Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)

Managers need to know how to mitigate rising stream water temperature (WT) due to climate change. This requires identifying the environmental drivers that influence thermal regime and determining the spatial area where interventions are most effective. We hypothesized that (i) extreme thermal events...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Blandine Georges, Adrien Michez, Hervé Piegay, Leo Huylenbroeck, Philippe Lejeune, Yves Brostaux
Formato: article
Lenguaje:EN
Publicado: PeerJ Inc. 2021
Materias:
R
Acceso en línea:https://doaj.org/article/c6142b7acf0f4174acbc44f12f8b2f92
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:c6142b7acf0f4174acbc44f12f8b2f92
record_format dspace
spelling oai:doaj.org-article:c6142b7acf0f4174acbc44f12f8b2f922021-11-24T15:05:10ZWhich environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)10.7717/peerj.124942167-8359https://doaj.org/article/c6142b7acf0f4174acbc44f12f8b2f922021-11-01T00:00:00Zhttps://peerj.com/articles/12494.pdfhttps://peerj.com/articles/12494/https://doaj.org/toc/2167-8359Managers need to know how to mitigate rising stream water temperature (WT) due to climate change. This requires identifying the environmental drivers that influence thermal regime and determining the spatial area where interventions are most effective. We hypothesized that (i) extreme thermal events can be influenced by a set of environmental factors that reduce thermal sensitivity and (ii) the role played by those factors varies spatially. To test these hypotheses, we (i) determined which of the environmental variables reported to be the most influential affected WT and (ii)identified the spatial scales over which those environmental variables influenced WT. To this end, the influence of multi-scale environmental variables, namely land cover, topography (channel slope, elevation), hydromorphology (channel sinuosity, water level, watershed area, baseflow index) and shade conditions, was analyzed on the three model variables (day thermal sensitivity, night thermal sensitivity, and non-convective thermal flux) in the model developed by Georges et al. (2021) of the temporal thermal dynamics of daily maximum WT during extreme events. Values were calculated on six spatial scales (the entire upstream catchment and the associated 1 km and 2 km circular buffer, and 50 m wide corridors on each side of the stream with the associated 1 km and 2 km circular buffer). The period considered was 17 extreme days during the summer identified by Georges et al. (2021) based on WT data measured every 10 min for 7 years (2012–2018) at 92 measurement sites. Sites were located evenly throughout the Wallonia (southern Belgium) hydrological network. Results showed that shade, baseflow index (a proxy of the influence of groundwater), water level and watershed area were the most significant variables influencing thermal sensitivity. Since managers with finite financial and human resources can act on only a few environmental variables, we advocate restoring and preserving the vegetation cover that limits solar radiation on the watercourse as a cost-effective solution to reduce thermal sensitivity. Moreover, management at small spatial scale (50 m riparian buffer) should be strategically promoted (for finance and staffing) as our results show that a larger management scale is not more effective in reducing thermal sensitivity to extreme events.Blandine GeorgesAdrien MichezHervé PiegayLeo HuylenbroeckPhilippe LejeuneYves BrostauxPeerJ Inc.articleStream water temperatureRiparian vegetationChannel morphologyShadeExtremeEnvironmental factorsMedicineRENPeerJ, Vol 9, p e12494 (2021)
institution DOAJ
collection DOAJ
language EN
topic Stream water temperature
Riparian vegetation
Channel morphology
Shade
Extreme
Environmental factors
Medicine
R
spellingShingle Stream water temperature
Riparian vegetation
Channel morphology
Shade
Extreme
Environmental factors
Medicine
R
Blandine Georges
Adrien Michez
Hervé Piegay
Leo Huylenbroeck
Philippe Lejeune
Yves Brostaux
Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
description Managers need to know how to mitigate rising stream water temperature (WT) due to climate change. This requires identifying the environmental drivers that influence thermal regime and determining the spatial area where interventions are most effective. We hypothesized that (i) extreme thermal events can be influenced by a set of environmental factors that reduce thermal sensitivity and (ii) the role played by those factors varies spatially. To test these hypotheses, we (i) determined which of the environmental variables reported to be the most influential affected WT and (ii)identified the spatial scales over which those environmental variables influenced WT. To this end, the influence of multi-scale environmental variables, namely land cover, topography (channel slope, elevation), hydromorphology (channel sinuosity, water level, watershed area, baseflow index) and shade conditions, was analyzed on the three model variables (day thermal sensitivity, night thermal sensitivity, and non-convective thermal flux) in the model developed by Georges et al. (2021) of the temporal thermal dynamics of daily maximum WT during extreme events. Values were calculated on six spatial scales (the entire upstream catchment and the associated 1 km and 2 km circular buffer, and 50 m wide corridors on each side of the stream with the associated 1 km and 2 km circular buffer). The period considered was 17 extreme days during the summer identified by Georges et al. (2021) based on WT data measured every 10 min for 7 years (2012–2018) at 92 measurement sites. Sites were located evenly throughout the Wallonia (southern Belgium) hydrological network. Results showed that shade, baseflow index (a proxy of the influence of groundwater), water level and watershed area were the most significant variables influencing thermal sensitivity. Since managers with finite financial and human resources can act on only a few environmental variables, we advocate restoring and preserving the vegetation cover that limits solar radiation on the watercourse as a cost-effective solution to reduce thermal sensitivity. Moreover, management at small spatial scale (50 m riparian buffer) should be strategically promoted (for finance and staffing) as our results show that a larger management scale is not more effective in reducing thermal sensitivity to extreme events.
format article
author Blandine Georges
Adrien Michez
Hervé Piegay
Leo Huylenbroeck
Philippe Lejeune
Yves Brostaux
author_facet Blandine Georges
Adrien Michez
Hervé Piegay
Leo Huylenbroeck
Philippe Lejeune
Yves Brostaux
author_sort Blandine Georges
title Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
title_short Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
title_full Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
title_fullStr Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
title_full_unstemmed Which environmental factors control extreme thermal events in rivers? A multi-scale approach (Wallonia, Belgium)
title_sort which environmental factors control extreme thermal events in rivers? a multi-scale approach (wallonia, belgium)
publisher PeerJ Inc.
publishDate 2021
url https://doaj.org/article/c6142b7acf0f4174acbc44f12f8b2f92
work_keys_str_mv AT blandinegeorges whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
AT adrienmichez whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
AT hervepiegay whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
AT leohuylenbroeck whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
AT philippelejeune whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
AT yvesbrostaux whichenvironmentalfactorscontrolextremethermaleventsinriversamultiscaleapproachwalloniabelgium
_version_ 1718414955754029056