IB ESS HL Topic 2 — Ecology Paper 1 & 2 Core idea ~11 min read

Global Biomes and Their Distribution

A biome is a group of ecosystems that share a climate and, because of that, share a look. You do not need to memorise every number in the tables below — you need to be able to say why a rainforest sits where it does and a tundra does not, and what happens to both as the climate shifts.

📘 What you need to know

What decides where a biome forms

Three abiotic factors do most of the work:

Put temperature and precipitation together and you can predict the biome. That is the single most useful idea on this page.

What decides which biome you get Temperature across, rainfall down – a simplified grid COLD TEMPERATE HOT HIGH rain MEDIUM rain LOW rain boreal forest temperate rainforest tropical rainforest tundra temperate forest savanna polar desert temperate grassland hot desert Temperature and precipitation together set the biome Real boundaries are fuzzy – soil, fire and people shift them
A deliberate simplification of the usual climate diagram. Real boundaries blend into each other, but the pattern is right: warm and wet gives rainforest, cold and dry gives polar desert.
If a question gives you a temperature and a rainfall figure and asks which biome it is, do not panic about exact boundaries. Place it roughly on this grid and justify your answer with the two numbers. The reasoning is what is marked.

Forest biomes

FeatureTropical rainforestTemperate forestBoreal forest
LocationLow latitudes, within the tropics; Amazon, Southeast Asia, Congo Basin40 to 60 degrees north and south; western Europe, northeast USA, eastern Asia50 to 60 degrees north and south; Canada, Russia, Scandinavia
Annual precipitationOver 2000 mm750 to 1500 mm, all year round300 to 900 mm, all year round
Temperature26 to 28 degrees CAbove 0 in winter, 20 to 25 in summerAround minus 30 in winter, up to 20 in summer
SeasonsNo real seasons; hot and wet all yearFour seasons of similar lengthTwo main seasons: winter and summer
Growing seasonAll year6 to 8 months2 to 3 months
SoilsFairly infertile: heavy leaching and fast nutrient uptake by plantsFairly fertile: organic matter decomposes over autumn and winterPoor and often acidic, with permafrost and a thick litter layer
BiodiversityVery high; roughly half of the world’s species. Mahogany, lianas, orchids; toucans, jaguars, frogsHigh, but below rainforest. Beech, oak, birch; deer, squirrels, bearsLower than temperate forest. Conifers; reindeer, wolves, bears

Notice the pattern running left to right: as you move away from the equator, the growing season shortens, precipitation falls and biodiversity drops. That trend is worth far more in an exam than any individual figure.

Grassland biomes

FeatureSavannaTemperate grassland
Location5 to 30 degrees north and south, bordering tropical forest; central Africa such as Tanzania and Kenya40 to 60 degrees north and south; the pampas of Argentina, steppes of Russia, plains of the USA
Annual precipitation800 to 900 mm250 to 750 mm
Temperature15 to 35 degrees CMinus 40 to 40 degrees C
SeasonsWet season and dry seasonFour seasons
Growing seasonDuring the wet season, 4 to 5 monthsDuring summer, depending on temperature
SoilsFree draining, thin humus layer, most nutrients near the surfaceFertile
BiodiversityWide range of species and the greatest diversity of hoofed animals. Grasses, baobab, acacia; zebras, elephants, giraffesLarge numbers of plants and animals. Grasses and sunflowers; bison, antelopes, rabbits

Desert and tundra biomes

FeatureHot desertTundra
Location15 to 30 degrees north and south; Sahara, Kalahari, Namib, Australia, Middle EastNorth of the Arctic Circle, and Antarctica
Annual precipitationBelow 250 mmLess than 250 mm
TemperatureDaytime can reach 50 degrees C, averaging around 25; nights below 0Below 0 degrees C for 6 to 10 months
SeasonsSummer and winterWinter and summer
Growing seasonAll yearOnly 6 to 10 weeks
SoilsInfertile and dryThin, infertile, with permafrost beneath
BiodiversityLow. Cacti and yucca; spiders, scorpions, camels, meerkatsLow. Grasses, mosses, lichens; snowy owls, arctic foxes, caribou, polar bears
Same low rainfall, opposite reason for low productivity. In a hot desert, water is the limiting factor. In the tundra, water is technically scarce too, but the real limits are low temperature and permafrost, which lock the water away and shorten the growing season to weeks.

How global warming is moving biomes

Because biome distribution follows climate, changing the climate moves the biomes. Two things happen, and exams want both named:

The direction of movement is consistent: boundaries shift poleward and upward in elevation. Warmer biomes such as tropical rainforest and savanna expand, while colder biomes such as tundra and boreal forest contract.

The consequences follow on:

WORKED EXAMPLE

A region has a mean annual temperature of 27 degrees C and annual precipitation of 2400 mm, with no dry season. Identify the biome and justify your answer.

Step 1: Read the temperature 27 degrees C is hot and consistent, so this is a low latitude Step 2: Read the precipitation 2400 mm is above 2000 mm, with no dry season Step 3: Combine them Hot plus very wet plus no seasons gives a year-round growing season Tropical rainforest Savanna would need a distinct dry season, which is absent here
WORKED EXAMPLE

Explain why tundra species are especially at risk as global temperatures rise.

Step 1: What happens to the biome Warming allows boreal forest to expand northward into tundra Step 2: Where can tundra species go? poleward – but the Arctic Ocean ends the land Step 3: State the consequence Their range is squeezed against a hard boundary, so there is no refuge Range contraction with nowhere to shift, raising extinction risk

💡 Exam tip

⚠ Common mix-up

Up next: Circulating Air and Ocean Currents — the reason deserts sit at 30 degrees and rainforests sit on the equator.

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