OCR A-Level Geography Physical systems (01), June 2025: Question 4

33 marks · Hard difficulty · Extended Response

Assess atmospheric carbon dioxide data, examine the cryosphere's role in linking the water and carbon cycles, and evaluate whether improved forestry techniques protect the global water cycle more effectively than drainage basin planning.

Practise this question

Question

Question 4 from Section B on Earth's Life Support Systems. Part (a)(i) asks to identify three limitations of Fig. 4 showing atmospheric carbon dioxide from 1960 to 2021 for 3 marks. Part (a)(ii) asks to suggest why it is important to identify and record changes to the global carbon cycle for 4 marks. Part (b) asks to examine the significance of the role of the cryosphere in linking the water and carbon cycles for 10 marks. Part (c)* asks 'Improving forestry techniques protects the global water cycle more effectively than drainage basin planning.' How far do you agree with this statement? for 16 marks.
Question text

Section B

Earth’s Life Support Systems

(a) Study Fig. 4, which shows atmospheric carbon dioxide, 1960–2021.

(i) Identify three limitations of this graph. [3]

(ii) Suggest why it is important to identify and record changes to the global carbon cycle. [4]

(b) Examine the significance of the role of the cryosphere (ice) in linking the water and carbon

cycles. [10]

(c)* ‘Improving forestry techniques protects the global water cycle more effectively than drainage

basin planning.’

How far do you agree with this statement? [16]

Mark scheme

Show the mark scheme Mark scheme for Question 4. Part (a)(i) awards 3 marks for identifying graphical limitations such as lack of source context, narrow timeline, lack of key, scale resolution, and lack of diurnal/monthly variations. Part (a)(ii) awards 4 marks across AO2 for explaining the importance of monitoring the carbon cycle to mitigate climate damage, track trends, and inform policy. Part (b) uses a 3-level mark scheme for 10 marks assessing knowledge of cryospheric carbon and water interactions, melting impacts, and feedbacks. Part (c)* uses levels-based criteria across AO1 and AO2 for 16 marks evaluating forestry techniques versus drainage basin planning in protecting the water cycle.

Question Answer Mark Guidance

4 (a) (i) Study Fig. 4 which shows atmospheric carbon 3 AO3 – 1 marks

dioxide, 1960-2021. AO3 x3 3 x 1 (✓) for identification of limitations of this line

Identify THREE limitations of this graph. graph.

• Lack of information on potential bias – who has Allow any appropriate limitation

recorded the information and why ( )

• Timeline relatively short for global atmospheric

carbon change ( )

• No key to indicate difference between the two

types of line on the graph ( )

• The two lines on the graph are the same colour

so hard to distinguish them ( )

• The graph does not indicate where the data was

collected / located ( )

• Intervals on the scale are too broad so you can’t

read precise data ( )

• Data only shows to 2021 so is outdated ( )

• Difficult to read accurate data measurements

( )

• Does not show temporal variations (diurnal /

monthly) ( )

4 (a) (ii) Suggest why it is important to identify and record 4 AO2 – 4 marks

changes to the global carbon cycle. AO2 x4 4 x 1 (✓) for appropriate reasons, or

• The potential damage of increasing atmospheric 3 x 1 (✓) for appropriate reasons and 1 x 1 (DEV) for

carbon is widespread ( ) so monitoring is three reasons with one developed or

essential, enabling effective management to be

implemented e.g. carbon capture (DEV) 2 x 1 (✓) and 2 x 1 (DEV) for two appropriate reasons

• Monitoring allows us to identify trends / patterns and development or

( ) allowing appropriate mitigation strategies /

management to be implemented (DEV) 1 x 1 (✓) and 3 x 1 (DEV) for one appropriate reason

• Records of change allow GIS mapping showing with extended development of why it is important to

anomalies and trends effectively ( ) illustrating identify and record changes to the global carbon cycle.

need for different levels of management or

mitigation across the world (DEV)

• Carbon is vital for life so it’s important to monitor

changes ( ) and the impact of anthropogenic

emissions through burning fossil fuels (DEV)

which allows evidence for mitigation strategies

(DEV)

• We need to monitor the carbon cycle to identify

thresholds to see if we are reaching a tipping

point ( ) so we can understand what may be

causing these changes (DEV) and therefore

implement appropriate mitigation (DEV). We can

also evaluate the effectiveness of this mitigation

through continuous monitoring (DEV)

