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
Exploring Oceans
Sea ice, the albedo feedback and irreversible thresholds
- 2 things to know
- Component 03
Overview
Recall questions on sea ice and icebergs, the seasonal cycle and decline of Arctic sea ice extent and volume, albedo and the positive ice-albedo feedback, Arctic amplification, an opposing negative feedback, climate tipping points in Greenland, West Antarctica and ocean circulation, and hysteresis.
What you need to know
Answer each one before you reveal it.
What is sea ice, and how does it differ from an iceberg?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is sea ice, and how does it differ from an iceberg?
Model answer
Sea ice is frozen sea water that forms and floats on the ocean surface, whereas an iceberg is a mass of freshwater ice that has broken off a glacier or ice shelf on land.
- 2
In which months does Arctic sea ice reach its minimum and maximum extent?
Model answer
It reaches its minimum in September at the end of the melt season and its maximum in March.
- 3
Describe the trend in the September extent of Arctic sea ice since satellite records began.
Model answer
It has fallen sharply, at roughly 13% per decade, with the lowest extent on record set in September 2012.
- 4
Why is the loss of Arctic ice volume even greater than the loss of extent?
Model answer
Thick multi-year ice has largely been replaced by thin first-year ice, so the ice that remains is far younger and thinner than it used to be.
- 5
Define albedo.
Model answer
Albedo is the proportion of incoming solar radiation that a surface reflects rather than absorbs.
- 6
Compare the albedo of snow-covered sea ice with that of open ocean.
Model answer
Snow-covered ice reflects a very high proportion of incoming radiation, around 0.8, while open water reflects less than 0.1 and absorbs almost everything that reaches it.
Other ways to work this
The same content, four other ways.
What is inside Levo
Six ways to work the same material.
Every question in Exploring Oceans, on a schedule.
Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.
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