Waves crash into sea walls in coastal town in south-west England, during severe weather and flood crisis. Source: BBC Editorial

Whatever Climate Change Does to the World, Cities Will Be Hit Hardest

More than half of humanity is crowded together in cities. That’s about 4 billion people living on top of one another, working, commuting, polluting, and figuring out how to survive. And that proportion will only rise: By the end of the century, about 85% of the world’s population will be urban, according to the Organization for Economic Cooperation and Development.

Cities are also incredibly vulnerable to climate change. High temperatures, sea level rise, and extreme weather are all felt more acutely in urban areas. Built on concrete, they absorb solar radiation but not water, making the effects of both heat waves and heavy rains more severe.

If humans keep emitting planet-warming greenhouse gases at our current pace, Earth will warm by at least 3C and as much as 4C by the end of the century compared with preindustrial temperatures, causing much of the planet to become unlivable. Radical emissions cuts could change that forecast if they’re made within the next few decades. Lockdowns during the coronavirus led to a record 7.5% drop in emissions in 2020, but the reduction was short-lived. The latest data from the International Energy Agency shows that global emissions were 2% higher in December than at the same point in 2019.

No matter how much the world warms, cities will have it worse, with average summer temperatures rising between 1.9C and 4.4C above current levels, depending on how the future plays out, according to a research team led by Lei Zhao at the University of Illinois. That increase will lead to more deaths in places with scarce resources to adapt and mitigate the effects of a changing climate.

By 2100, cities will be significantly hotter than surrounding regions

Average summer temperature change under RCP 4.5

Difference between projected urban warming and background regional warming

–0.9C

1.3C

Buenos Aires

6

ARGENTINA

URUGUAY

5

4

+1.1C

Urban warming

3

Buenos Aires

2

+1.0C

Region warming

1

2000

2100

Muscat

6

5

4

Muscat

UAE

+1.6C

3

2

+1.4C

SAUDI

ARABIA

1

OMAN

2000

2100

Melbourne

6

AUSTRALIA

5

4

3

Melbourne

+1.1C

2

1

+0.7C

2000

2100

Difference between projected urban warming

and background regional warming

–0.9C

1.3C

Buenos Aires

6

5

ARGENTINA

URUGUAY

4

+1.1C

Urban warming

3

Buenos Aires

2

+1.0C

Region warming

1

2000

2100

Muscat

6

5

4

Muscat

+1.6C

3

UAE

2

+1.4C

SAUDI

ARABIA

1

OMAN

2100

2000

Melbourne

6

AUSTRALIA

5

4

3

+1.1C

Melbourne

2

1

+0.7C

2100

2000

Difference between projected urban warming

and background regional warming

–0.9C

1.3C

Buenos Aires

ARGENTINA

URUGUAY

Buenos Aires

Muscat

Muscat

UAE

OMAN

Melbourne

AUSTRALIA

Melbourne

Difference between projected urban warming and background regional warming

–0.9C

1.3C

Buenos Aires

6

ARGENTINA

URUGUAY

5

4

+1.1C

Urban warming

3

Buenos Aires

2

+1.0C

Region warming

1

2000

2100

Muscat

6

5

4

Muscat

UAE

+1.6C

3

2

+1.4C

SAUDI

ARABIA

1

OMAN

2000

2100

Melbourne

6

AUSTRALIA

5

4

3

Melbourne

+1.1C

2

1

+0.7C

2000

2100

Difference between projected urban warming and background regional warming

–0.9C

1.3C

AUSTRALIA

ARGENTINA

URUGUAY

Muscat

UAE

Melbourne

Buenos Aires

SAUDI

ARABIA

OMAN

Buenos Aires

Muscat

Melbourne

6

6

5

5

4

4

+1.6C

+1.1C

Urban warming

3

3

+1.1C

2

2

+1.0C

Region warming

+1.4C

+0.7C

1

1

2000

2100

2000

2100

2000

2100

Note: Urban temperatures are currently between 1 and 2 degrees Celsius warmer than surrounding areas due to the urban heat island effect, according to Zhao’s research

