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                <identifier>ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai:2:6960</identifier>
                <datestamp>2019-05-28T05:13:17Z</datestamp>
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                    <dim:field mdschema="dc" element="title" lang="en">Karst groundwater budget and discharge regime of Banja Spring near Petnica</dim:field>
                    <dim:field mdschema="dc" element="date" qualifier="issued">2015</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="udc">911.2:551.444(497.11)</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">http://ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai/record/2/6960</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">http://www.gi.sanu.ac.rs/site/index.php/en/publishing/journal/122-collection-of-papers-volume-65-1</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:26989" confidence="-1">V. Ristić Vakanjac</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:26990" confidence="-1">P. Papić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:26991" confidence="-1">R. Golubović</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="etfid:888" confidence="-1">B. Vakanjac</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:26993" confidence="-1">M. Čokorilo Ilić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:26994" confidence="-1">M. Jokić</dim:field>
                    <dim:field mdschema="dc" element="description" qualifier="abstract">Detailed hydrological and hydrogeological assessments of karst spring discharge
require information about the groundwater regime in the study area/watershed. However,
groundwater regime monitoring is often organized locally and sporadically, as required for specific
studies or projects, and seldom lasts longer than one year. On the other hand, if time series of
quantitative parameters are shorter than 15 years, the watershed is considered to be ungauged. As a
result, discharge regime and karst aquifer budget assessments of ungauged watersheds can be
misleading. To minimize water budget assessment errors, available time series need to be extended
as far as possible. Regression models are commonly used to extend, simulate or fill gaps in
existing time series. The paper presents an application of multiple linear regression to extend the
existing time series of mean monthly discharges of Banja Spring (at Petnica, western Serbia), in
order to cover the entire study period (1960-2006).</dim:field>
                    <dim:field mdschema="dc" element="type">article</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="doi">10.2298/IJGI1501019R</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="volume">65/1</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="spage">19</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="epage">32</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="issn">0350-7599</dim:field>
                    <dim:field mdschema="dc" element="source">Journal of Geographical Institute &amp;quot;Jovan Cvijic&amp;quot;</dim:field>
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