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Climate & Natural Vegetation

Revise Climate & Natural Vegetation for Geography 0460 (O Level) — revision notes and instant AI marking.

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CIE IGCSE Geography · Unit 2.5

Climate & Natural Vegetation

Big Idea: Where you are on Earth (mainly your latitude and the pressure system sitting over you) decides your climate — and your climate decides what ecosystem grows there, how fragile that ecosystem's nutrients are, and how badly it suffers when humans clear it.

Quick Summary

  • Climate is shaped by 7 factors: latitude, altitude, continentality, ocean currents, aspect, prevailing winds, and pressure systems.
  • The equatorial climate is hot and wet all year round — no seasons — because it sits under permanent low pressure.
  • The hot desert climate is hot and dry with huge temperature swings, because it sits under permanent high pressure at 15°–30° N/S.
  • The tropical rainforest (TRF) ecosystem has the highest biodiversity on Earth, a rapid nutrient cycle, and infertile soil — because nutrients live in the plants, not the ground.
  • The hot desert ecosystem has low biodiversity, a slow nutrient cycle, and nutrients stored mostly in the soil (not the plants).
  • Plants and animals in both biomes show clear adaptations to survive extreme heat, extreme dryness, or intense competition for light.
  • Deforestation has environmental, social, and economic causes and effects — you need real case study detail (Malaysia) to score top marks.
  • Hot desert ecosystems face their own human threats — tourism, mining, agriculture, poaching (Namib Desert case study).

1. Why Climate Varies Across the World

Before you can explain any single climate, you need the toolbox of 7 reasons climate differs from place to place. Think of these as dials — turn each one and you change the temperature or rainfall of a location.

The 7 Climate Controls
FactorWhat it does
LatitudeFurther from the equator = less direct sunlight (solar radiation is spread over a bigger area and passes through more atmosphere) = colder and less sunshine.
AltitudeHigher up = colder. Air thins out and holds less heat.
ContinentalityLand heats up and cools down faster than the sea. So places deep inland (far from the coast) have hotter summers and colder winters than coastal places at the same latitude.
Ocean currentsWarm currents heat nearby land; cold currents cool it. This is why some coastal deserts (like the Namib) are cooler than you'd expect.
AspectWhich way a slope faces. In the Northern Hemisphere, south-facing slopes get more direct sun = warmer.
Prevailing windsWind blowing from a warm region brings warm air (and vice versa).
Pressure systemsLow pressure = rising air = cooling = condensation = clouds = rain. High pressure = sinking air = warming = no condensation = dry, clear skies.
The one rule to remember Rising air = wet weather. Sinking air = dry weather. Almost everything about the equatorial and hot desert climates comes back to this single idea.
Quick Analogy Think of pressure systems like a fizzy drink bottle. Shake it (heat it at the equator) and the gas rises and escapes — that's rising air cooling, condensing, and dumping rain. Somewhere else, that same air has to come back down (sink) — and sinking air is dry, like the flat air pushed back into a closed, undisturbed bottle.
Practice Question
Explain why locations further from the equator generally have lower temperatures. [2 marks]

Deforestation

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Also in the full note
  • 2. Equatorial Climate Characteristics
  • 3. Hot Desert Climate Characteristics
  • 4. Tropical Rainforest Ecosystem Characteristics
  • 5. Hot Desert Ecosystem Characteristics
  • 6. Deforestation of Tropical Rainforest — Case Study: Malaysia
  • 7. Hot Desert Ecosystem Case Study: The Namib Desert
  • What to Memorise
  • Concepts Checklist
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