<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-P7RLY3AW</identifier><date>2015</date><creator>Ivajnšič, Danijel</creator><creator>Kaligarič, Mitja</creator><relation>documents/doc/P/URN_NBN_SI_doc-P7RLY3AW_001.pdf</relation><relation>documents/doc/P/URN_NBN_SI_doc-P7RLY3AW_001.txt</relation><format format_type="issue">2</format><format format_type="volume">25</format><format format_type="type">article</format><format format_type="extent">str. 173-182</format><identifier identifier_type="ISSN">1408-533X</identifier><identifier identifier_type="COBISSID">21938952</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-P7RLY3AW</identifier><language>eng</language><publisher>Societá storica del Litorale</publisher><publisher>Zgodovinsko društvo za južno Primorsko</publisher><source>Annales. Series historia naturalis</source><rights>BY-NC</rights><subject language_type_id="slv">evapotranspiracija</subject><subject language_type_id="slv">klasični Kras</subject><subject language_type_id="slv">krajinske spremembe</subject><subject language_type_id="slv">raba tal</subject><title>Can evapotranspiration be considered an additional indicator for understanding the changed landscape identity of the classic Karst?</title></Record>