IB ESS HL Topic 8 — Urban Systems Paper 1 & 2 Core idea ~11 min read

Urban Sprawl and Expansion

Cities do not only grow upwards and inwards. They creep outwards across farmland, forest and wetland, usually faster than their population grows. That gap — area rising faster than people — is what sprawl actually is, and it drives most of the environmental damage in this topic.

📚 What you need to know

Suburbanisation and sprawl

Suburbanisation describes who is moving and where. People leave the crowded centre for the edge, looking for a bigger home, a garden, quieter streets and often better schools. It is a normal part of a city maturing.

Urban sprawl describes the result when that outward movement is not planned or controlled. Housing spreads thinly, shops and offices follow, and the city’s edge dissolves into a patchwork of estates, retail parks and half-used land. The two are linked but they are not the same word: suburbanisation is a process, sprawl is a pattern.

Why it happens

Notice that improved transport appears as a cause, not a solution. Every new ring road makes land further out worth building on, so the city spreads a bit more and the road fills up again. Planners call this induced demand, and it is a genuinely useful phrase in an evaluation answer.

The measurement that defines sprawl

If a city’s population doubles and its built-up area doubles, that is growth. If the population doubles and the area grows six-fold, that is sprawl. The test is what happens to density.

Population density density = total population ÷ built-up area (km2)
One city, forty years of spreading out Square areas are drawn to scale. The people did not multiply as fast as the land. 1980 2000 2020Built-up area and density 1980: 120 km2, 1.0m people 8 300 people per km2 2000: 300 km2, 1.8m people 6 000 people per km2 2020: 700 km2, 2.6m people 3 700 people per km2Population up 2.6 times Built-up area up 5.8 timesFalling density is the fingerprint of sprawl. Every extra square kilometre needs its own roads, pipes, cables and bus routes.
If you are given city data in an exam, calculate density for both years. A fall proves sprawl in one line.
WORKED EXAMPLE

City A has 900 000 people in a built-up area of 300 km2. City B has the same population spread over 1 200 km2. Calculate both densities and explain what the difference means for the environment.

Step 1: City A 900 000 ÷ 300 = 3 000 people per km2 Step 2: City B 900 000 ÷ 1 200 = 750 people per km2 City B is four times less dense Step 3: what it means City B has taken 900 km2 more land from farming and habitat for the same number of people, needs four times the length of roads and pipes per person, and is too spread out for buses or trains to work well, so almost everyone drives. Always convert a density difference into consequences. The number on its own is only half the mark.

Environmental impacts

What sprawl does to the environment Six consequences, and several of them feed each other. URBAN SPRAWL low density, spreading Farmland built over food grown further away Habitats cleared biodiversity falls More hard surfaces runoff and flash flooding Longer commutes more traffic emissions Heat island spreads more cooling needed Infrastructure cost roads and pipes stretchedLink them up: hard surfaces cause runoff and store heat. Examiners reward chains of cause and effect, not lists of separate impacts.
Chains beat lists. Sprawl removes trees, which removes shade and evaporation, which raises temperatures, which raises air-conditioning demand, which raises emissions.

Land

Water

Air and climate

Biodiversity

The impact that lasts longest. Buildings can be retrofitted and power grids can be decarbonised, but a city’s shape is close to permanent. A low-density layout commits its residents to driving for a century. That is why sprawl is treated as a serious environmental problem rather than a planning preference.
WORKED EXAMPLE

Explain how urban sprawl can increase the risk of flooding in and around a city.

Step 1: what sprawl replaces Soil and vegetation are covered with impermeable surfaces such as roofs, roads and car parks. Step 2: what that does to rainfall Water can no longer infiltrate, so instead of soaking in slowly it becomes surface runoff and reaches drains and rivers quickly. Step 3: the effect on the river Lag time falls and peak discharge rises, so the river rises faster and higher after a storm. Step 4: the extra factor Wetlands that used to store floodwater have often been drained and built on, removing the natural buffer. Faster runoff plus lost storage equals higher flood risk Using lag time and peak discharge shows you can connect this topic to hydrology, which is exactly what “explain” wants.

💡 Exam tip

⚠ Common mix-ups

Up next: Planning Sustainable Cities — the tools planners use to stop all of this, and how to judge whether they work.

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