4 (b) Examine the significance of the role of the 10 Indicative content

cryosphere (ice) in linking the water and carbon AO1 6 AO1 – 6 marks

cycles. AO2 4 Knowledge and understanding of the role of the

cryosphere (ice) in linking the water and carbon cycles

Level 3 (7-10 marks) could potentially include:

Demonstrates thorough knowledge and understanding • Cryosphere is a store of both water and carbon

of the role of the cryosphere (ice) in linking the water • Rising temperature results in melting of the

and carbon cycles (AO1). cryosphere. This leads to the release of carbon

to the atmosphere, further increasing

Demonstrates thorough application of knowledge and temperatures so more ice melts and pools of

understanding to provide a detailed evaluation that water can gather on the surface due to limited

offers generally secure judgements with some links infiltration

between rational conclusions and evidence regarding • Melting of the cryosphere results in some plant

the significance of the role of cryosphere (ice) in linking growth, which requires water for photosynthesis.

the water and carbon cycles (AO2). As plants grow, they take in more CO2 from the

atmosphere

• Permafrost melting exposes organic material to

oxidation and decomposition which releases

This will be shown by including well-developed ideas CO2 and CH4. This causes a rise in

about the significance of the role of cryosphere (ice) in temperatures and further melting which can

linking the water and carbon cycles. increase surface run off

• CO2 levels in the atmosphere determine the

Level 2 (4-6 marks) intensity of the greenhouse effect and the

Demonstrates reasonable knowledge and melting of the cryosphere. Due to the

understanding of the role of cryosphere (ice) in linking impermeability of the permafrost, water can pool

the water and carbon cycles (AO1). on the surface leading to limited evaporation

taking place

Demonstrates reasonable application of knowledge

and understanding to provide a sound evaluation that AO2 – 4 marks

offers generalised judgements and conclusions, with Apply knowledge and understanding to provide a

limited use of evidence regarding the significance of the detailed evaluation of the significance of the role of the

role of cryosphere (ice) in linking the water and carbon cryosphere (ice) in linking the water and carbon cycles

cycles (AO2). could potentially include:

• Significance could be in terms of temporal or

This will be shown by including developed ideas about spatial scales e.g. seasonal change, short term

the significance of the role of cryosphere (ice) in linking cycling is significant to continual functioning of

the water and carbon cycles. the cycles

• Disturbance of the cycles in equilibrium and

Level 1 (1–3 marks) subsequent positive or negative feedback e.g.

Demonstrates basic knowledge and understanding of reduced precipitation, means less water to be

the role of cryosphere (ice) in linking the water and accumulated in glaciers

carbon cycles (AO1).

• Decomposition very slow reducing carbon

content in the soil (only 0.01%)

Demonstrates basic application of knowledge and

understanding to provide an evaluation about the • Consideration of how significance varies with

significance of the role of cryosphere (ice) in linking the temperature e.g. seasonal variations

water and carbon cycles (AO2). • The extent to which the role of cryosphere links

the cycles is of limited significance when

This will be shown by including some ideas about the compared to other links e.g. vegetation and

significance of the role of cryosphere (ice) in linking the animals combined contain 2000 billion tonnes of

water and carbon cycles. carbon, whereas oceans contain 38,000 giga

tonnes of carbon – however all required to keep

the cycles functioning

0 marks

No response or no response worthy of credit.

4 (c*) ‘Improving forestry techniques protects the global 16 Indicative content

water cycle more effectively than drainage basin AO1 8 AO1 – 8 marks

planning’. How far do you agree with the AO2 8 Knowledge and understanding of forestry techniques,

statement? drainage basin planning and global water cycle could

potentially include:

AO1 • Forestry techniques e.g. afforestation, protection

Level 3 (6–8 marks) schemes e.g. REDD / FCPF / ARPA

Demonstrates thorough knowledge and understanding • Drainage basin planning e.g. scale appropriate

of forestry techniques, drainage basin planning and for holistic management between users, flow

global water cycle. targets, surface water storage

• Global water cycle

The answer should include accurate place-specific • Processes e.g. infiltration, percolation,

detail. precipitation, transpiration, condensation,

evaporation

Level 2 (3–5 marks) • Stores e.g. channel, atmosphere, vegetation,

Demonstrates reasonable knowledge and surface, soil moisture, groundwater

understanding of forestry techniques, drainage basin

planning and global water cycle. AO2 – 8 marks

Apply knowledge and understanding to analyse and

The answer should include some place-specific detail evaluate whether improved forestry techniques protects

which is partially accurate. the global water cycle more effectively than drainage

basin planning could potentially include:

