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
Earth’s Life Support Systems
Change over time in the cycles, and the monitoring that records it
- 2 things to know
- Component 01
Overview
Recall questions on daily and seasonal change in the cycles, the sawtooth carbon dioxide record, deciduous woodland and monsoon water cycles, long-term change through volcanic outgassing, the carbonate-silicate cycle, the Carboniferous and glacial periods, and monitoring by Mauna Loa, ice cores, flux towers and satellites.
What you need to know
Answer each one before you reveal it.
Why does transpiration peak in the early afternoon?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Describe the daily pattern of carbon dioxide concentration in the air above a forest.
Model answer
It falls through the day as photosynthesis exceeds respiration, and rises again overnight when photosynthesis stops and only respiration continues.
- 2
Why does transpiration peak in the early afternoon?
Model answer
Temperature and solar radiation are at their highest and the stomata are fully open, so evaporative demand and water loss from the leaves are greatest.
- 3
Why does dew form on clear, still nights?
Model answer
The ground loses heat rapidly by longwave radiation and cools the air in contact with it below its dew point, so water vapour condenses directly onto the surface.
- 4
Describe the seasonal sawtooth pattern in the record of atmospheric carbon dioxide.
Model answer
Concentrations fall through the northern spring and summer as vegetation grows, reach a minimum in September, and rise again through the northern autumn and winter.
- 5
Why does the annual cycle of atmospheric carbon dioxide follow the northern hemisphere's seasons?
Model answer
Most of the world's land and vegetation lies north of the equator, so northern growth and dormancy dominate the global pattern of uptake and release.
- 6
State the approximate size of the annual swing in atmospheric carbon dioxide at a northern monitoring site.
Model answer
About 6 to 7 ppm between the May maximum and the September minimum.
Other ways to work this
The same content, four other ways.
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