Eduqas A-Level Geography A110QS
Coastal LandscapesLandscape
Glaciated LandscapesLandscape
Changing Places
Water and Carbon Cycles
Global Migration
Global Governance of the Oceans
Tectonic Hazards
EcosystemsContemporary theme
Economic Growth and Challenge: IndiaContemporary theme
Economic Growth and Challenge: ChinaContemporary theme
Development in an African ContextContemporary theme
Energy Challenges and DilemmasContemporary theme
Weather and ClimateContemporary theme
Geographical Skills
Water and Carbon Cycles
Changing stores: sea level change and cryospheric processes
- 2 things to know
- Component 2
Overview
Components of the cryosphere, accumulation as it applies to a glacier and glacier's mass balance.
What you need to know
Answer each one before you reveal it.
Define accumulation as it applies to a glacier.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Name the components of the cryosphere.
Model answer
The cryosphere comprises ice sheets, ice caps, valley glaciers, sea ice, seasonal snow cover and permafrost. Each component responds to warming on a different timescale.
- 2
Define accumulation as it applies to a glacier.
Model answer
Accumulation is the addition of mass to a glacier, chiefly as snowfall. Avalanches and wind-blown snow contribute in mountain settings.
- 3
What is meant by ablation?
Model answer
Ablation is the loss of mass from a glacier through melting, sublimation and calving. Wind erosion of snow adds a small further loss.
- 4
What is a glacier's mass balance?
Model answer
Mass balance is the difference between total accumulation and total ablation over a year. A positive balance makes the glacier advance and a negative balance makes it retreat.
- 5
Where on a glacier is the equilibrium line?
Model answer
The equilibrium line marks the boundary where annual accumulation exactly equals annual ablation. Accumulation dominates above the line and ablation below it.
- 6
Distinguish between eustatic and isostatic sea level change.
Model answer
Eustatic change alters the global volume of ocean water, through ice melt or thermal expansion. Isostatic change alters the height of the land relative to the sea.
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