Tropical Rainforests: KS3 Geography Explained

Tropical rainforests are dense, layered forests found in a band around the Equator, between roughly 10° North and South. They receive over 2,000 mm of rainfall per year, have year-round temperatures of 25–30°C, and cover only 6% of Earth's land surface — yet contain over 50% of the world's species.

Where are tropical rainforests found?

The three major tropical rainforest regions lie close to the Equator, where sunlight is most intense and rainfall is plentiful throughout the year.

Region | Location | Key forest
South America | Amazon Basin, Brazil, Peru, Colombia | Amazon Rainforest (largest in the world, c. 5.5 million km²)
Central Africa | Congo Basin, Democratic Republic of Congo | Congo Rainforest (second largest)
South-East Asia | Malaysia, Indonesia, Papua New Guinea | Borneo, Sumatra rainforests
Central America | Mexico, Guatemala, Belize | Mesoamerican forests

The Amazon accounts for approximately half of the world's remaining tropical rainforest. The Amazon basin drains an area roughly the size of Australia, and the river itself carries about 20% of all the fresh water discharged into the world's oceans.

What is the structure of a tropical rainforest?

Tropical rainforests are organised into distinct vertical layers, each with its own characteristic species.

Emergent layer — the tallest trees (30–60 m) poke above the canopy. They must withstand strong winds, intense sunlight, and dramatic temperature variation. Large buttress roots support them at ground level. Eagles, monkeys, and large insects live here.

Canopy (20–40 m) — a near-continuous layer of interlocking tree tops that intercepts about 80% of incoming sunlight. The vast majority of rainforest biodiversity is found here: birds, insects, mammals (including sloths, monkeys, and tree frogs), bromeliads, and epiphytes (plants that grow on other plants without rooting in the soil).

Understorey (5–20 m) — a shaded layer below the canopy, receiving only 2–5% of sunlight. Plants here have evolved large, dark-green leaves to maximise photosynthesis. Jaguars, leopards, and many reptiles inhabit this layer.

Forest floor — the darkest layer, receiving less than 1% of sunlight. The floor is covered in a thin layer of dead leaf litter that decomposes rapidly in the warm, humid conditions (within weeks, compared with months or years in cooler climates). Nutrients are quickly recycled by fungi and micro-organisms. The soil beneath is often surprisingly poor and infertile — the nutrients are locked in the living biomass, not the soil.

Why are tropical rainforests so biodiverse?

Several interconnected factors explain rainforest biodiversity.

Stable climate: Tropical rainforests have existed for tens of millions of years with relatively little climate variation. This long period of stability has allowed evolution to produce an extraordinary range of specialist species occupying very narrow ecological niches.

Year-round sunlight and moisture: Plants can photosynthesise and grow throughout the year. This supports a complex food web with many levels.

Niche specialisation: Competition for resources has driven species to specialise. Different species of bee, for example, may feed exclusively from flowers at different heights. Different birds occupy different layers. This partitioning of resources allows enormous numbers of species to coexist.

Co-evolutionary relationships: Many rainforest plants and animals have co-evolved tightly: a particular orchid pollinated by only one species of bee; a fruit eaten by only one species of bird that then disperses its seeds. These relationships generate further biodiversity.

What are the causes of tropical rainforest deforestation?

Despite their importance, tropical rainforests are being destroyed at a rapid rate. Satellite data shows that approximately 15 billion trees are cut down worldwide each year, with tropical forests accounting for a large proportion of this loss.

The main causes include:

Commercial farming: Large-scale conversion of forest to agricultural land, primarily for cattle ranching in the Amazon and palm oil plantations in South-East Asia. Palm oil appears in approximately 50% of supermarket products, creating consumer links to deforestation.

Logging: Legal and illegal timber extraction for tropical hardwoods (mahogany, teak, rosewood).

Road construction: New roads — including Brazil's expanding network into the Amazon — open previously inaccessible forest to settlement and exploitation.

Mining: Extraction of gold, bauxite, iron ore, and other minerals.

