Carbon cycles: stocks, fluxes and changing feedbacks

Calculate carbon balances, explain fast and slow pathways, and evaluate coupled climate feedbacks.

A-level study: check your qualification and chosen options below.

Dense forest meets secondary growth and cultivated land.

Distinguish a carbon stock from a flux

A stock is carbon held in a reservoir; a flux transfers carbon per unit time. Photosynthesis, respiration and decomposition exchange carbon among atmosphere, vegetation and soils.

Geological storage and weathering operate over longer timescales. Specify the boundary and period before deciding whether a system is a net sink or source.

Worked example

A fictional forest absorbs 12 tonnes C/year and releases 9 tonnes C/year across the stated boundary. Its net uptake is 3 tonnes C/year; its total stored carbon remains a different quantity.

Common mistake: A large forest stock does not demonstrate a large current net sink.

Percentage change · Source evaluation

Explain land-use change through the system

Clearance can transfer biomass carbon through burning or decay and reduce future uptake. Soil responses depend on land use, disturbance and moisture.

Restoration can rebuild stores over time, but survival, fire, management and displaced land uses affect permanence. A planted area is not a measured carbon removal.

Worked example

A fictional stock falls from 100 to 70 tonnes C/ha on 200 ha: loss is 6,000 tonnes C. The data do not show how much entered the atmosphere, products or another store.

Common mistake: Stock loss and atmospheric emissions need matching boundaries.

Percentage change · Source evaluation

Reason through a climate–carbon feedback

Warming can influence decomposition, fire and frozen-ground carbon, which can change atmospheric greenhouse gases and further affect climate. These pathways have different speeds and uncertainties.

Additional carbon dioxide can also influence uptake, constrained by nutrients, water and disturbance. Evaluate competing processes instead of treating every feedback as the same response.

Worked example

A fictional warming perturbation adds 2 units of release and 1 unit of additional uptake per year. The net +1 atmospheric transfer amplifies the original change within this simplified boundary.

Common mistake: Positive feedback means amplification, not a beneficial outcome.

Source evaluation · Scatter plots

Try a different resource

Time series and missing observations

The same river level threshold is used throughout. One annual record is missing. Line segments only connect consecutive observed years; no zero or interpolated observation has been inserted.

Scroll the diagram sideways to see the full resource.

Fictional annual river recordExact observations: 2018: 29 days; 2019: 36 days; 2020: 25 days; 2021: 38 days; 2022: missing days; 2023: 33 days; 2024: 26 days; 2025: 31 days. The line is deliberately broken at the missing year.01020304050607020182019202020212022Missing202320242025Annual days above the stated river level
YearDays above the fixed level
201829
201936
202025
202138
2022Missing
202333
202426
202531
Fictional annual river record. Original fictional resource; not an official map or real dataset.
Resource description

Exact observations: 2018: 29 days; 2019: 36 days; 2020: 25 days; 2021: 38 days; 2022: missing days; 2023: 33 days; 2024: 26 days; 2025: 31 days. The line is deliberately broken at the missing year.

1. What is the mean of the observed annual counts, to two decimal places?

2. What is the signed change between the first and last observed years?

3. What does the missing year establish?

Choose an answer

The maps and data are fictional. These exercises do not count as required fieldwork.

Write an explanation

Check your answer
  • Use stocks and fluxes with correct units.
  • Connect fast and slow pathways.
  • Analyse an amplifying or damping feedback.
  • Evaluate permanence, scale and uncertainty of management.

Practise and review a written answer

Case studies

Amazon forest conversion · Forest and plantations in Kalimantan · Permafrost thaw and Denali’s park road

These pages provide selected evidence. Check the whole case requirement with your teacher.

Read further

Forest conversion and distant demand · Ecosystem interdependence · Power, energy and reliable supply

Course links

AQA A-level Geography · Pearson Edexcel A-level Geography · OCR A-level Geography · Eduqas A-level Geography

Next topics

Climate change: evidence, causes and responses · Water cycles: budgets, residence time and feedback

Selected teaching sequence with fictional worked data. The linked case records supply bounded evidence; they do not satisfy every course case requirement.

Worked numerical examples are fictional unless explicitly attributed. These lessons cover selected parts of the topic; check your course requirements for the rest.