2021
DOI: 10.1007/978-3-030-90055-7_35
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Assessment of Regional Analyses Methods for Spatial Interpolation of Flood Quantiles in the Basins of Bosnia and Herzegovina and Serbia

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Cited by 3 publications
(4 citation statements)
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“…Due to input data issues (e.g., data gaps), the use of LP3 with the expected moments algorithm (EMA) should be reconsidered [11]. Overall better Q100 estimates were achieved in previous research [33] conducted using the Hydrologic Engineering Center's Statistical Software Package (HEC-SSP) where EMA is installed. In addition to the 53 HSs here, more HSs were included, and a study area comprising 74 HSs was delineated in the three regions.…”
Section: Discussionmentioning
confidence: 99%
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“…Due to input data issues (e.g., data gaps), the use of LP3 with the expected moments algorithm (EMA) should be reconsidered [11]. Overall better Q100 estimates were achieved in previous research [33] conducted using the Hydrologic Engineering Center's Statistical Software Package (HEC-SSP) where EMA is installed. In addition to the 53 HSs here, more HSs were included, and a study area comprising 74 HSs was delineated in the three regions.…”
Section: Discussionmentioning
confidence: 99%
“…In the study area for this research, i.e., Bosnia and Herzegovina, specific runoff diagrams or regression that relates flood quantiles and catchment area are most often used for flood quantile estimation in ungauged catchments [32]. It was shown that this approach can give significant under-/overestimation of flood quantiles and that geographically continuous regions of water basins are considered homogeneous regions without testing [33,34]. Other methods for flood data transfer used to improve flood quantile estimation included an extension of the gauged peak flow data based on gauged water stage, assumed rating curves [35], and historic floods [36].…”
Section: Introductionmentioning
confidence: 99%
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“…Estimates of extreme rainfall are often derived from analyses of long-term rain gauge data. Due to the scarcity of rain gauges in many parts of the world, an interpolation approach is often used to provide a spatial map for the predicted frequency [26]. However, the sparse spatial density of rain gauges has a substantial impact on the dependability of estimations of extreme rainfall.…”
Section: Introductionmentioning
confidence: 99%