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Global Population Distribution

Geography
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Global Population Distribution

Geography
01 May 2026

Spatial Distribution of the Present-Day Global Population

The world’s population of over 8 billion people is unevenly distributed across the planet’s land surface. Understanding this distribution — where people live and why — is foundational to Unit 4 Population Geography.

Key Patterns of Population Distribution

Ecumene vs Non-ecumene
- The ecumene refers to permanently inhabited areas of the world
- The non-ecumene refers to areas not permanently inhabited: extreme deserts, high mountains, polar ice
- Approximately 90% of the world’s population lives on just 10% of its land area

Hemispheric distribution
- ~90% of the world’s population lives in the Northern Hemisphere
- ~80% lives between the Tropics and 60°N latitude
- Over 50% lives in Asia

Continental distribution (approximate 2024)

Region Population (millions) % of World
Asia 4,700 ~58%
Africa 1,450 ~18%
Europe 750 ~9%
Latin America & Caribbean 660 ~8%
North America 380 ~5%
Oceania 45 ~0.5%

Highest population densities:
- Indo-Gangetic Plain (India, Bangladesh, Pakistan) — >1,000 people/km² in some districts
- Eastern China (Yellow River, Yangtze deltas)
- Java, Indonesia — one of the most densely populated large islands on Earth (~150 million people)
- Rhine Valley and North European Plain
- Nile Delta, Egypt — >1,500 people/km²
- North-eastern USA (Boston–Washington megalopolis)

Sparsely populated areas:
- Sahara and Arabian deserts
- Siberian taiga and tundra
- Central Australian interior
- Amazon Basin (despite being relatively populous by regional standards)
- Tibetan Plateau and Himalayan interior
- Greenland and Antarctica

Explaining the Distribution

Population distribution reflects a combination of physical, economic, historical and political factors:

Physical factors favouring high density:
- Flat, fertile agricultural land (alluvial plains, river valleys)
- Moderate climate with reliable rainfall (200–1,500 mm/year)
- Proximity to fresh water
- Access to coastlines and navigable rivers (trade)
- Low altitude (most people live below 500 m)

Physical factors limiting population:
- Extreme cold (polar regions: permafrost, short growing seasons)
- Extreme aridity (deserts: <250 mm rainfall cannot support agriculture)
- Extreme altitude (above ~3,500 m: low oxygen, poor soils, harsh climate)
- Steep terrain (limits agriculture and settlement)

Human factors:
- Historical agricultural civilisations formed in fertile river valleys (Nile, Indus, Yellow, Tigris-Euphrates)
- Industrial Revolution concentrated population in coal fields and ports (UK, Germany, north-eastern USA)
- Colonial-era trade routes and ports attracted settlement
- Continued urban migration amplifies existing concentrations

Population Density Measures

Arithmetic (crude) density: Total population ÷ total land area
Physiological density: Total population ÷ arable land area (better indicator of pressure on agricultural land)
Agricultural density: Agricultural population ÷ arable land area

KEY TAKEAWAY: Global population is concentrated in a band between the tropics and 60°N, particularly in South and East Asia, Western Europe, and north-eastern North America. Distribution reflects the intersection of physical opportunity (fertile soils, water, mild climate) and historical human processes (agricultural origins, industrialisation).

EXAM TIP: When describing population distribution, always distinguish between high-density and low-density areas, name specific regions or countries, and provide at least one explanatory factor linking distribution to physical or human geography.

COMMON MISTAKE: Students often describe distribution without linking it to causes. A complete response identifies the pattern AND explains why it exists (e.g., “The Indo-Gangetic Plain supports high population density because of its flat topography, fertile alluvial soils and reliable monsoonal rainfall, which sustain intensive rice and wheat agriculture”).

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