Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters

In the context of the ongoing climate warming in Europe, the seasonality and magnitudes of low flows and streamflow droughts are expected to change in the future. Increasing temperature and evaporation rates, stagnating precipitation amounts and decreasing snow cover will probably further intensify...

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Main Authors: Vojtech Vlach, Ondrej Ledvinka, Milada Matouskova
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/12/3575
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spelling doaj-076a5d7d8bcd4973b6a64bc59bab7a412020-12-21T00:00:03ZengMDPI AGWater2073-44412020-12-01123575357510.3390/w12123575Changing Low Flow and Streamflow Drought Seasonality in Central European HeadwatersVojtech Vlach0Ondrej Ledvinka1Milada Matouskova2Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech RepublicCzech Hydrometeorological Institute, Hydrology Database and Water Budget Department, Na Sabatce 2050/17, 143 06 Prague 412, Czech RepublicDepartment of Physical Geography and Geoecology, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech RepublicIn the context of the ongoing climate warming in Europe, the seasonality and magnitudes of low flows and streamflow droughts are expected to change in the future. Increasing temperature and evaporation rates, stagnating precipitation amounts and decreasing snow cover will probably further intensify the summer streamflow deficits. This study analyzed the long-term variability and seasonality of low flows and streamflow droughts in fifteen headwater catchments of three regions within Central Europe. To quantify the changes in the low flow regime of selected catchments during the 1968–2019 period, we applied the R package lfstat for computing the seasonality ratio (SR), the seasonality index (SI), mean annual minima, as well as for the detection of streamflow drought events along with deficit volumes. Trend analysis of summer minimum discharges was performed using the Mann–Kendall test. Our results showed a substantial increase in the proportion of summer low flows during the analyzed period, accompanied with an apparent shift in the average date of low flow occurrence towards the start of the year. The most pronounced seasonality shifts were found predominantly in catchments with the mean altitude 800–1000 m.a.s.l. in all study regions. In contrast, the regime of low flows in catchments with terrain above 1000 m.a.s.l. remained nearly stable throughout the 1968–2019 period. Moreover, the analysis of mean summer minimum discharges indicated a much-diversified pattern in behavior of long-term trends than it might have been expected. The findings of this study may help identify the potentially most vulnerable near-natural headwater catchments facing worsening summer water scarcity.https://www.mdpi.com/2073-4441/12/12/3575low flowsstreamflow droughtminimum dischargesheadwaterseasonalitytrends
collection DOAJ
language English
format Article
sources DOAJ
author Vojtech Vlach
Ondrej Ledvinka
Milada Matouskova
spellingShingle Vojtech Vlach
Ondrej Ledvinka
Milada Matouskova
Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
Water
low flows
streamflow drought
minimum discharges
headwater
seasonality
trends
author_facet Vojtech Vlach
Ondrej Ledvinka
Milada Matouskova
author_sort Vojtech Vlach
title Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
title_short Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
title_full Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
title_fullStr Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
title_full_unstemmed Changing Low Flow and Streamflow Drought Seasonality in Central European Headwaters
title_sort changing low flow and streamflow drought seasonality in central european headwaters
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-12-01
description In the context of the ongoing climate warming in Europe, the seasonality and magnitudes of low flows and streamflow droughts are expected to change in the future. Increasing temperature and evaporation rates, stagnating precipitation amounts and decreasing snow cover will probably further intensify the summer streamflow deficits. This study analyzed the long-term variability and seasonality of low flows and streamflow droughts in fifteen headwater catchments of three regions within Central Europe. To quantify the changes in the low flow regime of selected catchments during the 1968–2019 period, we applied the R package lfstat for computing the seasonality ratio (SR), the seasonality index (SI), mean annual minima, as well as for the detection of streamflow drought events along with deficit volumes. Trend analysis of summer minimum discharges was performed using the Mann–Kendall test. Our results showed a substantial increase in the proportion of summer low flows during the analyzed period, accompanied with an apparent shift in the average date of low flow occurrence towards the start of the year. The most pronounced seasonality shifts were found predominantly in catchments with the mean altitude 800–1000 m.a.s.l. in all study regions. In contrast, the regime of low flows in catchments with terrain above 1000 m.a.s.l. remained nearly stable throughout the 1968–2019 period. Moreover, the analysis of mean summer minimum discharges indicated a much-diversified pattern in behavior of long-term trends than it might have been expected. The findings of this study may help identify the potentially most vulnerable near-natural headwater catchments facing worsening summer water scarcity.
topic low flows
streamflow drought
minimum discharges
headwater
seasonality
trends
url https://www.mdpi.com/2073-4441/12/12/3575
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