By 2100, cities will be significantly hotter than surrounding regions

Average summer temperature change under RCP 8.5

Difference between projected urban warming and background regional warming

–0.9C

1.3C

Buenos Aires

6

ARGENTINA

URUGUAY

5

+2.4C

Urban warming

4

3

Buenos Aires

2

+1.2C

Region warming

1

2000

2100

Muscat

6

+3.8C

5

4

Muscat

UAE

+3.0C

3

2

SAUDI

ARABIA

1

OMAN

2000

2100

Melbourne

6

AUSTRALIA

5

+2.7C

4

3

Melbourne

+2.6C

2

1

2000

2100

Difference between projected urban warming

and background regional warming

–0.9C

1.3C

Buenos Aires

6

5

ARGENTINA

URUGUAY

+2.4C

Urban warming

4

3

Buenos Aires

2

+1.2C

Region warming

1

2000

2100

Muscat

6

+3.8C

5

4

Muscat

3

+3.0C

UAE

2

SAUDI

ARABIA

1

OMAN

2000

2100

Melbourne

6

AUSTRALIA

5

+2.7C

4

3

+2.6C

Melbourne

2

1

2100

2000

Difference between projected urban warming

and background regional warming

Difference between projected urban warming

and background regional warming

–0.9C

–0.9C

1.3C

1.3C

Buenos Aires

ARGENTINA

URUGUAY

Buenos Aires

Muscat

Muscat

UAE

OMAN

Melbourne

AUSTRALIA

Melbourne

Difference between projected urban warming and background regional warming

–0.9C

1.3C

Buenos Aires

6

ARGENTINA

URUGUAY

5

+2.4C

Urban warming

4

3

Buenos Aires

2

+1.2C

Region warming

1

2000

2100

Muscat

6

+3.8C

5

4

Muscat

UAE

3

+3.0C

2

SAUDI

ARABIA

1

OMAN

2000

2100

Melbourne

6

AUSTRALIA

5

+2.7C

4

3

Melbourne

+2.6C

2

1

2000

2100

Difference between projected urban warming and background regional warming

–0.9C

1.3C

AUSTRALIA

ARGENTINA

URUGUAY

Muscat

UAE

Melbourne

Buenos Aires

SAUDI

ARABIA

OMAN

Buenos Aires

Muscat

Melbourne

6

6

+3.8C

5

5

+2.4C

Urban warming

+2.7C

4

4

+3.0C

3

3

+2.6C

2

2

+1.2C

Region warming

1

1

2000

2100

2000

2100

2000

2100

Note: Urban temperatures are currently between 1 and 2 degrees Celsius warmer than surrounding areas due to the urban heat island effect, according to Zhao’s research

Cities in the northern U.S., southern Canada, central and northern Asia, the Middle East, Europe, and northwestern China will experience the most pronounced warming by the end of the century.

In March, Muscat got a preview of what’s coming for cities in the Arabian peninsula when thermometers hit 41.3C (106.3F), a temperature typically reached around June. The Omani capital will be between 1.6C and 3.8C hotter on average by 2100.

The previous images showed the expected temperature change under a middle-of-the road emissions scenario, known as RCP 4.5, which assumes emissions will peak around 2040. These images show the worst-case scenario, RCP 8.5, which is controversial because it factors in unlikely events such as a significant expansion of coal consumption. Scientists use it less and less, but it’s still useful to illustrate where the world could wind up without emissions controls.

Summer temperatures in Buenos Aires, meanwhile, are rising faster than the global average, for a total increase of 1.3C over the past three decades. Humidity and the lack of green space will make the heat worse.

Warming in Melbourne will exacerbate extreme events like the heatwaves, bushfires, and rains experienced in recent months. It’s likely to take a toll on city dwellers too–during a heatwave in 2009, ambulance calls rose 46%.

Being close to the sea has historically been an advantage, but today some of the world’s most densely populated urban areas are suffering disproportionately from rising tides. Coastal areas representing 58% of the world’s population have experienced relative sea level increases of 7.8 millimeters to 9.9mm annually, according to scientific research. That compares with an average sea level increase of 2.5mm a year globally for the past two decades.

When extreme weather events hit, people in the countryside seek safe harbor in cities, which have stronger infrastructure and more hospitals and other essential services. To a storm refugee, that can make the difference between life and death.

Most people displaced by natural disasters eventually return to their place of origin. But not all. Some settle in the suburbs or on the outskirts of cities, adding further stress to urban infrastructure, services, and resources.

Bangladesh’s capital, Dhaka, is one of the most densely populated cities on Earth, nearly twice as crowded as the island of Manhattan. About 40% of the city’s 14 million residents live in informal settlements, and 70% of those were forced to leave their homes because of phenomena related to climate change, including cyclones and coastal and riverbank erosion.