Small-scale subsistence farming: Smallholder farmers clear land for food crops, a practice known as "slash and burn" (shifting cultivation), which can be sustainable at low population densities but becomes destructive at scale.

Hydroelectric dams: Large dam projects (e.g. the Belo Monte Dam in Brazil) flood vast areas of forest.

What are the SEEP consequences of deforestation?

Applying the SEEP lens helps you think systematically about consequences.

Social: Indigenous communities — the Amazon is home to over 400 distinct indigenous peoples, some of whom have had no contact with the outside world — lose their homes, cultures, and livelihoods. Local farmers may gain short-term agricultural land but face soil exhaustion within a few years as the thin, nutrient-poor soils lose fertility once forest cover is removed.

Economic: Tropical forests have an estimated economic value of trillions of dollars when ecosystem services (water regulation, carbon storage, medicines, tourism) are counted. Deforestation converts this long-term value to short-term agricultural profit. Developing countries that contain major rainforests face a real tension between economic development needs and conservation.

Environmental: Deforestation releases stored carbon dioxide (trees are enormous carbon stores), contributing to climate change. It destroys habitats, driving species extinct — scientists estimate species are being lost at 1,000 to 10,000 times the natural background extinction rate. Deforestation also disrupts the water cycle: rainforests create their own rainfall through transpiration, so large-scale clearing can reduce regional rainfall, damaging agriculture in surrounding areas.

Political: Rainforest conservation is a source of international tension. High-income countries that cleared their own forests centuries ago call on developing nations to preserve theirs — an argument that many in Brazil, Indonesia, and elsewhere regard as hypocritical. International agreements (including the Paris Agreement and the COP26 Glasgow Forest Commitment of 2021) attempt to provide financial incentives for conservation.

Frequently asked questions

Why do rainforests produce so much of the world's oxygen?

Tropical rainforests absorb large amounts of carbon dioxide and release oxygen through photosynthesis. However, the Amazon has sometimes been called "the lungs of the Earth" in a misleading way: because the plants and soil organisms of rainforests also consume oxygen through respiration, a mature rainforest is approximately carbon and oxygen neutral overall. The real importance of the Amazon and other rainforests for climate regulation is as a carbon store — they lock up enormous quantities of carbon in their biomass and soil. Destroying them releases this carbon as carbon dioxide.

What is a keystone species and can you give a rainforest example?

A keystone species is one whose influence on its ecosystem is disproportionately large relative to its abundance — remove it and the ecosystem changes radically. In the Amazon, the jaguar is a keystone predator: by controlling populations of deer, peccaries, and other herbivores, it prevents overgrazing and maintains the balance of the ecosystem. Brazil nut trees are another example: they can only be pollinated by large-bodied bees, which in turn need to nest in trees hollowed out by woodpeckers. The chain of dependency is long and fragile.

What is the "closed nutrient cycle" and why does it matter?

In a tropical rainforest, nutrients cycle very rapidly through the ecosystem: dead leaves and animal remains decompose within weeks in the warm, humid conditions, releasing minerals that are immediately taken up by plant roots. Very little accumulates in the soil. This is why rainforest soils appear thin and infertile beneath the surface — the fertility is in the living system, not the ground. When forest is cleared, the cycle is broken: without the rapid recycling, nutrients leach away in heavy rainfall, leaving exhausted, laterite soils that may become useless for farming within 3–5 years.

What can be done to protect tropical rainforests?

Approaches being tried include: creating protected areas and national parks (though enforcement is difficult); REDD+ schemes (Reducing Emissions from Deforestation and Forest Degradation), which pay developing-country governments to preserve forest; certification schemes for timber and palm oil (e.g. the Rainforest Alliance, Forest Stewardship Council) that encourage sustainable sourcing; and consumer awareness campaigns that connect purchasing decisions to rainforest destruction. No single approach is sufficient — the problem is connected to global economic inequality, consumer demand in high-income countries, and political pressures in forest nations.

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