Pafos [Administrative division]

Extreme heat occurs when air temperatures significantly exceed normal seasonal averages for prolonged periods, creating conditions that stress human thermoregulation and can lead to heat-related illness. The hazard is measured using indices that combine temperature and humidity to assess heat stress on the human body, such as wet bulb globe temperature (WBGT). The severity depends on temperature intensity, duration, humidity levels, nighttime cooling, and the vulnerability of exposed populations.

In the area you have selected (Pafos) extreme heat hazard is classified as medium based on modeled heat information currently available to this tool. This means that there is approximately 5% chance per year that at least one period of prolonged exposure to extreme heat, resulting in heat stress, will occur (about 23% chance in the next five years). Risk studies, project planning decisions, project design, and construction methods should take into account the level of extreme heat hazard.

According to the most recent assessment report of the Intergovernmental panel on Climate Change (IPCC, 2013), continued emissions of greenhouse gases will cause further warming, and it is virtually certain that there will be more frequent hot temperature extremes over most land areas during the next fifty years. Warming will not be regionally uniform. In the area you have selected, the temperature increase in the next fifty years will be slightly lower than the worldwide average, but still significant. It would be prudent to design projects in this area to be robust to global warming in the long-term.

For hazard management recommendations, see documentation.

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Based on the global extreme heat maps published by GFDRR-VITO (2025). Available for download at Risk Data Library.

We welcome any suggestions for improvements to the tool, including suggestions of data, recommendations, or resources to include.

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