People fleeing to second-largest city
Researchers tracking Bangladeshi mobile phones detected an influx of people arriving in Chittagong, the country’s second-largest city, two days after the cyclone hit. Within six weeks, 50,000 people had arrived from almost every corner of the country. Photo: STRDEL/AFP via Getty Images

Displacement doesn’t happen only in developing nations. Cities like Buffalo, N.Y., are labeling themselves climate havens and opening themselves up to climate migrants. In the U.S., 13 million coastal residents are expected to be displaced from their homes by the end of the century as sea levels rise, according to a 2020 Plos One study.

By 2100, flooding will displace millions on the coasts

Percentage of people living on flooded land, by county

5

10

25

50%

5

10

25

50%

5

10

25

50%

5

10

25

50%

Seattle

Boston

New York

Philadelphia

San Francisco

Washington, D.C.

Los Angeles

San Diego

New Orleans

Orlando

Houston

Tampa

Miami

5

10

25

50%

Seattle

Boston

New York

Philadelphia

San Francisco

Washington, D.C.

Los Angeles

San Diego

New Orleans

Orlando

Houston

Tampa

Miami

By 2100, flooding will displace millions on the coasts

Percentage population increase due to sea level rise, by county

1

3

6

9%

1

3

6

9%

1

3

6

9%

1

3

6

9%

Seattle

Boston

Detroit

New York

Philadelphia

Chicago

San Francisco

Washington, D.C.

Las Vegas

Nashville

Los Angeles

Memphis

Columbia

San Diego

Atlanta

Dallas

New Orleans

Austin

Orlando

Houston

Tampa

Miami

1

3

6

9%

Seattle

Boston

Detroit

New York

Philadelphia

Chicago

San Francisco

Washington, D.C.

Las Vegas

Nashville

Los Angeles

Memphis

Columbia

San Diego

Atlanta

Dallas

New Orleans

Austin

Orlando

Houston

Tampa

Miami

Sea levels could rise as much as 6 feet in certain places under the worst-case scenario.

As people flee coastal counties, inland populations will increase. Extreme events such as 2005’s Hurricane Katrina or last year’s wildfires in California show that a flood of internal migrants can lead to a spike in housing prices in the counties where people resettle.

In many places, heat and flooding aren’t either-or. Some cities are or will be affected by both, making adaptation and mitigation efforts even more challenging.

A Deadly Combination

High heat and humidity together render the body’s defenses useless

+35C

Temperature

100%

Humidity

6 hours

Maximum time

6 hours

Maximum time

+35C

Temperature

100%

Humidity

6 hours

Maximum time

+35C

Temperature

100%

Humidity

Humans can bear either high temperatures or high humidity, but the two things combined can be deadly. The body copes with heat by sweating, but when the air is damp already, that defense becomes useless.

Climate models project the first occurrences of deadly combined heat and humidity will arrive by mid-century. But scientists have found that such episodes have already taken place at least twice and that the frequency of extreme humidity and heat has more than doubled since 1979. Under business-as-usual emissions scenarios, these conditions will occur several times in the North China Plain between 2070 and 2100, MIT researchers found.

Tianjin, only 80 miles east of Beijing and one of China’s largest cities, is likely to be affected by both extreme humidity and heat. The city has a population of 12.8 million and sits at the heart of China’s most populous and agriculturally important region.

Tianjin at Risk

Temperature increase in the city and sea level rise by 2100 under RCP 4.5

–0.9C

2.5C

Area at risk of flooding

2.5C

Tianjin

Bohai

Bay

10 mi

10 km

Temperature increase in the city and sea level rise by 2100 under RCP 4.5

–0.9C

2.5C

Area at risk of flooding

2.5C

Tianjin

Bohai

Bay

10 mi

10 km

Temperature increase in the city and sea level

rise by 2100 under RCP 4.5

–0.9C

2.5C

Area at risk of flooding

2.5C

Tianjin

Bohai

Bay

10 mi

10 km

Sea level rise will wipe out most of Tianjin’s current surface area if no adaptation measures are taken. Meanwhile, average temperatures in the city are expected to increase between 2.5C and 5C above current levels.

As the world warms, the effects of climate change will become more unpredictable, with storms, cold spells, and heat waves often matching or even surpassing scientists’ worst-case scenarios. Cities and their dwellers will need to spend trillions to mitigate damages, adapt, and survive in a planet that’s growing more hostile by the minute.