OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Glaciated Landscapes
Climate, latitude and altitude as controls on glaciation
- 3 things to know
- Component 01
Overview
Recall questions on how precipitation, maritime and continental climates, latitude and altitude control glaciation, the dry interior of Antarctica, the environmental lapse rate with a worked calculation, the snow line on Kilimanjaro and in Norway, and why glaciers reach sea level in Greenland.
What you need to know
Answer each one before you reveal it.
How does the annual precipitation total affect the size of a glacier?
Roughly how much precipitation falls each year in the interior of Antarctica?
Questions from this subtopic
Each one with the model answer underneath.
- 1
How does the annual precipitation total affect the size of a glacier?
Model answer
High snowfall increases accumulation, so glaciers in wet maritime mountains can be large and fast-flowing even where temperatures are relatively mild.
- 2
Explain why a very cold polar desert may hold only small glaciers.
Model answer
Accumulation depends on snowfall, and precipitation in polar deserts is extremely low, so little snow is available to build ice despite the intense cold.
- 3
Roughly how much precipitation falls each year in the interior of Antarctica?
Model answer
Less than about 50 mm of water equivalent, making it one of the driest places on Earth.
- 4
What is the difference between a maritime and a continental glacial climate?
Model answer
Maritime climates bring heavy snowfall and milder temperatures with a high turnover of ice, while continental climates bring low snowfall and severe cold with slow-moving glaciers.
- 5
Why does the seasonal distribution of precipitation matter as much as the annual total?
Model answer
Precipitation falling as winter snow adds to accumulation, while the same amount arriving as summer rain warms the surface and speeds up ablation.
- 6
How does latitude affect the amount of solar energy a glaciated landscape receives?
Model answer
At high latitudes the sun's rays strike at a low angle and pass through more atmosphere, so the same energy is spread over a larger area and surface heating is weak.
Other ways to work this
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