Level 1 (1–2 marks) • Expect range of evaluation – candidates may

Demonstrates basic knowledge and understanding of compare over temporal or spatial scales

forestry techniques, drainage basin planning and global • Role in protecting global water cycle can vary

water cycle.

depending on use of case study

There is an attempt to include place-specific detail but • Drainage basin planning allows for targets to be

it is inaccurate. set across a variety of flows e.g. reducing run-off

which could include afforestation to do that,

however drainage basin planning includes a

0 marks more holistic management of the drainage basin

No response or no response worthy of credit. which is more effective as it addresses the

system as a whole e.g. including water quality

and abstraction rates within the basin

AO2 • Afforestation is more effective for LIDCs and

Level 3 (6-8 marks) EDCs e.g. Brazil where afforestation has

Demonstrates thorough application of knowledge and stabilised the regional water cycle, supported

understanding to provide a clear and developed indigenous forest communities and promoted

analysis that shows accuracy. Includes a detailed ecotourism encouraging small scale local

evaluation that offers generally secure judgements, with communities and bringing sustainable economic

some link between rational conclusions and evidence options. Promoting social and economic

regarding whether improved forestry techniques sustainability makes it more likely that this action

protects the global water cycle more effectively than will continue, which influences the global water

drainage basin planning. cycle more

• Afforestation offsets 430 million tonnes of

Level 2 (3-5 marks) carbon per annum in Brazil alone having a

Demonstrate reasonable application of knowledge and significant impact on the global water cycle as

understanding to provide a sound analysis that shows this reduces global warming

some accuracy. Includes a sound evaluation about • The effectiveness of improving forest techniques

whether improved forestry techniques protects the can vary according to the political leadership at

global water cycle more effectively than drainage basin the time eg Bolsonaro v Lula da Silva

planning. Judgements and conclusions are generalised,

with limited use of evidence. • Drainage basin planning is more effective at a

global scale as it includes a wider variety of

management that can target a variety of stores

Level 1 (1-2 marks)

rather than just vegetation e.g. reducing artificial

Application of knowledge and understanding is basic.

drainage, or increasing flood storage areas,

Analysis is simple with limited accuracy. Evaluation is

restricting floodplain development

un-supported and offers simple conclusions with regard

to whether improved forestry techniques protects the

global water cycle more effectively than drainage basin Highest level likely to refer to dynamic equilibrium /

planning. spatial variations / temporal variations

0 marks

No response or no response worthy of credit.

Quality of extended response

Level 3

There is a well-developed line of reasoning which is

clear and logically structured. The information

presented is relevant and substantiated.

Level 2

There is a line of reasoning presented with some

structure. The information presented is in the most-part

relevant and supported by some evidence.

Level 1

The information is basic and communicated in an

unstructured way. The information is supported by

limited evidence and the relationship to the evidence

may not be clear.

How to answer it

Earth's Life Support Systems: Carbon, Cryosphere & Water Management

📌 WHAT THIS QUESTION TESTS

Core Specification Themes: Water and Carbon Cycles (Topic 1.2)

  • AO3 (Fieldwork & Skills): Critical evaluation of quantitative data presentations, spotting graphical bias, scale deficiencies, and presentation limitations.
  • AO1 (Knowledge & Understanding): The role of the cryosphere as a store and transfer mechanism; systems feedback loops; forestry management techniques (REDD, afforestation); drainage basin planning schemes (abstraction caps, runoff control).
  • AO2 (Application & Evaluation): Analysing the imperative for real-time carbon cycle monitoring; synthesising the interconnectedness of water and carbon via freeze-thaw/albedo/permafrost dynamics; evaluating spatial, temporal, and political scales in water cycle protection.
AO3 Question 4 (a) (i) • [3 Marks]

Limitations of Climate Graphs

Identify three limitations of Fig. 4 (Atmospheric CO₂ 1960–2021).

