Climate risk in Manchester
England, United Kingdom
Main risks in Manchester
Heat, downpours and earthquakes threaten Manchester less than most of the world's 626 large cities.
The sea at Manchester is projected to rise 21 cm by 2050 if emissions level off. [1]
Counted from the 1995-2014 average; 14 cm of it comes after 2020. Higher than 51% of the world's large coastal cities.
For comparison: Rio de Janeiro 20 cm, Singapore 20 cm, Seoul 20 cm.
21 cm Natural Earth Sea level rise by 2050 over the 1995-2014 average, if emissions level off
This week in Manchester
This week's forecast risk around the city, by day and by hour, and the hazard events near it now. [2] [3]
This week's forecast for the city cannot be shown here right now.
Open the city on the mapThe 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 mapManchester's climate in the 2050s
2041-2060 compared with 1991-2020, if emissions level off [4] [5]
By the 2050s, Manchester's climate will have changed but will still be closer to its own today than to any other large city's. Of the others, Amsterdam (Netherlands) comes closest.
+1.1 °C
Mean temperature over the year
+1.7 °C
Average daily high, warmest month
+0.7 °C
Average nightly low, coldest month
-1%
Precipitation over the year
If emissions keep rising, Manchester would have the climate that Amsterdam (Netherlands) has 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. 2 of the 3 estimates from the climate models, the middle one and the two ends of their range, point to Amsterdam. [6]
Everything else measured
From the highest among the world's 626 large cities to the lowest.
| Reading | Manchester | Among 626 large cities | Rank in the United Kingdom (1 = highest) |
|---|---|---|---|
| Drought risk [7] | High | the same grade as 44% of large cities; higher than 50%, lower than 6% | |
| Earthquake shaking on firm ground, 10% chance in 50 years [8] | moderate shaking, 0.06 g | higher than 48% of large cities | Rank in the United Kingdom (1 = highest): 1 of 6 |
| Days with 20 mm of rain or more in 2025 [9] | 7 days | higher than 40% of large cities | Rank in the United Kingdom (1 = highest): 1 of 6 |
| Water stress [7] | Low-Medium: 10 to 20% of the available water drawn | the same grade as 12% of large cities; higher than 30%, lower than 58% | |
| Hottest day of 2025 [9] | 28.5 °C | higher than 4% of large cities | Rank in the United Kingdom (1 = highest): 6 of 6 |
| Warming by 2050, if emissions level off [5] | +1 °C | higher than 1% of large cities | Rank in the United Kingdom (1 = highest): 4 of 6 |
| Hot days in 2025, over 35 °C [9] | 0 days | like 37% of large cities | |
| Tropical nights in 2025, over 20 °C [9] | 0 nights | like 14% 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] | 0% | like 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.
- Sheffield · United Kingdom · 51 km
- Leeds · United Kingdom · 58 km
- Birmingham · United Kingdom · 110 km
- London · United Kingdom · 260 km
Large cities in the United Kingdom
Sources
- IPCC AR6 Sea Level Projections: sea level rise
- Environment and Climate Change Canada: Global Deterministic Prediction System (GDPS): the week's forecast map
- EUMETNET MeteoAlarm, Environment and Climate Change Canada, Mexico's Servicio Meteorológico Nacional, the India Meteorological Department, Brazil's Instituto Nacional de Meteorologia and national weather services, via WMO WIS2: flood near the city now
- TerraClimate: the 2050s comparison
- NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP-CMIP6): the 2050s comparison, warming
- Mahony, Cannon, Wang and Aitken (2017). A closer look at novel climates: new methods and insights at continental to landscape scales. Global Change Biology 23, 3934-3955: how climates are compared
- Aqueduct 4.0 Water Risk Framework: drought risk, water stress
- GSHAP Global Seismic Hazard Map: earthquake shaking
- ERA5 Single Levels Daily Statistics: heavy rain, hottest day, hot days, nights
- Aqueduct Floods Hazard Maps: river flood depth, coastal floods
- Global Land Subsidence Mapping Reveals Widespread Loss of Aquifer Storage Capacity: sinking land
- Global Biomass Burning at 500 m (GFED500): burned land
- IRIS: the Imperial College Storm Model dataset: tropical cyclone wind
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Source: Criora (criora.com), based on IPCC, ECCC, EUMETNET MeteoAlarm, Environment and Climate Change Canada, Mexico's Servicio Meteorológico Nacional, the India Meteorological Department, Brazil's Instituto Nacional de Meteorologia and national weather services, via WMO WIS2, TerraClimate, NEX-GDDP-CMIP6, WRI, GSHAP, ECMWF, HydroShare, GFED500, IRIS
APA
Criora. (2026). Manchester, United Kingdom: climate risk profile [Data set]. Retrieved November 4, 2026, from https://criora.com/atlas/GBR/manchester BibTeX
@misc{criora_atlas_GBR_manchester_2026,
author = {{Criora}},
title = {Manchester, United Kingdom: climate risk profile},
year = {2026},
url = {https://criora.com/atlas/GBR/manchester},
urldate = {2026-11-04}
} The figures may be reused on the terms of their sources, which this page names.
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