Urban heat island - Nicosia

Where the city holds its heat

863 mapped cells scoring urban heat risk, exposure, vulnerability, and heat-island potential across Nicosia.

Indicator

UHI potential (UHIp) from a physics-constrained model trained on temperature measurements. Shows where the built form is more likely to store and release heat.

Land classification

Filter the heat cells to a WUDAPT local climate zone group.

Am I affected?Search, use GPS, or pick the map

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Map displayRoad / 1 visible
Base map
Heatmap style
Visible layers
Data source

Risk, exposure, vulnerability, and UHIE potential: Nicosia study dataset. Local climate zones: WUDAPT global LCZ map.

Read the map

Tap any cell to see how much heat it holds and who lives there.

Very Low0.0 to 2.0
Low2.0 to 4.0
Moderate4.0 to 6.0
High6.0 to 8.0
Very High8.0 to 10.0
What does each 0-10 score mean?
0.0 to 2.0 · Very Low

Very Low relative UHIE potential in the supplied dataset.

2.0 to 4.0 · Low

Low relative UHIE potential in the supplied dataset.

4.0 to 6.0 · Moderate

Moderate relative UHIE potential in the supplied dataset.

6.0 to 8.0 · High

High relative UHIE potential in the supplied dataset.

8.0 to 10.0 · Very High

Very High relative UHIE potential in the supplied dataset.

01The phenomenon

Why do some streets stay hot long after sunset?

The urban heat island effect happens when built-up parts of Nicosia become warmer than nearby rural or greener areas. Roads, roofs, and dense buildings absorb solar heat all day and release it slowly after dark, so some streets simply never get the chance to cool down.

Hard Surfaces Absorb Heat

1

Dark roofs, asphalt, and exposed pavements absorb solar energy. By afternoon, they can become much hotter than shaded soil or vegetation.

City roofs and paved surfaces absorbing heat under strong sun

Dense Blocks Release It Slowly

2

Close buildings and narrow streets hold warm air. At night, stored heat is released back into the street, so the city cools more slowly.

Dense city blocks releasing stored heat after sunset

Daily Exposure Adds Up

3

Higher outdoor temperatures affect walking, work, transport, schools, and older residents. The same temperature can be more dangerous in exposed streets.

Pedestrians and transport moving through a hot urban street
02The study

What this map is made of

863mapped cells
200 mcell size
H × E × Vrisk model

The Nicosia layer is built from the study's UHI risk dataset. The city is divided into 863 cells of 200 × 200 metres each, roughly the scale of an urban block. Every cell carries four standardized indicators: combined risk, heat-island potential (hazard), population exposure, and demographic vulnerability.

How to read the four indicators

What the three components measure, and how they combine into risk. Methodology basis: the supplied Nicosia UHI risk dataset and its accompanying modelling study.

Values at the selected location
01

UHI Risk

Risk is calculated as Hazard × Exposure × Vulnerability. Because the three factors are multiplied, a low value in any single component significantly reduces overall risk. High UHI risk only emerges where strong heat potential coincides with both high population presence and high demographic susceptibility.

02

Hazard: UHI Potential

The UHI potential (UHIp), derived from a physics-constrained model trained on car-mounted temperature measurements. It represents how much each cell can raise local temperature due to its built form, averaged for the August-September peak heat window.

03

Exposure: Population

Total population living inside each 200 × 200 m cell. Before being used in the risk calculation, population values are adjusted using a logarithmic scale so that areas with very large populations do not disproportionately influence the results. Cells with no population have an exposure value of zero.

04

Vulnerability: Demographics

The share of vulnerable people in each cell, calculated as (pregnant women + infants + elderly) divided by total population. This produces a ratio between 0 and 1 that highlights cells where a greater proportion of residents may be more susceptible to heat-related impacts.

How to read the scores

All hazard and exposure layers are standardized to a 0-1 range using min-max normalization. On the platform, this is displayed as a 0-10 scale for readability. A score is not an absolute measurement. It marks how a cell compares to others in the study area. A cell scoring 8.1 / 10 on exposure means it is near the top of the population range across all 863 cells, not that a specific number of people are at risk.

When the map shows 'Vulnerable population: 41', that means an estimated 41 pregnant women, infants, and elderly persons live inside that single 200 × 200 m cell. 'Vulnerable share: 16%' means they make up 16% of the cell's total population.

03Cooling the city

How Nicosia can cool down

Evidence-based strategies for reducing urban heat, street by street.

The same neighbourhood, with and without green infrastructure

04Project support

The project behind the Nicosia maps

The climate risk assessment and the resulting maps presented on this website were produced using the CLIMAAX methodological framework through the CLIMAAX-NIC project. The project is implemented by the Nicosia Municipality in collaboration with the CYENS Centre of Excellence and is funded by the European Union under the Horizon Europe programme.