<?xml version="1.0"?><rdf: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-I8EV3HXF/b8057561-efb2-4bb8-b19c-75f04e346c4c/PDF"><dcterms:extent>1012 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-I8EV3HXF/1fc8343f-a961-4c7f-843e-66a4811f24d3/TEXT"><dcterms:extent>0 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="2013-2025"><edm:begin xml:lang="en">2013</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-I8EV3HXF"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-MCCAWXYE" /><dcterms:issued>2021</dcterms:issued><dc:creator>Kobal, Milan</dc:creator><dc:creator>Nastran, Mojca</dc:creator><dc:creator>Pečan, Petra</dc:creator><dc:creator>Simčič, Anica</dc:creator><dc:format xml:lang="sl">številka:125</dc:format><dc:format xml:lang="sl">str. 13-24</dc:format><dc:identifier>DOI:10.20315/ASetL.125.2</dc:identifier><dc:identifier>ISSN:2335-3112</dc:identifier><dc:identifier>COBISSID_HOST:73225219</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-I8EV3HXF</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Biotehniška fakulteta, Oddelek za gozdarstvo in obnovljive gozdne vire</dc:publisher><dc:publisher xml:lang="sl">Biotehniška fakulteta, Oddelek za lesarstvo</dc:publisher><dc:publisher xml:lang="sl">Gozdarski inštitut Slovenije, založba Silvae Slovenica</dc:publisher><dcterms:isPartOf xml:lang="sl">Acta silvae et ligni</dcterms:isPartOf><dc:subject xml:lang="en">artificial surface</dc:subject><dc:subject xml:lang="en">forest cover</dc:subject><dc:subject xml:lang="en">forest fragmentation</dc:subject><dc:subject xml:lang="sl">fragmentiranost gozda</dc:subject><dc:subject xml:lang="sl">gozdnatost</dc:subject><dc:subject xml:lang="en">heat island</dc:subject><dc:subject xml:lang="sl">toplotni otok</dc:subject><dc:subject xml:lang="sl">umetne površine</dc:subject><dcterms:temporal rdf:resource="2013-2025" /><dc:title xml:lang="sl">The influence of land use on the spatial distribution and intensity of heat islands in Slovenia| Vpliv rabe tal na prostorsko razporeditev in intenzivnost toplotnih otokov v Sloveniji|</dc:title><dc:description xml:lang="sl">Heat islands (HI) are a common anthropogenic phenomenon and are defined as artificial surfaces (urban areas) that have a higher average temperature than their surroundings (rural areas). The aim of this work was to determine the influence of land use on the spatial distribution and intensity (HIi ) of HI in Slovenia. The MODIS Land Surface Temperature (LST) and Corine Land Cover (CLC) databases were used to perform the analysis. Within the identified HI, two HI levels were determined based on temperature difference. The results revealed a statistically significant negative correlation between HIi and both forest co%ver and forest fragmentation (forest edge density and ratio of mean forest patch size to HI size). Artificial surface was positively correlated with HIi . The results contribute to the understanding of the spatial distribution of HI and HIi and provide informati%on for spatial planning and policy-making to reduce the negative impact of HI</dc:description><dc:description xml:lang="sl">Heat islands (HI) are a common anthropogenic phenomenon and are defined as artificial surfaces (urban areas) that have a higher average temperature than their surroundings (rural areas). The aim of this work was to determine the influence of land use on the spatial distribution and intensity (HIi ) of HI in Slovenia. The MODIS Land Surface Temperature (LST) and Corine Land Cover (CLC) databases were used to perform the analysis. Within the identified HI, two HI levels were determined based on temperature difference. The results revealed a statistically significant negative correlation between HIi and both forest co%ver and forest fragmentation (forest edge density and ratio of mean forest patch size to HI size). Artificial surface was positively correlated with HIi . The results contribute to the understanding of the spatial distribution of HI and HIi and provide information for spatial planning and policy-making to reduce the negative impact of HI</dc:description><edm:type>TEXT</edm:type><dc:type xml:lang="sl">znanstveno časopisje</dc:type><dc:type xml:lang="en">journals</dc:type><dc:type rdf:resource="http://www.wikidata.org/entity/Q361785" /></edm:ProvidedCHO><ore:Aggregation rdf:about="http://www.dlib.si/?URN=URN:NBN:SI:doc-I8EV3HXF"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-I8EV3HXF" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-I8EV3HXF/b8057561-efb2-4bb8-b19c-75f04e346c4c/PDF" /><edm:rights rdf:resource="http://creativecommons.org/licenses/by-sa/4.0/" /><edm:provider>Slovenian National E-content Aggregator</edm:provider><edm:intermediateProvider xml:lang="en">National and University Library of Slovenia</edm:intermediateProvider><edm:dataProvider xml:lang="sl">Gozdarski inštitut Slovenije</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-I8EV3HXF/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-I8EV3HXF" /></ore:Aggregation></rdf:RDF>