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dc.creatorUrošev, Marko
dc.creatorŠtrbac, Dragoljub
dc.creatorKovačević-Majkić, Jelena
dc.creatorPlavšić, Jasna
dc.creatorYamashkin, Stanislav
dc.date.accessioned2021-01-19T08:09:45Z
dc.date.available2021-01-19T08:09:45Z
dc.date.issued2020
dc.identifier.issn0350-7599
dc.identifier.urihttps://grafar.grf.bg.ac.rs/handle/123456789/2229
dc.description.abstractOne of the indicators of water potential and water resources is specific runoff. Specific runoff for the whole territory of Serbia was obtained using the exponential relation between depth of runoff Y (mm) and precipitation P (mm). This relation is obtained on the basis of the mean annual amount of precipitation and annual water discharge, namely the depth of the runoff for 69 basins for the period 1961–2010. Coefficient of determination (R²) of relation between the depth of runoff and precipitation is 0.72. The differences between measured and modeled values of specific runoff vary from basin to basin, but at the level of the whole Serbia it is 3.5%. More precisely, the measured specific runoff amounts 5.6 l/s/km2, and the modeled specific runoff is 5.7 l/s/km2. The verification was done by applying the model to 11 large river basins in Serbia. Spatial distribution of the modeled specific runoff is presented by a digital map of specific runoff with pixel resolution 100 × 100 m which enables the estimation of mean annual water discharge in any ungauged basin in Serbia.sr
dc.language.isoensr
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/47007/RS//
dc.rightsopenAccesssr
dc.sourceJ. Geogr. Inst. Cvijic.sr
dc.titleSpatial distribution of specific runoff in Serbia based on rainfall-runoff relationshipsr
dc.typearticlesr
dc.rights.licenseARRsr
dc.citation.epage214
dc.citation.rankM24~
dc.citation.spage203
dc.citation.volume70
dc.identifier.doi10.2298/IJGI2003203U
dc.identifier.fulltexthttp://grafar.grf.bg.ac.rs/bitstream/id/8925/bitstream_8925.pdf
dc.type.versionpublishedVersionsr


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