Overview of Heat islands map

The increasing frequency of heat waves is one of the main future climate risks in Estonia and elsewhere in the world. Heat waves are amplified primarily in cities, but also in densely populated areas as a heat island effect, where large dark surfaces (e.g. asphalt roads, asphalt-covered parking lots, bitumen roofs) absorb most of the solar radiation, which in turn heats the air in the urban space. An analysis was completed in cooperation with the Ministry of the Environment and the Environmental Agency, during which the formation of heat islands in Tallinn, Tartu, Pärnu, Viljandi, Rakvere, Narva and Kohtla-Järve was studied based on Landsat8 satellite data. The analysis and the completed map application are good support material for local governments and planners. The heat island effect can be mitigated by limiting heat accumulation through planning and construction solutions and by implementing microclimatic measures in the urban environment, preserving and expanding green areas, landscaping and water bodies.

The report "Assessment of heat islands in Estonian cities in 2014-2019" (in estonian), map layers and map story can be found on the Environmental Portal.

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ID: soojussaared_2021_juuni

Nimi
Soojussaared (19. juuni 2021)
Metaandmed
Linna soojussaar on ümbritsevast maapiirkonnast märkimisväärselt soojem linnastunud ala. Tegemist on satelliitpiltidelt arvutatud kiirgustemperatuuridega kasutades kolme lävendit: üle +30°C, üle +35°C ja üle +40°C. Neil hinnangulistel kiirgustemperatuuridel on tugev seos nii maapinna kui ka õhutemperatuuriga. Kuupäevade valik on tehtud vastavalt suvistele kuumalainetele ja vastavalt satelliitandmete olemasolule.
Name
Heat islands (June 19, 2021)
Metadata
An urban heat island is an urbanized area that is significantly warmer than the surrounding rural landscape. It refers to radiation temperatures calculated from satellite imagery using three thresholds: above +30 °C, above +35 °C, and above +40 °C. These estimated radiation temperatures are strongly correlated with both land‑surface and air temperatures. The dates were chosen according to summer heat waves and´according to satellite data availability.
copyright
Keskkonnaaagentuur
WFS URL
WMS URL

Last update: 23.04.2025 11:39
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