Spatial distribution of specific runoff in Serbia based on rainfall-runoff relationship

Marko Urosev, D. Štrbac, Jelena Kovačević-Majkić, J. Plavšić, S. Yamashkin
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引用次数: 1

Abstract

One 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 (R?) 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.
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基于降雨-径流关系的塞尔维亚特定径流空间分布
具体径流量是水势和水资源的指标之一。利用径流深度Y (mm)与降水量P (mm)之间的指数关系,获得了塞尔维亚全境的具体径流量。这一关系是基于1961-2010年69个流域年平均降水量与年径流量(即径流深度)的关系得出的。径流深度与降水关系的决定系数R为0.72。具体径流量的测量值与模拟值之间的差异因流域而异,但在整个塞尔维亚的水平上,这一差异为3.5%。更精确地说,实测的比径流量为5.6 l/s/km2,模拟的比径流量为5.7 l/s/km2。将该模型应用于塞尔维亚的11个大河流域进行了验证。模拟的特定径流的空间分布由特定径流的数字地图呈现,像素分辨率为100 ?100米,可以估计塞尔维亚任何未测量盆地的年平均水量。
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来源期刊
CiteScore
2.00
自引率
16.70%
发文量
16
审稿时长
12 weeks
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