:
Warming causes peat to dry out as water tables fall, increasing decomposition rates and releasing methane. A warming of 4˚C causes a 40% loss of soil organic carbon from shallow peat, and 86% from deep peat.
Permafrost
The melting of permafrost releases trapped CO2 and methane.
Tipping Points
A climate tipping point is a critical threshold whereby a carbon sink could become a carbon source.
Two particular phenomena are capable of creating tipping points
Forest die back
Changes to thermohaline circulation
Forest die back
Rainfall in the amazon basin is largely recycled from moisture within the forest. If the rainforest is subject to drought, trees die back.
A tipping point can be reached when the level of die back actually stops the recycling of moisture – resulting in further die back.
Thermohaline circulation
- Increased melting of northern glaciers and ice caps would result in large amounts of non-salty, less dense water entering into the oceans.
- This would disturb the conveyor belt of hot water moving from the tropics to the cold water from the poles.
- The change in the thermohaline system may result in cooling of temperatures in the Northern Hemisphere.
Future changes to carbon stores
Terrestrial sinks
Modelled to increase generally until 2050
When saturation is reached they begin to act as sources:
* thawing tundra permafrost in the Arctic
* shift of boreal forests to the north as tundra thaws; these may be able to store more COz if more nutrients (nitrogen) available
* tropical rainforests are already at their carbon capacity and may reduce their storage, especially after drought
Future changes to carbon stores
Oceanic sink
Increased store in sea grasses and algae, but overall reduction as sink because:
* tropical oceans have decreased COz solubility because they are warming, so less uptake of CO2
* decreased efficiency and slowing down of the biological pump taking nutrients and dissolved inorganic carbon from the surface to ocean floor sediment sink
Key concept: Climate forcing
Predictions are uncertain because changes to the climate have several causes and feedback mechanisms. Increasing GHGs, changes in volcanic aerosols and ozone levels all cause similar circulation changes in models of the atmosphere.
Facing the Future
Even if greenhouse gas emissions were to stabilise or even fall, the planet would continue to warm.
Therefore it’s important to assess consequent changes, whilst trying to prevent them from worsening.
The IPCC outlined two approaches for the future:
Adaption
Mitigation
Adaption
Adopting new ways of doing things in order to live with the likely outcome of climate change.
Mitigation:
Involves the reduction or prevention of GHG emissions by new technologies e.g. renewables
The more CO, there is in the atmosphere,
the greater the effects on Earth’s systems, and hence the more difficult adaptation will be.
specific adaptation strategies for a changed climate
costs and benefits
Water conservation and management
Resilient agricultural systems
Land-use planning
Flood-risk management
Solar radiation management
Water conservation and management
benefits
Less resources used, less groundwater abstraction
Attitudinal change operates on a long-term basis: use more grey water (recycled water)