Skip to content
Dabour HubLEARN · PRACTICE · EXPLORESign inStudent

12.4Chapter 12: The Carbon Cycle and Climate Change

Predicting the future — Alhussan Biology - Stage 9 Revision Notes & Topical Questions

5 min read 8 parts Lesson 4 of 6 2 quizzes

🩺
100% Curriculum Specification Match Lesson Doctor Verified
The only platform with 100% curriculum specification match and verified interactive question banks.
0%read
Lesson summary

12.4 Predicting the future — Computer Climate Models — Alhussan International Academy — Biology (Stages 7–9) notes: Describe predicted impacts of future climate change and how computer climate models are built, tested and evaluated.Svante Arrhenius — in the 1890s he calculated th…

  • IPCC (Intergovernmental Panel on Climate Change)
  • Prediction
  • Droughts and heat waves
  • Wetter regions
  • Temperature changes
  • Extreme weather

Part 1 of 6IPCC and the greenhouse effect

IPCC and the greenhouse effect
Svante Arrhenius
  • Svante Arrhenius in the 1890s he calculated that doubling atmospheric carbon dioxide would make the Earth's surface 5 °C warmer, seriously affecting the climate.
  • His predictions are coming true in the 21st century.
IPCC (Intergovernmental Panel on Climate Change)
  • IPCC (Intergovernmental Panel on Climate Change) it studies evidence from thousands of scientists worldwide and advises governments.
  • It states that global warming is happening because of human activities such as burning fossil fuels and deforestation,
    • which raise carbon dioxide and other greenhouse gases.
Prediction
  • Prediction by the middle of the 21st century global temperatures will rise by another 1.3-1.8 °C.

Part 2 of 6Predicted impacts

Sea level
  • Sea level as oceans warm and land ice melts, some scientists predict a rise of between 26 and 82 cm by the end of the 21st century.
  • Low-lying countries such as Tuvalu, and areas of many other countries, will disappear beneath the sea.
Droughts and heat waves
  • Droughts and heat waves as temperatures rise and rainfall patterns change, huge areas will become infertile and dry and arid land will expand.
  • Species will die out where there is no water, people will starve and fires will destroy whole ecosystems.
Wetter regions
  • Wetter regions many parts will get more rain and snow than ever before, often as extreme storms or blizzards.
  • This will cause floods that wash away fertile soil and cause loss of homes and lives.
Temperature changes
  • Temperature changes some countries will get hotter and others colder.
  • Warmer places will support pests such as mosquitoes, ticks and crop pests, affecting health and agriculture.
  • Plant life, animal migration patterns and local species will change, and many species will become extinct.
Extreme weather
  • Extreme weather hurricanes and storms will happen more often, and a single storm can badly damage power supplies, buildings, roads and railways.
Hope
  • Hope only a third of the predicted temperature rise for the next half century will happen for certain,
  • so changing how we live may stop climate change before it cannot be undone.

Part 3 of 6What a climate model is

Climate model
Climate model a computer program that uses mathematical equations to represent the processes that control the climate.
Grid
  • Grid the Earth is divided into a three-dimensional grid of boxes covering atmosphere, ocean, land and ice.
  • For each box the model calculates temperature, pressure, humidity, wind and other quantities,
    • and how energy and water move between neighbouring boxes through time.
Computing
  • Computing there are billions of calculations, so very powerful supercomputers are needed.

Part 4 of 6Inputs and outputs

Inputs
  • Inputs energy from the Sun, greenhouse gas concentrations, aerosols from volcanoes and pollution, land use and ocean currents.
Scenarios
  • Scenarios scientists run the model with different assumptions about future emissions, such as emissions that keep rising or fall sharply by 2050.
Outputs
  • Outputs predicted temperature, rainfall, sea level and ice cover for each region over coming decades.

Part 5 of 6Testing the model

Hindcasting
  • Hindcasting the model is started at a past date, such as 1900, to see whether it reproduces the known temperature record up to the present.
  • Models with both natural and human factors match observed warming well, while models with only natural factors do not.
Comparison
  • Comparison many independently built models giving similar predictions increases confidence.

Part 6 of 6Strengths and limitations

StrengthsLimitations
Can test what might happen without risk or costThe climate is very complex; some processes, such as clouds, are hard to represent
Can test different future scenariosThe future depends on human choices that are unknown
Improve as data and computers improveGrid boxes are large, so small-scale detail is missing
Uncertainty
  • Uncertainty predictions are given as a range, such as 1.5 to 4.5 °C of warming by 2100 depending on the scenario.
Uses
  • Uses governments plan sea defences, farming and energy supply and set emission targets.
Weather forecasts
  • Weather forecasts they use similar models but are reliable for only a few days, while climate models predict long-term averages.

Key terms

TermMeaning
IPCCThe Intergovernmental Panel on Climate Change, which advises governments.
Climate modelA computer program that represents the processes controlling climate.
ScenarioAn assumption about future emissions used to run a model.
HindcastingTesting a model by checking whether it reproduces past records.
AridVery dry with little rainfall.
ExtinctNo longer existing as a species.

Avoid these mistakes

1
Saying models are wrong because they cannot predict the weather next week.
2
Treating a model prediction as a certain fact.
3
Confusing a model with a real experiment.
4
Forgetting that the inputs strongly affect the output.

?What do you want to solve now?

Last updated: