Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin

In the present study, we have assessed low-flow discharge deficits, and the characteristics of the low flows at a constant and variable (monthly) low-flow threshold. The low-flow truncation level was identified based on the 70th percentile from the flow duration curve (Q70%). Q95% was assumed to be...

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Main Author: Edmund Tomaszewski
Format: Article
Language:English
Published: Publishing House of the University of Agriculture in Krakow 2018-09-01
Series:Acta Scientiarum Polonorum. Formatio Circumiectus
Subjects:
Online Access:http://www.formatiocircumiectus.actapol.net/pub/17_3_205.pdf
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author Edmund Tomaszewski
author_facet Edmund Tomaszewski
author_sort Edmund Tomaszewski
collection DOAJ
description In the present study, we have assessed low-flow discharge deficits, and the characteristics of the low flows at a constant and variable (monthly) low-flow threshold. The low-flow truncation level was identified based on the 70th percentile from the flow duration curve (Q70%). Q95% was assumed to be the threshold for the deep low-flow discharge. Thirteen catchments in the Vistula basin, varying in size, river regime, and physico-geographical conditions, were selected for the study. The input data was a series of daily discharge data sets from the period 1951–2016, made available by IMGW-PIB (Polish Institute of Meteorology and Water Management – National Research Institute). Analyses were conducted of drought flow discharge deficit volume in absolute and relative values, and low-flow duration and deficits contributing to severe low-flows were calculated for temporal scales of months and years. Comparison of the obtained results led us to the determination of the basic factors affecting the formation of low-flow deficits, and the indication of restrictions when applying fixed and variable criteria for identifying river low-flows.
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spelling doaj.art-181fcb6908b14f5cb8829df38959158a2022-12-21T18:22:46ZengPublishing House of the University of Agriculture in KrakowActa Scientiarum Polonorum. Formatio Circumiectus1644-07652018-09-0117320521610.15576/ASP.FC/2018.17.3.205Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basinEdmund Tomaszewski0Faculty of Geographical Sciences, University of ŁódźIn the present study, we have assessed low-flow discharge deficits, and the characteristics of the low flows at a constant and variable (monthly) low-flow threshold. The low-flow truncation level was identified based on the 70th percentile from the flow duration curve (Q70%). Q95% was assumed to be the threshold for the deep low-flow discharge. Thirteen catchments in the Vistula basin, varying in size, river regime, and physico-geographical conditions, were selected for the study. The input data was a series of daily discharge data sets from the period 1951–2016, made available by IMGW-PIB (Polish Institute of Meteorology and Water Management – National Research Institute). Analyses were conducted of drought flow discharge deficit volume in absolute and relative values, and low-flow duration and deficits contributing to severe low-flows were calculated for temporal scales of months and years. Comparison of the obtained results led us to the determination of the basic factors affecting the formation of low-flow deficits, and the indication of restrictions when applying fixed and variable criteria for identifying river low-flows.http://www.formatiocircumiectus.actapol.net/pub/17_3_205.pdflow-flow regimelow-flow threshold levelhydrological droughtthe Vistula river basin
spellingShingle Edmund Tomaszewski
Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
Acta Scientiarum Polonorum. Formatio Circumiectus
low-flow regime
low-flow threshold level
hydrological drought
the Vistula river basin
title Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
title_full Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
title_fullStr Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
title_full_unstemmed Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
title_short Low-flow discharge deficits assessment, applying constant and variable low-flow threshold levels, as illustrated with the example of selected catchments in the Vistula river basin
title_sort low flow discharge deficits assessment applying constant and variable low flow threshold levels as illustrated with the example of selected catchments in the vistula river basin
topic low-flow regime
low-flow threshold level
hydrological drought
the Vistula river basin
url http://www.formatiocircumiectus.actapol.net/pub/17_3_205.pdf
work_keys_str_mv AT edmundtomaszewski lowflowdischargedeficitsassessmentapplyingconstantandvariablelowflowthresholdlevelsasillustratedwiththeexampleofselectedcatchmentsinthevistulariverbasin