{"?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-YADFNJRA/63f70f19-ca23-453c-8c50-6ec13c5350d6/PDF","dcterms:extent":"752 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:DOC-YADFNJRA/3e27cea7-17b1-416c-91db-39450aa80e89/TEXT","dcterms:extent":"55 KB"}],"edm:TimeSpan":{"@rdf:about":"2009-2026","edm:begin":{"@xml:lang":"en","#text":"2009"},"edm:end":{"@xml:lang":"en","#text":"2026"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:DOC-YADFNJRA","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-THPLMJH3"},{"@xml:lang":"sl","#text":"Economic and business review"}],"dcterms:issued":"2009","dc:creator":"Kajfež-Bogataj, Lučka","dc:format":[{"@xml:lang":"sl","#text":"številka:1"},{"@xml:lang":"sl","#text":"letnik:11"},{"@xml:lang":"sl","#text":"str. 9-27"}],"dc:identifier":["ISSN:1580-0466","COBISSID:18486758","URN:URN:NBN:SI:doc-YADFNJRA"],"dc:language":"en","dc:publisher":{"@xml:lang":"sl","#text":"Ekonomska fakulteta"},"dc:subject":[{"@xml:lang":"sl","#text":"antropogeni vplivi"},{"@xml:lang":"sl","#text":"Evropa"},{"@xml:lang":"sl","#text":"globalno ogrevanje"},{"@xml:lang":"sl","#text":"klimatske spremembe"},{"@xml:lang":"sl","#text":"podnebje"}],"dcterms:temporal":{"@rdf:resource":"2009-2026"},"dc:title":{"@xml:lang":"sl","#text":"Climate change and future adaptation|"},"dc:description":[{"@xml:lang":"sl","#text":"This paper provides a summary of the current scientific understanding of the International Panel on Climate Change (IPCC) on the natural and anthropogenic drivers of changes in global climate. It presents an overview of observed changes in the climate system and their relationships with physical processes as well as an overview of projections for future climate changes. A summary of observed climate changes in Slovenia in the last decades is given and future projections are discussed. Europe has warmed by almost 1°C in the last century, faster than the global average. Precipitation has significantly increased in northern Europe, whereas drying has been observed in the Mediterranean. Continuing the observed trend, average precipitation as well as extreme precipitation are very likely to further increase in most of northern Europe whereas precipitation is very likely to decrease in the Mediterranean. The reduction of precipitation in summer in Slovenia is expected to have serious effects, e.g. more frequent droughts, with considerable impacts on horticulture and the availability of water. Adaptationcan reduce vulnerability to climate variability and change. This paper also discusses the appropriate responses to climate change from the mitigation and adaptation points of view"},{"@xml:lang":"sl","#text":"Članek prinaša povzetek dosedanjih znanstvenih spoznanj Medvladnega odbora za podnebne spremembe (IPCC) o naravnih in antropogenih dejavnikih globalnih podnebnih sprememb. Ponuja pregled opazovanih sprememb v podnebnem sistemu in njihove povezave s fizičnimi procesi, poleg tega pa tudi pregled projekcij bodočih podnebnih sprememb. Članek vsebuje tudi povzetek opazovanih podnebnih sprememb v Sloveniji v zadnjih desetletjih in obravnava bodoče projekcije. Evropa se je v zadnjem stoletju segrela za skorajda 1°C, kar je hitreje od globalnega povprečja. V severni Evropi se je pomembno povečala količina padavin, medtem ko je v Sredozemlju opažen trend izsušitev. Ob nadaljevanju takšnega trenda obstaja velika verjetnost, da bo v velikem delu severne Evrope prišlo še do nadaljnjega naraščanja povprečne količine padavin ter števila ekstremnih padavin, medtem ko se bo v Sredozemlju količina padavin po vsej verjetnosti zmanjšala. V Sloveniji bo zmanjšanje količine padavin v poletnih mesecih imelo resne posledice, npr. bolj pogoste suše z znatnimi vplivi na hortikulturo in razpoložljivost vodnih virov. Prilagajanje lahko zmanjša ranljivost zaradi podnebne spremenljivosti in podnebnih sprememb. Članek razčlenjuje tudi ustrezne odzive na podnebne spremembe s stališča ublažitve posledic ter prilagajanja"}],"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-YADFNJRA","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:DOC-YADFNJRA"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:DOC-YADFNJRA/63f70f19-ca23-453c-8c50-6ec13c5350d6/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by-nc-nd/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, Ekonomska fakulteta"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:DOC-YADFNJRA/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:DOC-YADFNJRA"}}}}