{"?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-ZWGIYG7U/a1424a5a-55a9-44b4-a9da-68f3eb949570/PDF","dcterms:extent":"10530 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-ZWGIYG7U/5afbb867-a4dc-4701-8210-81d8bd21513c/TEXT","dcterms:extent":"44 KB"}],"edm:TimeSpan":{"@rdf:about":"2003-2025","edm:begin":{"@xml:lang":"en","#text":"2003"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-ZWGIYG7U","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-EEHMIXWQ"},{"@xml:lang":"sl","#text":"Acta geographica Slovenica"}],"dcterms:issued":"2022","dc:creator":["Jelovčan, Mateja","Šraj, Mojca"],"dc:format":[{"@xml:lang":"sl","#text":"številka:1"},{"@xml:lang":"sl","#text":"letnik:62"},{"@xml:lang":"sl","#text":"str. 37-53"}],"dc:identifier":["DOI:10.3986/AGS.9399","COBISSID_HOST:112460291","ISSN:1581-6613","URN:URN:NBN:SI:doc-ZWGIYG7U"],"dc:language":"en","dc:publisher":[{"@xml:lang":"sl","#text":"Geografski inštitut Antona Melika ZRC SAZU"},{"@xml:lang":"sl","#text":"Slovenska akademija znanosti in umetnosti"},{"@xml:lang":"sl","#text":"Založba ZRC"}],"dc:subject":[{"@xml:lang":"sl","#text":"analiza nizkih pretokov"},{"@xml:lang":"en","#text":"lfstat package"},{"@xml:lang":"en","#text":"low-flow analysis"},{"@xml:lang":"sl","#text":"paket lfstat"},{"@xml:lang":"sl","#text":"reka Vipava"},{"@xml:lang":"en","#text":"Slovenia"},{"@xml:lang":"sl","#text":"Slovenija"},{"@xml:lang":"en","#text":"Vipava River"},{"@xml:lang":"en","#text":"Vipava Valley"},{"@xml:lang":"sl","#text":"Vipavska dolina"}],"dcterms:temporal":{"@rdf:resource":"2003-2025"},"dc:title":{"@xml:lang":"sl","#text":"Comprehensive low-flow analysis of the Vipava river|"},"dc:description":[{"@xml:lang":"sl","#text":"he article presents the results of the analysis of low flows at 5 gauging stations on the Vipava River, which has a Dinaric pluvial-nival regime (catchment area of 590 km2). The low-flow statistics show that the gauging station Vipava stands out with the lowest values. Baseflow index (BFI) values are comparable among the considered stations and are around 0.40. Relatively low BFI values indicate low soil permeability. A high similarity between the mean annual minimum 7-day flow (MAM7) and the 95th percentile exceedance discharge (Q95) at all gauging stations indicates a temperate climate. The highest flows values occur in spring and autumn, and the lowest in summer. In wet years there are relatively large fluctuations in flow, while in dry years the flow consists mainly of baseflow. This is also confirmed with the flow duration curves analysis. The seasonality analysis shows a predominant summer regime with low flows"},{"@xml:lang":"sl","#text":"V članku so predstavljeni rezultati analize nizkih pretokov na 5 vodomernih postajah na reki Vipavi, kiima dinarski dežno-snežni režim (površina zaledja 590km2). Rezultati statistik nizkih pretokov kažejo,da z najnižjimi vrednostmi izstopa vodomerna postaja Vipava. Vrednosti indeksa baznega odtoka (BFI)so med obravnavanimi postajami primerljive in se gibljejo okoli 0,40. Relativno nizke vrednosti BFI kaže-jo na nizko prepustnost tal. Velika podobnost med srednjim letnim 7-dnevnim minimalnim pretokom(MAM7) in 95-odstotnim pretokom (Q95)na vseh vodomernih postajah kaže na zmerno podnebje. Največjevrednosti pretokov se pojavijo spomladi in jeseni, najnižje pa poleti. Za mokra leta so značilna relativnovelika nihanja pretoka, v sušnih letih pa pretok predstavlja predvsem bazni odtok. To potrjuje tudi anal-iza krivulj trajanja pretokov. Analiza sezonskosti kaže prevladujoč poletni režim nizkih pretokov"}],"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-ZWGIYG7U","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-ZWGIYG7U"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-ZWGIYG7U/a1424a5a-55a9-44b4-a9da-68f3eb949570/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":"ZRC SAZU"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-ZWGIYG7U/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-ZWGIYG7U"}}}}