Counteracting Urban Heat Island Effects in a Global Climate Change Scenario 2016
DOI: 10.1007/978-3-319-10425-6_12
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Urban Heat Island in the Ljubljana City

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Cited by 5 publications
(5 citation statements)
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“…Increased ambience temperatures deteriorate the physical well-being of a city's population, as a result of thermoregulatory Sustainability 2017, 9, 122 3 of 20 morning time to having a top speed of around 2-3 m/s in the afternoon (both stations); air humidity was the lowest at that time (both stations). The weak SW wind and low humidity caused low night-time temperatures, especially at the rural station where the UHI intensity rose by 0.5-2 K [17] (pp. 363-365).…”
Section: Introductionmentioning
confidence: 99%
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“…Increased ambience temperatures deteriorate the physical well-being of a city's population, as a result of thermoregulatory Sustainability 2017, 9, 122 3 of 20 morning time to having a top speed of around 2-3 m/s in the afternoon (both stations); air humidity was the lowest at that time (both stations). The weak SW wind and low humidity caused low night-time temperatures, especially at the rural station where the UHI intensity rose by 0.5-2 K [17] (pp. 363-365).…”
Section: Introductionmentioning
confidence: 99%
“…The weak SW wind and low humidity caused low nighttime temperatures, especially at the rural station where the UHI intensity rose by 0.5-2 K [17] (pp. 363-365).…”
Section: Introductionmentioning
confidence: 99%
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“…The warming trend in Ljubljana is between 0.3 and 0.4 • C/10 years [27]. As in many other cities, the warming trend in Ljubljana is the result of a combination of climate change and the city's UHI effect that has existed for decades [6,20,21]. Despite the temperate continental climate, Ljubljana has a fairly humid climate.…”
Section: Study Areamentioning
confidence: 99%
“…The intensity of the UHI in Ljubljana is said to have increased, especially after 1950. Komac et al [21] published a study of UHI measurements in Ljubljana as a combination of satellite imagery and a comparison of temperatures and hot days between the city and its surroundings. They demonstrated an increase in the number of hot days and a decrease in the number of cold days in Ljubljana, as well as an internal differentiation of surface warming indicating a surface urban heat island (SUHI).…”
mentioning
confidence: 99%