✅ Acceptable Graph Limitations (Choose 3)

  • Scale intervals: Scale divisions are too broad/coarse to extract precise annual or monthly numerical values.
  • Temporal resolution: Does not reveal intra-annual fluctuations (seasonal cycles driven by Northern Hemisphere vegetation growth/decay) or diurnal variations.
  • Spatial ambiguity: Fails to declare sampling location/provenance (e.g., Mauna Loa baseline vs global mean).
  • Graphic design: Traces share identical or poorly distinguished colours without a disambiguating key.
  • Timeline context: 61-year window (1960–2021) is geologically tiny; excludes pre-industrial baseline (~280 ppm).
  • Provenance & bias: Lack of publisher/institutional metadata (who recorded it and why).

🧠 Exam Technique

Rule of 3: Give 3 clearly distinct limitations. Do not waste time explaining each one extensively—this is an "Identify" command requiring concise, direct observations.

Mark Scheme Breakdown: 3 × 1 mark (✓) for identifying each valid limitation directly from the resource.

❌ Common Errors to Avoid

  • Stating vague criticisms like "it is hard to read" without explaining why (e.g. lack of fine gridlines or indistinct legends).
  • Critiquing the scientific data itself rather than the graphical presentation.
AO2 Question 4 (a) (ii) • [4 Marks]

Importance of Monitoring the Global Carbon Cycle

Suggest why it is important to identify and record changes to the global carbon cycle.

✅ Core Reasons + Developed Chains (DEV)

  • Mitigation Target Planning: Atmospheric CO₂ accumulation drives global warming (✓); tracking rates informs carbon capture strategies, net-zero legislation, and international emission quotas (✓ DEV).
  • Identifying Tipping Points: Highlights critical thresholds where stores shift from net sinks to net sources (e.g., Amazon dieback or permafrost thaw) (✓), allowing early intervention (✓ DEV).
  • Policy Effectiveness: Continuous time-series verify whether mitigation policies (renewable transitions, cap-and-trade) are actually working (✓ DEV).
  • Spatial Anomaly Tracking: GIS mapping of emissions flags regional disparities and industrial hotspots needing targeted remediation (✓ DEV).

🧠 Exam Technique: Securing 4 Marks

The mark scheme allows several combinations:

  • 2 points with 2 developments (2 × 1 mark + 2 × 1 DEV) ← Best approach!
  • 3 points with 1 development (3 × 1 mark + 1 DEV)
  • 1 point with extended development (1 mark + 3 DEV)

Tip: Use connective phrases like "consequently this allows...", "which provides empirical evidence for..." to guarantee DEV marks.

❌ Common Errors

  • Giving descriptive facts about carbon stores without explaining why recording/measuring them matters.
  • Forgetting to link carbon increases to applied management solutions or climate policy.
AO1 AO2 Question 4 (b) • [10 Marks]

The Cryosphere: Linking the Water and Carbon Cycles

Examine the significance of the role of the cryosphere (ice) in linking the water and carbon cycles.

💡 AO1: Key Cycle Interconnections

  • The Cryosphere Store: The cryosphere stores ~1.7% of Earth's total water (68.7% of freshwater) and locks up ~1,600 Gt of organic carbon in permafrost soils.
  • Permafrost Thaw Mechanism: Warmer atmospheric conditions (carbon-driven) melt cryospheric ice (water cycle transfer). Thawing active layers expose ancient organic matter to anaerobic/aerobic microbial breakdown, releasing CO₂ and CH₄.
  • Surface Hydrology & Vegetation: Melting ice creates thermokarst pools and saturated soils. Impermeable permafrost restricts infiltration, driving surface runoff while supplying water for seasonal tundra plant growth (photosynthetic carbon uptake).

🧠 AO2: Evaluative Arguments (Significance)

  • Positive Feedback Loop: Increased atmospheric carbon → higher temperatures → cryosphere melt → amplified greenhouse emissions (CH₄/CO₂) → further warming. Highly significant feedback!
  • Temporal Scales: Highly significant seasonally (active layer thaw in Arctic summer) and on geological timescales (glacial/interglacial transitions), but cycling is slow and locked during freezing winter periods.
  • Relative Magnitude: Compared to ocean carbon stores (~38,000 Gt) or oceanic water stores (97%), the cryosphere's direct carbon content is modest (~1,600 Gt). However, its sensitivity makes it an disproportionately powerful driver of global system shifts.

