{"?xml":{"@version":"1.0"},"edm:RDF":{"@xmlns:dc":"http://purl.org/dc/elements/1.1/","@xmlns:edm":"http://www.europeana.eu/schemas/edm/","@xmlns:wgs84_pos":"http://www.w3.org/2003/01/geo/wgs84_pos","@xmlns:foaf":"http://xmlns.com/foaf/0.1/","@xmlns:rdaGr2":"http://rdvocab.info/ElementsGr2","@xmlns:oai":"http://www.openarchives.org/OAI/2.0/","@xmlns:owl":"http://www.w3.org/2002/07/owl#","@xmlns:rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","@xmlns:ore":"http://www.openarchives.org/ore/terms/","@xmlns:skos":"http://www.w3.org/2004/02/skos/core#","@xmlns:dcterms":"http://purl.org/dc/terms/","edm:WebResource":[{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-RV4AZD2B/8d7167a0-e4f9-497e-9519-295c2c209ce3/PDF","dcterms:extent":"1202 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-RV4AZD2B/f1fb68c5-d181-4719-88ae-4c3544e8384c/TEXT","dcterms:extent":"0 KB"}],"edm:TimeSpan":{"@rdf:about":"2006-2025","edm:begin":{"@xml:lang":"en","#text":"2006"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-RV4AZD2B","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-8USLDTJD"},{"@xml:lang":"sl","#text":"Revija za geografijo"}],"dcterms:issued":"2020","dc:creator":["Črepinšek, Zalika","Donša, Daša","Grujić, Jaša Veno","Ivajnšič, Danijel","Kajfež-Bogataj, Lučka","Kaligarič, Mitja","Pipenbaher, Nataša","Škornik, Sonja","Žiberna, Igor"],"dc:format":[{"@xml:lang":"sl","#text":"letnik:15"},{"@xml:lang":"sl","#text":"številka:2"},{"@xml:lang":"sl","#text":"str. 91-104"}],"dc:identifier":["ISSN:1854-665X","COBISSID_HOST:53075715","URN:URN:NBN:SI:doc-RV4AZD2B"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Univerza v Mariboru, Filozofska fakulteta"},"dc:subject":[{"@xml:lang":"en","#text":"climate changes"},{"@xml:lang":"en","#text":"heat waves"},{"@xml:lang":"sl","#text":"Ljutomer"},{"@xml:lang":"sl","#text":"mestni toplotni otoki"},{"@xml:lang":"sl","#text":"podnebne spremembe"},{"@xml:lang":"en","#text":"urban geography"},{"@xml:lang":"en","#text":"urban heat islands"},{"@xml:lang":"sl","#text":"urbana geografija"},{"@xml:lang":"sl","#text":"vremenski tipi"},{"@xml:lang":"sl","#text":"vročinski valovi"},{"@xml:lang":"en","#text":"weather types"}],"dcterms:temporal":{"@rdf:resource":"2006-2025"},"dc:title":{"@xml:lang":"sl","#text":"Letna dinamika pojava mestnega toplotnega otoka v malem urbanem sistemu|"},"dc:description":[{"@xml:lang":"sl","#text":"The urban heat island phenomenon (UHI) is a consequence of anthropogenic activity and local climatic conditions. Most UHI studies address large metropolitan areas. However, the data show that UHI magnitude can reach high values even in small urban systems. The study focused on the seasonal dynamics of the UHI magnitude variable (average, maximum and minimum temperature anomaly) in the town of Ljutomer by considering different weather types. Under anticyclonic or advective air circulation pattern, predominantly in summer, UHI magnitude in Ljutomer can reach values comparable to midsize or large urban systems (up to 8°C). The results of such studies are of particular concern in regard to increasing frequency of heat waves as a consequence of climate change, which further increases the already present heat stress in cities all over the Globe"},{"@xml:lang":"sl","#text":"Pojav mestnega toplotnega otoka (MTO) je posledica antropogenega spreminjanja prostora ter lokalnih podnebnih razmer. Večina študij o MTO obravnava velika metropolitanska območja. Podatki kažejo da je jakost pojava MTO lahko velika tudi v malih urbanih sistemih. V študiji smo se osredotočili na jakost pojava MTO v luči povprečnih, maksimalnih in minimalnih dnevnih temperatur zraka v različnih vremenskih tipih po sezonah v mestu Ljutomer. Ob anticiklonalni ali advektivni zračni cirkulaciji, predvsem v poletnih mesecih, je jakost MTO v Ljutomeru primerljiva srednjim in velikim urbanim sistemom (tudi do 8°C). Rezultati študije so še posebej zaskrbljujoči z vidika vse pogostejših vročinskih valov kot posledice podnebnih sprememb, ki še dodatno povečujejo, že tako prisotni, toplotni stres v mestih"}],"edm:type":"TEXT","dc:type":[{"@xml:lang":"sl","#text":"znanstveno časopisje"},{"@xml:lang":"en","#text":"journals"},{"@rdf:resource":"http://www.wikidata.org/entity/Q361785"}]},"ore:Aggregation":{"@rdf:about":"http://www.dlib.si/?URN=URN:NBN:SI:doc-RV4AZD2B","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-RV4AZD2B"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-RV4AZD2B/8d7167a0-e4f9-497e-9519-295c2c209ce3/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by/4.0/"},"edm:provider":"Slovenian National E-content Aggregator","edm:intermediateProvider":{"@xml:lang":"en","#text":"National and University Library of Slovenia"},"edm:dataProvider":{"@xml:lang":"sl","#text":"Univerza v Mariboru, Filozofska fakulteta"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-RV4AZD2B/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-RV4AZD2B"}}}}