20.500.12556/DKUM-88945 Mestna klima Dravograda, Slovenj Gradca in Raven na Koroškem magistrsko delo The city climate of Dravograd, Slovenj Gradec and Ravne na Koroškem Spreminjanje naravne pokrajine zaradi procesa urbanizacije je vse pogostejši pojav v sodobnem času. Ljudje namreč v mestih proizvedemo veliko umetne energije. Z asfaltnimi in betonskimi površinami spreminjamo tako energijsko kot vodno bilanco ter z vse pogostejšo visoko gradnjo vplivamo tudi na lokalno zračno cirkulacijo. Tako človek z lastnim vnosom toplote, z gostejšo pozidanostjo in odsotnostjo vegetacije spreminja temperaturo zraka, relativno vlago, smer ter hitrost vetra in višino padavin. Vse te spremembe se v okolju manifestirajo v obliki specifične t. i. »mestne klime«, za katero so značilne višje temperature od tistih v okolici mesta. Toplotni otok Dravograda, mesta Slovenj Gradec in Raven na Koroškem je najizrazitejši v središčih naselij, od koder se glede na različne vremenske tipe širi v različne smeri. Na obliko toplotnega otoka v vseh treh naseljih poleg gostote pozidanosti, gostote prebivalstva in antropogenega vnosa energije, vpliva še relief, večje vodne površine ter zelene površine. Oblika in intenziteta toplotnega otoka se tekom dneva spreminja. Temperaturni maksimumi in minimumi se čez dan razvijajo v različnih delih naselij. The alteration of the natural landscape due to the process of urbanization is becoming increasingly common in modern times. People generate a significant amount of artificial energy in cities. Through asphalt and concrete surfaces, we alter both the energy and water balance, and with the increasingly frequent high-rise construction, we also influence local air circulation. Thus, humans, with their own heat input, denser built-up areas, and absence of vegetation, modify air temperature, relative humidity, wind direction and speed, and rainfall height. All these changes manifest in the environment in the form of specific "urban climate," characterized by higher temperatures than those in the surrounding countryside. The heat island of Dravograd, the city of Slovenj Gradec, and Ravne na Koroškem is most pronounced in the centers of the places, from where it spreads in different directions depending on the various weather types. In all three locations, the shape of the heat island is influenced not only by building density, population density, and anthropogenic energy input but also by relief, larger water surfaces, and green areas. The shape and intensity of the heat island change throughout the day. Temperature maxima and minima develop in different parts of the places during the day. Mestna klima toplotni otok temperaturne razlike med mestom in okolico temperaturni profil urban climate heat island temperature differences between the city and its surroundings temperature profile true true false I. Dvornik Polenik Slovenski jezik Angleški jezik Dravograd (Slovenija); Slovenj Gradec (Slovenija); Ravne na Koroškem (Slovenija); Magistrsko delo/naloga 2024-05-31 09:29:50 2024-07-08 15:20:10 2024-07-09 03:49:50 0000-00-00 00:00:00 2024 0 Maribor 0 Maribor 1 spletni vir (1 datoteka PDF (XVI, 204 str.)) 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 551.582(497.413)(043.2) 201077507 MAG_Dvornik_Polenik_Ivo_2024.pdf MAG_Dvornik_Polenik_Ivo_2024.pdf 1 C9405334B7E79B9245C067BCE1E21D77 434190ca19a09fe7ebdcf70e9db2dbca565a9f9f01ac8aa349e6716b151d208b 423e606b-1f21-11ef-bf9d-00155d000105 https://dk.um.si/Dokument.php?lang=slv&id=180030 Filozofska fakulteta 0 0 0