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
Climate Change
Icehouse and greenhouse Earth, from Cenozoic cooling to the Holocene
- 2 things to know
- Component 03
Overview
Recall questions on greenhouse and icehouse Earth, cooling over the last 100 million years and its causes, silicate weathering, the glaciation of Antarctica and ocean gateways, the Quaternary glacial cycles and their changing rhythm, the Last Glacial Maximum and its ice sheets, the Holocene, the Medieval Warm Period and the Little Ice Age.
What you need to know
Answer each one before you reveal it.
Define a greenhouse Earth state.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define a greenhouse Earth state.
Model answer
A greenhouse Earth is a prolonged interval with no permanent ice at either pole, high atmospheric CO₂ and a weak temperature gradient between equator and poles.
- 2
Define an icehouse Earth state.
Model answer
An icehouse Earth is a prolonged interval in which permanent ice exists at one or both poles, with that ice repeatedly expanding and contracting.
- 3
Is Earth currently in a greenhouse or an icehouse state, and how can you tell?
Model answer
Earth is in an icehouse state, because permanent ice sheets survive on Greenland and Antarctica even through warm interglacials.
- 4
Describe the overall direction of global climate over the past 100 million years.
Model answer
Climate has cooled substantially, from a Cretaceous world with no polar ice to the glaciated icehouse of the present.
- 5
Give two reasons for the long-term cooling of the last 100 million years.
Model answer
Rates of sea-floor spreading and volcanic outgassing of CO₂ declined, and mountain uplift such as the rise of the Himalaya increased chemical weathering, which draws CO₂ out of the atmosphere.
- 6
How does chemical weathering of silicate rock cool the planet over geological time?
Model answer
Weathering consumes atmospheric CO₂ and converts it to dissolved bicarbonate, which is carried to the sea and buried as carbonate sediment, weakening the greenhouse effect.
Other ways to work this
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