CCEA A-Level Geography 3910
Processes That Shape Fluvial Environments
Human Interaction in Fluvial Environments
Global Biomes
Small-Scale Ecosystems
The Processes That Shape Our Weather and Climate
Weather in the British Isles
Global Weather Issues
Population Data
Population Change
Population and Resources
Settlement Change and the Rural-Urban Fringe
Planning in Rural Environments
Urban Challenges in MEDC and LEDC Cities
Measuring Development
Reducing the Development Gap
Emerging Markets
Data Collection
Data Processing
Fieldwork Skills and Techniques
Planning and Recording an Investigation
Plate Tectonics: Theory, Margins and LandformsTectonics
Volcanic Activity and Its ManagementTectonics
Seismic Activity and Its ManagementTectonics
Locations and Climates of the Major Tropical BiomesTropical
Management and Sustainability in Arid and Semi-Arid Tropical EcosystemsTropical
Management and Sustainability in the Tropical Forest EnvironmentTropical
Coastal Processes and FeaturesCoastal
Regional Coastlines: Submergence, Emergence and Rising Sea LevelCoastal
Coastal Management and SustainabilityCoastal
Natural Climate Change: Evidence, Causes and the Arrival of the HoloceneClimate
Lowland Glacial LandscapesClimate
Current Global Climate Change: Human Causes and ImpactsClimate
Managing Global Climate ChangeClimate
Cultural Groups, Social Inequality and LandscapeCultural
MigrationCultural
The Geographies of CyberspaceCultural
Sustainable Development in SettlementsPlanning
Urban Design, Planning and Management for SustainabilityPlanning
Traffic and TransportPlanning
Defining EthnicityEthnic
Processes That Create and Maintain Ethnic DiversityEthnic
Ethnic ConflictEthnic
The Changing Nature of TourismTourism
Challenges and Management of Mass TourismTourism
Ecotourism: Opportunities, Challenges and RegulationTourism
Decision Making in Geography
Locations and Climates of the Major Tropical Biomes
Tropical grassland: distribution, climate and biomass
- 3 things to know
- Unit A2 1
Overview
Climate of tropical grassland and vegetation of tropical grassland.
What you need to know
Answer each one before you reveal it.
When in the year is a tropical grassland at its hottest, and why is it not the middle of the wet season?
Why is the rainfall of tropical grassland unreliable as well as seasonal?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Where is tropical grassland found?
Model answer
In belts on the poleward margins of the tropical forest, roughly between 5 and 20 degrees north and south, forming a transition towards the deserts. The largest expanses are in Africa, north and south of the Congo forest, from the Sahel through East Africa to the veld and miombo of the south. There are also substantial areas in the llanos and campo cerrado of South America, in northern Australia and in parts of India and South East Asia.
- 2
Describe the climate of tropical grassland.
Model answer
Temperatures are high all year, generally 25-32 degrees Celsius, with a modest annual range of about 5-8 degrees. The distinguishing feature is rainfall: total annual rainfall is moderate, commonly 500-1500 mm, but it is strongly concentrated into a single wet season of about four to six months, leaving a long, reliable dry season in which some months receive virtually no rain at all. Rainfall totals fall and the dry season lengthens as you move away from the equator.
- 3
When in the year is a tropical grassland at its hottest, and why is it not the middle of the wet season?
Model answer
The temperature peak comes at the end of the dry season, just before the rains break. Through the dry season skies are cloudless, so insolation reaching the ground is at a maximum and there is little moisture to be evaporated, meaning almost all the energy goes into heating the ground and the air. Once the rains arrive, cloud cover reflects and absorbs incoming radiation and much of the remaining energy is used as latent heat in evaporation, so temperatures fall slightly during the wettest months.
- 4
Why is the rainfall of tropical grassland unreliable as well as seasonal?
Model answer
Because the wet season depends on how far the ITCZ migrates in a given year, and that varies. If the ITCZ fails to reach as far poleward as usual, or arrives late or withdraws early, the wet season is shortened and totals fall well below average. The margin closest to the desert is the most vulnerable, since it lies at the very limit of the ITCZ's reach, and this variability is why drought is a recurrent hazard on the desert edge of the grassland rather than a rare event.
- 5
Describe the vegetation of tropical grassland.
Model answer
A continuous ground layer of tall tussock grasses, often 1-3 m high, with scattered, widely spaced trees and shrubs above it. The proportion of trees changes with rainfall: near the forest margin there is enough woodland cover to be described as savanna woodland, while towards the desert the trees thin to isolated individuals and then to open thorn scrub and grass alone. Growth is strikingly seasonal, with grasses green and lush in the wet season and straw-coloured, dormant and dead above ground through the dry.
- 6
What adaptations allow savanna trees and grasses to survive the dry season?
Model answer
Many trees are deciduous, shedding their leaves at the onset of the dry season to cut transpiration losses. Leaves are often small, waxy or reduced to thorns for the same reason. Root systems are extensive: some species send down very long tap roots to reach deep groundwater, others spread wide, shallow root mats to capture the first rain. Trunks may be thick and water-storing, as in the baobab, and bark is often thick and corky to resist fire. Grasses survive by dying back above ground and holding their growing points at or below the surface, so they can resprout from roots and rhizomes within days of the first rains. Seeds of annuals lie dormant through the drought.
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