<?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-7NIP4YAL/5cc11706-b925-4e75-8fd3-ea60f809cbe9/PDF"><dcterms:extent>2694 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-7NIP4YAL/5ce5c477-d952-4c77-93e2-4be5059caffc/TEXT"><dcterms:extent>41 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1985-2025"><edm:begin xml:lang="en">1985</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-7NIP4YAL"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-U694A0TC" /><dcterms:issued>2019</dcterms:issued><dc:creator>Kácovská, Karolina</dc:creator><dc:creator>Ogrin, Darko</dc:creator><dc:creator>Vysoudil, Miroslav</dc:creator><dc:format xml:lang="sl">številka:51</dc:format><dc:format xml:lang="sl">str. 111-134</dc:format><dc:identifier>ISSN:0354-0596</dc:identifier><dc:identifier>COBISSID_HOST:70712674</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-7NIP4YAL</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Znanstvena založba Filozofske fakultete</dc:publisher><dcterms:isPartOf xml:lang="sl">Dela - Oddelek za geografijo Filozofske fakultete v Ljubljani</dcterms:isPartOf><dc:subject xml:lang="en">climatogeography</dc:subject><dc:subject xml:lang="en">Czech Republic</dc:subject><dc:subject xml:lang="sl">Češka</dc:subject><dc:subject xml:lang="en">hand-held thermal camera</dc:subject><dc:subject xml:lang="sl">klimatogeografija</dc:subject><dc:subject xml:lang="en">land cover-type</dc:subject><dc:subject xml:lang="sl">prenosna termalna kamera</dc:subject><dc:subject xml:lang="en">Slovenia</dc:subject><dc:subject xml:lang="sl">Slovenija</dc:subject><dc:subject xml:lang="en">surface temperature</dc:subject><dc:subject xml:lang="sl">temperatura</dc:subject><dc:subject xml:lang="sl">tipi pokrovnosti</dc:subject><dcterms:temporal rdf:resource="1985-2025" /><dc:title xml:lang="sl">Comparison of thermal behaviour of different land cover types in Slovenia and Czech Republic|</dc:title><dc:description xml:lang="sl">Th is paper presents the results of a study of thermal behaviour of diff erent land co-ver types in the Czech Republic and Slovenia. A hand-held thermal camera, Fluke Ti55, was used for data collection. Variation in the values of the surface temperature characteristics refl ects the geographically dissimilar spaces. Th e investigation demonstrated impact of dense green vegetation and water bodies on the balanced thermal behaviour of landscapes in both countries. Th us, they appear to be cold spots with the lowest values. Th e most obvious variation in surface temperature is associated with artifi cial areas and bare surfaces. Th ey usually represent hot spots in the landscape. In both countries similar thermal behaviour was found in artifi cial land cover types as opposed to agricultural land cover types</dc:description><dc:description xml:lang="sl">Prispevek predstavlja rezultate proučevanja toplotnega odziva različnih tipov pokrovnosti v Republiki Češki in Sloveniji. Podatki so pridobljeni s pomočjo prenosne termalne kamere "Fluke Ti 55". Velike razlike v temperaturi površja so posledica različnih geografskih razmer na Češkem in v Sloveniji. Raziskava je pokazala, da imajo v obeh državah gosto poraščene (gozd) in vodne (vlažne) površine uravnovešen toplotni odziv in v pokrajini običajno izstopajo kot hladne točke. Nasprotni temu so antropogeni tipi rabe tal in golo, neporaščeno površje, ki izkazujejo največjo temperaturno variabilnost in v pokrajini izstopajo kot vroče točke. V obeh državah je bil toplotni odziv antropogenih tipov rabe tal podoben, medtem ko se je najbolj razlikoval pri kmetijskih površinah</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-7NIP4YAL"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-7NIP4YAL" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-7NIP4YAL/5cc11706-b925-4e75-8fd3-ea60f809cbe9/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">Univerza v Ljubljani, Filozofska fakulteta</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-7NIP4YAL/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-7NIP4YAL" /></ore:Aggregation></rdf:RDF>