✅ How to Reach Level 3 (7–10 Marks)

  • Explicitly link both cycles together in the same breath (e.g., thermal energy → ice melt [water] → microbial decomposition [carbon] → greenhouse effect → atmospheric moisture holding capacity).
  • Reach an authoritative judgement on how significant the cryosphere is across differing temporal and spatial scales.

❌ Common Misconceptions

  • Treating water and carbon in isolation (writing one paragraph on glaciers melting, then a separate paragraph on CO₂ levels, without joining them).
  • Forgetting that ice melt provides the essential liquid water input needed for biological uptake and vegetation growth in polar biomes.
AO1 AO2 Question 4 (c)* • [16 Marks]

Essay: Forestry Techniques vs Drainage Basin Planning

‘Improving forestry techniques protects the global water cycle more effectively than drainage basin planning.’ How far do you agree with this statement?

💡 Forestry Techniques

  • Practices: Afforestation, selective logging, REDD+ initiatives, ARPA (Amazon Region Protected Areas).
  • Hydrological Role: Canopy interception reduces raindrop impact and soil compaction; promotes infiltration and soil moisture storage; sustains high evapotranspiration rates maintaining regional precipitation cycles (e.g., Amazonian "flying rivers").
  • Atmospheric Regulation: Offsetting carbon emissions mitigates global warming, reducing extreme hydrological disruptions (floods/droughts).

💡 Drainage Basin Planning

  • Practices: Abstraction licensing/caps, wetland restoration, artificial recharge of aquifers, flood attenuation basins, agricultural terracing, river buffer zones.
  • Hydrological Role: Directly controls channel flow, baseflow, and subsurface aquifers; manages surface runoff rates; protects groundwater tables against saltwater intrusion and over-abstraction.
  • System Scope: Holistically manages the complete drainage basin balance ( P = Q + E ± ΔS ).

🧠 AO2: Structuring a Level 3 Synoptic Evaluation (13–16 Marks)

To access Level 3, candidates must contrast both strategies explicitly across different scales and provide a supported judgement:

  • Spatial Scale: Drainage basin planning operates effectively at local and regional catchment levels (e.g., River Thames Catchment or Colorado River Basin). Forestry operates across macro-biomes (e.g., Amazonia), feeding macro-scale atmospheric moisture cycles.
  • Directness of Protection: Drainage basin planning directly manages all water cycle transfers and stores (groundwater, rivers, soil). Forestry primarily manipulates evapotranspiration and interception.
  • Socio-Political Feasibility: Forestry effectiveness depends heavily on national political will (e.g., changes between Bolsonaro and Lula administrations in Brazil). Drainage basin frameworks are often backed by strict domestic legal statutes (e.g., UK Environment Agency abstraction limits).
  • Dynamic Equilibrium: Drainage basin planning incorporates engineering, land-use zoning, and afforestation simultaneously—making forestry one component within drainage basin management rather than a standalone rival.

❌ Critical Pitfalls in 16-Mark Essays

  • Drifting into Carbon: Focusing predominantly on forestry's ability to store carbon rather than keeping the primary focus on the water cycle. Always bring carbon points back to their hydrological impacts.
  • Unbalanced Comparison: Writing 80% on Amazon deforestation and only a brief concluding sentence on drainage basin planning.
  • Lacking Case Studies: Neglecting specific, named examples of basin plans or forestry initiatives.
Examiner Insight for Level 3: The highest-scoring candidates argued that the statement is an oversimplification: improved forestry is vital for macro-scale precipitation and atmospheric moisture, but drainage basin planning is inherently more comprehensive because it manages surface, soil, aquifer, and channel stores collectively.

Topics

Topic 1.2 Earth’s Life Support Systems · 3.b. The pathways and processes which control the cycling of water and carbon vary over time. · 4.a. The two cycles are linked and interdependent. · 4.b. The global implications of water and carbon management.

Question and mark scheme from the OCR A-Level Geography examination, Physical systems (01), June 2025. QuestionVault is an independent revision resource; questions remain the copyright of the awarding body.