Criora

Climate risk in Cape Town

Western Cape, South Africa

Main risks in Cape Town

Heat, downpours and earthquakes threaten Cape Town less than most of the world's 626 large cities.

The sea at Cape Town is projected to rise 22 cm by 2050 if emissions level off. [1]

Counted from the 1995-2014 average; 17 cm of it comes after 2020. Higher than 70% of the world's large coastal cities.

For comparison: Lagos 23 cm, Abidjan 23 cm, Tokyo 21 cm.

22 cm Natural Earth

Sea level rise by 2050 over the 1995-2014 average, if emissions level off

0 100 cm
See the sea level rise around Cape Town on the live map 

This week in Cape Town

This week's forecast risk around the city, by day and by hour, and the hazard events near it now. [2] [3]

Open the city on the map

The Earth right now

The Earth's pulse reads the whole world, not this city, so it is the same on every city's page.

Earth's pulse, from 0 to 100. It rises with the number of people in the path of disasters now under way; 90 matches the 2004 tsunami.

Open the live map

Where else Cape Town stands out

extremely high

Water stress [4]

The top grade of its scale, shared by 30% of the world's large cities.

Around the city on the map

Water stress

Natural Earth
Water stress Low (<10%) Low-Medium (10-20%) Medium-High (20-40%) High (40-80%) Extremely High (>80%) Arid, low water use
See the water stress around Cape Town on the live map 

Cape Town's climate in the 2050s

2041-2060 compared with 1991-2020, if emissions level off [5] [6]

By the 2050s, Cape Town's climate will be unlike any large city's today, its own included; of the other cities, Port Elizabeth (South Africa) comes closest.

+0.9 °C

Mean temperature over the year

+1.0 °C

Average daily high, warmest month

+0.8 °C

Average nightly low, coldest month

-13%

Precipitation over the year

If emissions keep rising, it will differ even more from the climate of every large city today.

Climates are compared on seasonal temperature and rainfall alone, each difference weighed against the city's usual swings from year to year (the method of Mahony et al. 2017); heat waves, the heat of city streets and the rising sea are left out. All 3 estimates from the climate models, the middle one and the two ends of their range, point to Port Elizabeth. [7]

Everything else measured

From the highest among the world's 626 large cities to the lowest.

Earthquake shaking on firm ground, 10% chance in 50 years [8] moderate shaking, 0.05 g higher than 46% of large cities Rank in South Africa (1 = highest): 2 of 6
Days with 20 mm of rain or more in 2025 [9] 6 days higher than 37% of large cities Rank in South Africa (1 = highest): 5 of 6
Tropical nights in 2025, over 20 °C [9] 1 night higher than 14% of large cities Rank in South Africa (1 = highest): 4 of 6
Drought risk [4] Medium-High the same grade as 38% of large cities; higher than 12%, lower than 50%
Warming by 2050, if emissions level off [6] +1.2 °C higher than 4% of large cities Rank in South Africa (1 = highest): 6 of 6
Hottest day of 2025 [9] 27.7 °C higher than 3% of large cities Rank in South Africa (1 = highest): 6 of 6
Hot days in 2025, over 35 °C [9] 0 days like 37% of large cities
River flood depth, 100-year event [10] Dry at the centre; other districts can flood like 85% of large cities
Share of the land around the centre (a 10 km square) that a 100-year flood from the sea puts under 0.5 m of water or more [10] 0% today and by 2080 if emissions keep rising like 74% of large coastal cities
Share of land sinking over 1 cm a year, within 15 km [11] 1% higher than at least 80% of large cities
Land burned in an average year [12] 0% like 84% of large cities
Tropical cyclone wind, once in 100 years [13] No hurricane or typhoon reaches here like 71% of large cities
  • Flood depth is given for one 1 km square at the city centre, in today's climate.
  • Earthquake shaking is given for firm ground in g, the acceleration of gravity: around 0.1 g shaking is strong and can cause light damage, on the US Geological Survey's scale. The figure is the typical value over all the land within 15 km of the centre, not that of one point. Soft ground, such as an old lake bed or river silt, shakes harder.
  • Land subsidence comes from a model of satellite radar measurements from 2013 to 2019 in 2 km squares, read over all the land within 15 km of the centre rather than at one point.
  • Water stress is the share of the available water drawn every year. Drought risk is how often droughts come, against the area's own usual rain, and how many people and how much farmland they would reach. Both are graded on WRI's own scale.
  • If emissions level off: the IPCC's SSP2-4.5 scenario.
  • Water stress and drought risk have no rank in the country: they are steps of a scale, and many cities share one.
  • Tsunamis and landslides are not rated for a single city here.

The nearest large cities

Distance from centre to centre.

Cite or embed

Cite this page

In a line

Source: Criora (criora.com), based on IPCC, ECCC, NASA Fire Information for Resource Management System (FIRMS), WRI, TerraClimate, NEX-GDDP-CMIP6, GSHAP, ECMWF, HydroShare, GFED500, IRIS

APA

Criora. (2026). Cape Town, South Africa: climate risk profile [Data set]. Retrieved November 4, 2026, from https://criora.com/atlas/ZAF/cape-town

BibTeX

@misc{criora_atlas_ZAF_cape_town_2026,
  author = {{Criora}},
  title = {Cape Town, South Africa: climate risk profile},
  year = {2026},
  url = {https://criora.com/atlas/ZAF/cape-town},
  urldate = {2026-11-04}
}

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