Climate Change Flashcards
(33 cards)
The greenhouse gases
Carbon dioxide, CFCs, methane, nitrous oxide, ozone, water vapour.
The enhanced greenhouse effect
As global temperatures rise, so too does water vapour. Increasing global temperatures leads to greater evaporation of water which then leads to greater levels of condensation. Cloud cover increases which traps heat in the atmosphere.
The greenhouse effect
The earth intercepts the suns radiation, about 30% of it is reflected back into space. Some radiation is absorbed by the earths surface and some is re emitted by green house gases which warms up the earths atmosphere
Volcanic causes of climate change
Major eruptions eject material into the stratosphere where high level winds distribute it around the earth. Volcanoes eject huge amounts of ash, sulphur dioxide, water vapour and carbon dioxide.
The milankovitch cycles
Earths orbit changes from a circular shape to an elliptical shape over 100,000 years which changes the amount of radiation the earth receives.
Solar output
The amount of energy emitted by the sun varies as a result of sunspots. Dark spots appear on the surface of the sun as a result of magnetic storms.
More sunspots means more solar radiation towards the earth.
The stern review
Focused on the impacts of global warming and the actions need to take. The key features were: environmental impacts, economic impacts, options for change and UK government response.
Case study: London’s climate change strategy.
In 2007 plan was to reduce co2 emissions by 30% of 1990 emissions by 2025.
What was proposed?
Green homes programme.
Setting and enforcing new building standards for energy efficiency.
Investing in local renewable energy.
Encouraging “waste to energy” schemes.
Promoting purchase of low carbon goods
Case study: BedZED
Housing development which aims to be carbon neutral.
The homes use heat efficient, natural materials.
Has it’s own CHP plant.
What long term evidence is there for climate change?
Carbon dioxide levels - sampled from bubbles in ice cores.
Oxygen isotope levels - sampled from ice cores.
Pollen - extracted from peat bogs or lake beds.
What medium term evidence is there for climate change?
Historical records - analyse paintings, written accounts etc…
Tree rings - trees are sensitive to changes in temperature, sunlight etc…
Retreating glaciers - valley glaciers grow and shrink in response to climate change.
What is short term evidence for climate change?
Instrumental methods - thermometers, satellites etc…
Green strategy: afforestation
Planting trees - trees act act carbon sinks.
Destruction of trees releases co2 into the atmosphere.
However in order to plant more trees, land users will have to make way which could disrupt agriculture, jobs etc…
Green strategy: renewable energy projects.
Eg. The three gorges dam in China. Provides green energy but causes social problems such as relocation of residents and destruction of cultural sites.
Biofuel crop projects produce renewable energy but take up huge areas of land. Eg. In Brazil.
Case study: Community based green strategies in Oxfordshire.
ClimateXchange Oxfordshire has acted as a catalyst in lowering the areas carbon footprint…
Each road has waste champions who organise rubbish swaps.
Information is circulated to the 10 most effective ways in reducing co2.
Green transport is being introduced.
Cloth bags available in order to cut down plastic bag use.
Carbon offsetting
“Carbon credits”. It allows companies to pollute but at a cost. Each credit costs money which the polluter has to pay. It encourages companies to look for other means of production.
Climate Feedback
Can either amplify a small change and make it larger (positive) or
diminish the change and make it smaller (negative). An example of positive is snow and
ice cover. Small increases in snow and ice raise surface albedo so more solar energy is
reflected. This causes cooling.
An example of negative is cloud cover, as global warming occurs, more evaporation will
occur and this many increase global cloud cover.
Global Dimming?
Atmospheric pollutants reflect solar energy back into space and so have a net cooling
effect. Greenhouse gases reflect outgoing back to earth and so have a net warming effect.
It is possible that humans are both warming and cooling the planet.
Why is there uncertainty is predicting emissions and their impacts?
The level and nature of economic development, especially in countries like India
and China, this will determine greenhouse gas emissions s.
What international action will take place to reduce emissions.
The inertia of the system, even if greenhouse gas emissions stabilise , climate
change will continue.
Tipping point
this is reached when climate change occurs irreversibly and at an
increasing rate. Increasingly scientists are talking about visible manifestations of the
tipping point, such as the loss of ice sheets or the destruction of the Amazon rainforest. All
these visible changes will lead to catastrophic changes.
Mitigation
Reducing the output of greenhouse gases and increasing the size of
greenhouse gas sinks. For example:
Setting targets to reduce carbon dioxide emissions
Switching to renewables.
Capturing carbon emissions from power stations and storing them.
Adaption
Changing our lifestyles to cope with a new environment rather than trying to stop climate change. For example: Managed retreat of coastlines. Develop drought resistant crops. Enlarging existing conservation areas
For human systems: adaption or mitigation?
For human systems like the economy, Mitigation would involve an upfront cost, to reduce
the atmospheric pollution to ‘safe’ levels.
Adaption might mean that costs were spread over a longer time scale.
For natural systems: adaption or mitigation?
For natural systems like ecosystems, mitigation could limit damage.
Adaption might condemn natural systems which could not adapt to a changing climate.
Species may become extinct, and biodiversity be degraded as threats to ecosystems
increased