{"?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-IHCD5VAQ/d5fb7907-336f-4691-9752-b51093347970/PDF","dcterms:extent":"7427 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-IHCD5VAQ/0099714d-d55d-4c8d-a593-50010b63e28e/TEXT","dcterms:extent":"65 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-IHCD5VAQ/0306e58b-e5a7-4695-a364-a375a27b772e/PDF","dcterms:extent":"7042 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-IHCD5VAQ/4f055946-3d3b-4ad1-a4b6-85df8ec1c0c8/TEXT","dcterms:extent":"68 KB"}],"edm:TimeSpan":{"@rdf:about":"1985-2025","edm:begin":{"@xml:lang":"en","#text":"1985"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-IHCD5VAQ","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-U694A0TC"},{"@xml:lang":"sl","#text":"Dela - Oddelek za geografijo Filozofske fakultete v Ljubljani"}],"dcterms:issued":"2023","dc:creator":["Miklič, Stanka","Trobec, Tajan"],"dc:format":[{"@xml:lang":"sl","#text":"številka:59"},{"@xml:lang":"sl","#text":"str. 91-150"}],"dc:identifier":["ISSN:0354-0596","DOI:10.4312/dela.59.91-150","COBISSID_HOST:181283075","URN:URN:NBN:SI:doc-IHCD5VAQ"],"dc:language":["en","sl"],"dc:publisher":{"@xml:lang":"sl","#text":"Založba Univerze v Ljubljani"},"dc:subject":[{"@xml:lang":"sl","#text":"Cerkniško jezero"},{"@xml:lang":"en","#text":"climate change"},{"@xml:lang":"sl","#text":"hidrogeografija"},{"@xml:lang":"en","#text":"hydrogeography"},{"@xml:lang":"sl","#text":"jezera"},{"@xml:lang":"en","#text":"lake water regime"},{"@xml:lang":"en","#text":"lakes"},{"@xml:lang":"sl","#text":"podnebne spremembe"},{"@xml:lang":"en","#text":"Slovenia"},{"@xml:lang":"sl","#text":"Slovenija"}],"dcterms:temporal":{"@rdf:resource":"1985-2025"},"dc:title":{"@xml:lang":"sl","#text":"Sezonske spremembe gladine Cerkniškega jezera v obdobju 1961–2020| Seasonal changes in the Cerknica Lake level during the period 1961–2020|"},"dc:description":[{"@xml:lang":"sl","#text":"In this article, we analyse the annual changes in the minimum (Hnp), mean (Hs) and maximum (Hvp) water levels of Cerknica Lake in the period 1961–2020 and try to relate them to changes in the local climate. Lower precipitation, higher temperatures and the resulting higher evaporation as well as a reduced influence of snow retention are reflected in the changing discharge from the lake basin, which is a cause of a decrease in annual, spring and summer Hs and Hvp, while winter and fall Hs and Hvp have remained at a similar level. On the other hand, Hnp increases, except in spring, which is on an annual basis, in summer and fall (as far as the unreliability of data at the lowest water levels allows) probably due to artificial retention of water in the lake, and in winter and spring due to climate change"},{"@xml:lang":"sl","#text":"V prispevku analiziramo letne spremembe najnižjih (Hnp), srednjih (Hs) in najvišjih (Hvp) letnih vodostajev Cerkniškega jezera v obdobju 1961–2020 ter jih skušamo povezati s spremembami lokalnega podnebja. Manjša količina padavin, višja temperatura in posledično večje izhlapevanje ter manjši vpliv snežnega zadržka se odražajo v spremenjenem odtoku s pojezerja, kar se zrcali v upadu letnih, pomladnih in poletnih Hs in Hvp, medtem ko so zimski in jesenski Hs in Hvp ostali na podobni ravni. Po drugi strani so Hnp razen pomladi v porastu, kar na letni ravni, poleti in jeseni (kolikor to dopušča nezanesljivost podatkov ob najnižjih vodostajih) verjetno lahko pripišemo umetnemu zadrževanja vode v jezeru, pozimi in pomladi pa podnebnim spremembam"}],"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-IHCD5VAQ","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-IHCD5VAQ"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-IHCD5VAQ/d5fb7907-336f-4691-9752-b51093347970/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by-sa/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 Ljubljani, Filozofska fakulteta"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-IHCD5VAQ/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-IHCD5VAQ"}}}}