2015
DOI: 10.1590/1809-4430-eng.agric.v35n5p808-816/2015
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Low-flow estimates in regions of extrapolation of the regionalization equations: a new concept

Abstract: Knowledge of natural water availability, which is characterized by low flows, is essential for planning and management of water resources. One of the most widely used hydrological techniques to determine streamflow is regionalization, but the extrapolation of regionalization equations beyond the limits of sample data is not recommended. This paper proposes a new method for reducing overestimation errors associated with the extrapolation of regionalization equations for low flows. The method is based on the use… Show more

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Cited by 13 publications
(9 citation statements)
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“…Similar results were found for low flows in RODRIGUEZ (2008), PRUSKI et al (2012) and PRUSKI et al (2015). Although the qlt and C values tend to increase toward the headwaters, there is no guarantee that this trend of growth is as pronounced as that represented in the graphs of C versus drainage area (Figure 2) and in the qlt variation rate expressed by equation 6.…”
Section: Resultssupporting
confidence: 76%
See 1 more Smart Citation
“…Similar results were found for low flows in RODRIGUEZ (2008), PRUSKI et al (2012) and PRUSKI et al (2015). Although the qlt and C values tend to increase toward the headwaters, there is no guarantee that this trend of growth is as pronounced as that represented in the graphs of C versus drainage area (Figure 2) and in the qlt variation rate expressed by equation 6.…”
Section: Resultssupporting
confidence: 76%
“…Although there are no similar studies available for the long-term average flow, equivalent results were observed by PRUSKI et al (2015) when analyzing the performance for low flows. These authors showed that it was necessary to adjust 88% of the total Urucuia basin (a sub-basin of São Francisco basin) area using a threshold value.…”
Section: Resultsmentioning
confidence: 62%
“…This technique is a downscale of discharge for drainage areas smaller than the available measurements, using empirical equations based on independent variables like area upstream or average precipitation upstream. These authors tested several empirical relationships, and the best skill low streamflow regionalization was obtained by basin-specific regression equations of Q 90 against the upstream long-term annual rainfall minus an initial abstraction of 750 mm (P eq750 = P − 750) as independent variable [29]. Figure 11 plots 80% of long-term Q 90 (the maximum discharge that could be granted for all human use, including irrigation).…”
Section: Regionmentioning
confidence: 99%
“…Whereas there exist sites under long-term observation (so that low flow characteristics can be estimated with the use of direct -statistical methods) still, in many cases streamflow information is not available or is insufficient in terms of quality and quantity (Pruski et al, 2015;Arai et al, 2012). A lot of effort was made to establish low flow procedures and to evaluate methods for the estimation of low flow parameters at ungauged sites (Schreiber and Demuth, 1997).…”
Section: Introductionmentioning
confidence: 99%