climate change - 1 Flashcards
What is Climate change?
- Climate change refers to a statistically significant variation in either the mean state of the climate or in its variability, persisting for an extended period - typically decades or longer.
- Climate change may be due to natural internal processes or external forcing, or to persistent anthropogenic changes in the composition of the atmosphere or in land-use.
- Global climate change is a serious and urgent issue.
Global warming and climate change
- Global warming causes climate change
- Global warming is a problem in which the combustion of coal, oil and other fossil fuels causes the atmospheric concentrations of GHGs such as carbon dioxide, to increase.
- This results in mounting global air temperatures that lead to climate change
The basic science behind global warming - The Greenhouse effect
- Global warming is caused by greenhouse gases (GHG), a type of global pollutants
- The three most anthropogenic greenhouse gases are CO2, methane(CH4 ) and nitrous oxide (N2O), the levels of which have risen since the Industrial revolution.
- The sun sends energy in every direction some of which reaches the planet earth
- These global pollutants absorb the long-wavelength (infrared)radiation from the earth’s surface and atmosphere, trapping heatthat would otherwise radiate into space. Hence it is harder for energy to leave the planet than if there were no GHGs.
- This warms earth surface 30°C above normal
Global warming over the years
- The world is now more than 1.10 C warmer than it was in late 19th century.
- Human activities - mostly post-industrial revolution, have changed the composition and level ofGHG in atmosphere.
- CO2 : 280 ppm (pre industrial) to (approx.) 430 ppm today! I.e. it has risen by 50% since the startof Industrial Revolution and it is increasing by 2 ppm each year! (ppm: parts par million – a measure that describes small concentration of substance in a large solution)
- Highest concentrations of GHG for 650,000 years!
- Even if concentrations remained constant from now on, the global temperature would still rise by 1-30 C above pre-industrial levels
Global warming stats
- Atmospheric accumulations of GHG stays there for a long time
- The rate of warming currently at 0.130C per decade is increasing.
- IPCC (Intergovernmental panel on climate change) projects a temperature change of 1.50C to4.80 C by 2100!
- The global increases in CO2 concentration are due primarily to fossil-fuel use (e.g. in transport, energy, industries) and land-use (deforestation) changes; whereas methane and nitrous oxide concentrations arise primarily from agriculture
- Emissions are increasing at an increasing rate!
Observed impacts and changes - Ocean warming and acidification
- Ocean warming dominates the increase in energy stored in the climate system, accounting for more than 90% of the energy accumulated between 1971 and 2020.
- Since the beginning of the industrial era, oceanic uptake of CO2 has resulted in acidification of the ocean; the pH of ocean surface water has decreased by 0.1corresponding to a 26% increase in acidity.
Observed impacts changes - surface temperature
- Each of the last three decades has been successively warmer at the Earth’s surface than any preceding decade since1850.
- The globally averaged combined land and ocean surface temperature data show a warming of 0.85 [0.65 to 1.06] °C over the period 1880 to 2012.
Observed impacts and changes - Sea level rise, declining Arctic sea, shrinking ice sheets
- Over the period 1901–2010, global mean sea level rose by 0.19 [0.17 to 0.21] m
- The annual mean Arctic sea-ice extent decreased over the period 1979 to 2012, with a rate that was very likely in the range 3.5 to 4.1% per decade.
- Greenland and Antarctic ice sheets have been loosing mass, glaciers continue to shrink.
Projections and future impacts of climate change
- Consequently, people’s lives are changing where the poorest and most vulnerable countries are affected worst despite they usually being the lowest emitters.
- E.g. East Africa has suffered their worst draughts over 40 years, putting more than 20 million people at severe hunger; in 2022 and 2023 European heat waves led to abnormal increase deaths
How will future climate change affect our world?
Limiting long-term temperature rises to 1.50 C is absolutely crucial because the consequences of20 C vs 1.50 C could imply more frequent occurrences of extreme events including the following:
Sea-level rise would be 0.1m higher than at 1.5C, exposing up to 10 million more people to events including more frequent flooding
Loss of land and forest areas including coral reefs and wetlands => loss of species, extinction of flora and wildlife, marine lives: More than 99% of coral reefs would be lost, compared with70-90% at 1.5C; Loss of agricultural outputs due to draughts.
Impacts on people: Disruption of water supplies to cities and agriculture; Health damageand deaths due to spread of vector-borne diseases such as malaria, flooding and extremeheat. Several hundred million more people will be exposed to climate-related risks and susceptible to poverty by 2050 than at 1.5C.
Threshold effects known as Tipping points will create irreversible changes such as complete destruction of ecosystems in the long run if crossed.
Long term impact on growth and development especially in the poorer countries
Net Zero
reducing greenhouse gas emissions as much as possible, and removing any remaining emissions from the atmosphere i.e. all emissions released by human activities are counterbalanced by removing carbon from the atmosphere in a process known as carbon removal
Paris agreement
- In a landmark agreement signed inParis in 2015, almost 200 countries pledged to try to keep global warming to 1.5C.
- To achieve this, “net zero“ CO2emissions need to be reached by2050.
- Unfortunately we are nowhere near achieving this.
- In the most recent UN climate change summit, COP28 held in theUAE, countries for the first time, agreed to contribute to”transitioning away from fossil fuels”, although they are not forced to take action!!
Pollution targets
o maximising social welfare
o economic efficiency
o sustainability
o minimisation of health risk
Pollution flows, pollution stocks and pollution damage
o Pollution can be classified in terms of a damage mechanism.
o Damage can arise from the flow of pollution i.e. the rate of emission; or from the stock (or the concentration rate) of pollution in relevant environmental medium.
Flow-damage pollution
Flow-damage pollution occurs when damage results only from the flow of residuals i.e. the rate at which they are being discharged into the environmental system.For pure cases of flow-damage pollution, the damage will drop to zero if emissions flows become zero: e.g. noise or light pollution.
D = D(M)