Skip to content
Dabour HubLEARN · PRACTICE · EXPLORESign inStudent

BIOLOGY · Stage 9 · Chapter 12: The Carbon Cycle and Climate Change

Biology 12.5 Evaluating evidence for climate change

5 min read 6 parts Lesson 5 of 6

0%read
Lesson summary

12.5 Evaluating evidence for climate change — Alhussan International Academy — Biology (Stages 7–9) notes: Describe the types of evidence for climate change and judge their quality by considering source, method, sample and bias.IPCC view — the IPCC is convinced that rising atmosp…

  • Direct measurements
  • Proxy records
  • Biological evidence
  • Tree rings
  • Peat bog cores
  • Putting evidence together

Section 1 of 6Types of evidence

  • IPCC view
    • the IPCC is convinced that rising atmospheric carbon dioxide from human activities is causing global warming and climate change.
  • Direct measurements
    • thermometer records from weather stations over 150 years, ocean temperatures, and satellite data on ice cover and sea level.
  • Proxy records
    • ice cores, tree rings and pollen show earlier climates.
  • Biological evidence
    • plants flower earlier in spring and species move towards the poles or up mountains.
    • For example the Jersey tiger moth is spreading north in the UK as temperatures rise.

Section 2 of 6Mauna Loa Observatory

  • Site
    • it sits high on a volcano in Hawai'i, where the air is clean and there is little human activity or plant life.
  • Data
    • scientists have collected data on the composition of the air there since the 1950s.
  • Finding
    • carbon dioxide concentration in the atmosphere is rising every year.

Section 3 of 6Looking back in time

1Ice cores3 points
  • cores of ice from the Antarctic build up in layers, and the bubbles of trapped air are thousands of years old.
  • Analysing the gas gives carbon dioxide concentrations up to thousands of years ago.
  • The deepest layers are the oldest.
2Tree rings3 points
  • each ring represents a year of growth, and rings are wider in warm, wet years than in cooler, drier years.
  • Counting the rings gives the age of the tree.
  • Some trees live for hundreds or thousands of years, so tree-ring evidence is combined with ice cores.
3Peat bog cores2 points
  • the plants that formed peat grew thousands of years ago, and cores give a record up to 12 000 years back.
  • Pollen is preserved in the peat and shows which plants grew at different times.
4Putting evidence together3 points
  • scientists combine sources to reconstruct atmosphere and temperature over time, identify trends and link them to causes.
  • Combining sources increases validity.
  • The evidence is very strong that carbon dioxide is increasing and causing warming, and strong that the rise results from human activity.

Section 4 of 6Questions to ask about evidence

  • Source
    • who produced it, and is it a research organisation, a university or a company with an interest in the result?
  • Method
    • how was the data collected, were the instruments accurate and was the sample large and representative?
  • Peer review
    • was the work checked by other experts?
  • Agreement
    • do other independent studies give the same result?
  • Logic
    • do the conclusions follow from the data, or are they exaggerated?

Section 5 of 6Common errors in interpreting data

  • Cherry-picking
    • choosing a short period that fits a view, such as one cold winter, instead of the long-term trend.
  • Weather and climate
    • confusing the two.
  • Correlation without cause
    • two graphs may both rise without one causing the other.
    • The carbon dioxide and temperature link is supported by physics (infrared absorption) as well as by correlation.
  • Poor graphs
    • a truncated axis can make small changes look large.

Section 6 of 6Weighing the case

  • Temperature record
    • the global average has risen about 1.1 °C since 1880 even though individual years rise and fall.
    • The rise matches the increase in carbon dioxide from human sources and fits predictions based on the greenhouse effect.
    • Natural factors such as solar output and volcanoes cannot explain the recent warming.
  • Uncertainty
    • scientists give ranges for future warming because the outcome depends on future emissions and feedbacks such as melting ice.
  • Balanced conclusion
    • evidence from many independent sources strongly shows the Earth is warming with human activity the main cause, while details remain uncertain.
Stronger evidenceWeaker evidence
Long-term data from many placesData from one place or a few years
Peer-reviewed, repeated by othersUnpublished or from an interested group
Methods explained, with uncertainty givenClaims without methods

Last updated: