Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871

The length of streamflow observations is generally limited to the last 50 years even in data-rich countries like France. It therefore offers too small a sample of extreme low-flow events to properly explore the long-term evolution of their characteristics and associated impacts. To overcome this...

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Main Authors: L. Caillouet, J.-P. Vidal, E. Sauquet, A. Devers, B. Graff
Format: Article
Language:English
Published: Copernicus Publications 2017-06-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/21/2923/2017/hess-21-2923-2017.pdf
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spelling doaj-bc28f3aeb3b542ad8461ddf607fe3f482020-11-24T23:14:13ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-06-01212923295110.5194/hess-21-2923-2017Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871L. Caillouet0J.-P. Vidal1E. Sauquet2A. Devers3B. Graff4Irstea, UR HHLY, Hydrology and Hydraulics Research Unit, 5 rue de la Doua, BP32108, 69616 Villeurbanne CEDEX, FranceIrstea, UR HHLY, Hydrology and Hydraulics Research Unit, 5 rue de la Doua, BP32108, 69616 Villeurbanne CEDEX, FranceIrstea, UR HHLY, Hydrology and Hydraulics Research Unit, 5 rue de la Doua, BP32108, 69616 Villeurbanne CEDEX, FranceIrstea, UR HHLY, Hydrology and Hydraulics Research Unit, 5 rue de la Doua, BP32108, 69616 Villeurbanne CEDEX, FranceCompagnie Nationale du Rhône (CNR), 2 rue André Bonin, 69004 Lyon, FranceThe length of streamflow observations is generally limited to the last 50 years even in data-rich countries like France. It therefore offers too small a sample of extreme low-flow events to properly explore the long-term evolution of their characteristics and associated impacts. To overcome this limit, this work first presents a daily 140-year ensemble reconstructed streamflow dataset for a reference network of near-natural catchments in France. This dataset, called SCOPE Hydro (Spatially COherent Probabilistic Extended Hydrological dataset), is based on (1) a probabilistic precipitation, temperature, and reference evapotranspiration downscaling of the Twentieth Century Reanalysis over France, called SCOPE Climate, and (2) continuous hydrological modelling using SCOPE Climate as forcings over the whole period. This work then introduces tools for defining spatio-temporal extreme low-flow events. Extreme low-flow events are first locally defined through the sequent peak algorithm using a novel combination of a fixed threshold and a daily variable threshold. A dedicated spatial matching procedure is then established to identify spatio-temporal events across France. This procedure is furthermore adapted to the SCOPE Hydro 25-member ensemble to characterize in a probabilistic way unrecorded historical events at the national scale. Extreme low-flow events are described and compared in a spatially and temporally homogeneous way over 140 years on a large set of catchments. Results highlight well-known recent events like 1976 or 1989–1990, but also older and relatively forgotten ones like the 1878 and 1893 events. These results contribute to improving our knowledge of historical events and provide a selection of benchmark events for climate change adaptation purposes. Moreover, this study allows for further detailed analyses of the effect of climate variability and anthropogenic climate change on low-flow hydrology at the scale of France.http://www.hydrol-earth-syst-sci.net/21/2923/2017/hess-21-2923-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Caillouet
J.-P. Vidal
E. Sauquet
A. Devers
B. Graff
spellingShingle L. Caillouet
J.-P. Vidal
E. Sauquet
A. Devers
B. Graff
Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
Hydrology and Earth System Sciences
author_facet L. Caillouet
J.-P. Vidal
E. Sauquet
A. Devers
B. Graff
author_sort L. Caillouet
title Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
title_short Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
title_full Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
title_fullStr Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
title_full_unstemmed Ensemble reconstruction of spatio-temporal extreme low-flow events in France since 1871
title_sort ensemble reconstruction of spatio-temporal extreme low-flow events in france since 1871
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-06-01
description The length of streamflow observations is generally limited to the last 50 years even in data-rich countries like France. It therefore offers too small a sample of extreme low-flow events to properly explore the long-term evolution of their characteristics and associated impacts. To overcome this limit, this work first presents a daily 140-year ensemble reconstructed streamflow dataset for a reference network of near-natural catchments in France. This dataset, called SCOPE Hydro (Spatially COherent Probabilistic Extended Hydrological dataset), is based on (1) a probabilistic precipitation, temperature, and reference evapotranspiration downscaling of the Twentieth Century Reanalysis over France, called SCOPE Climate, and (2) continuous hydrological modelling using SCOPE Climate as forcings over the whole period. This work then introduces tools for defining spatio-temporal extreme low-flow events. Extreme low-flow events are first locally defined through the sequent peak algorithm using a novel combination of a fixed threshold and a daily variable threshold. A dedicated spatial matching procedure is then established to identify spatio-temporal events across France. This procedure is furthermore adapted to the SCOPE Hydro 25-member ensemble to characterize in a probabilistic way unrecorded historical events at the national scale. Extreme low-flow events are described and compared in a spatially and temporally homogeneous way over 140 years on a large set of catchments. Results highlight well-known recent events like 1976 or 1989–1990, but also older and relatively forgotten ones like the 1878 and 1893 events. These results contribute to improving our knowledge of historical events and provide a selection of benchmark events for climate change adaptation purposes. Moreover, this study allows for further detailed analyses of the effect of climate variability and anthropogenic climate change on low-flow hydrology at the scale of France.
url http://www.hydrol-earth-syst-sci.net/21/2923/2017/hess-21-2923-2017.pdf
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