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
Weather and Climate
The ITCZ and seasonal migration
- 3 things to know
- Component 3 Section B
Overview
Heat equator, seasonal migration of the ITCZ and sahel and how is its rainfall linked to the ITCZ.
What you need to know
Answer each one before you reveal it.
Why does heavy rainfall occur along the ITCZ?
What is the heat equator?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What does ITCZ stand for and what is it?
Model answer
ITCZ stands for the Inter-Tropical Convergence Zone. The zone is the belt of low pressure where the trade winds of the two hemispheres converge.
- 2
Why does heavy rainfall occur along the ITCZ?
Model answer
The converging trade winds force air to rise, and that air cools to its dew point. Towering cumulonimbus cloud forms and produces intense convectional rain.
- 3
What is the heat equator?
Model answer
The heat equator is the line joining the places with the highest mean temperature at a given time. The line broadly follows the overhead sun rather than the geographic equator.
- 4
Describe the seasonal migration of the ITCZ.
Model answer
The ITCZ moves north of the equator during the northern summer and south during the southern summer. The zone follows the overhead sun with a lag of a few weeks.
- 5
Why does the ITCZ lag behind the overhead sun?
Model answer
Land and sea take time to warm after the sun reaches its highest position. The zone of maximum heating therefore arrives some weeks later.
- 6
Over which surface does the ITCZ migrate furthest, and why?
Model answer
The ITCZ migrates furthest over continents, reaching about 25° over Asia and Africa. Land heats far faster than the ocean, which draws the zone further poleward.
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