Ensemble warming projections in Germany's largest drinking water reservoir and potential adaptation strategies.

CE-QUAL-W2 Climate change Rappbode Reservoir Selective water withdrawal Thermal structure

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
15 Dec 2020
Historique:
received: 16 01 2020
revised: 19 07 2020
accepted: 28 07 2020
pubmed: 18 8 2020
medline: 18 8 2020
entrez: 18 8 2020
Statut: ppublish

Résumé

The thermal structure in reservoirs affects the development of aquatic ecosystems, and can be substantially influenced by climate change and management strategies. We applied a two-dimensional hydrodynamic model to explore the response of the thermal structure in Germany's largest drinking water reservoir, Rappbode Reservoir, to future climate projections and different water withdrawal strategies. We used projections for representative concentration pathways (RCP) 2.6, 6.0 and 8.5 from an ensemble of 4 different global climate models. Simulation results showed that epilimnetic water temperatures in the reservoir strongly increased under all three climate scenarios. Hypolimnetic temperatures remained rather constant under RCP 2.6 and RCP 6.0 but increased markedly under RCP 8.5. Under the intense warming in RCP 8.5, hypolimnion temperatures were projected to rise from 5 °C to 8 °C by the end of the century. Stratification in the reservoir was projected to be more stable under RCP 6.0 and RCP 8.5, but did not show significant changes under RCP 2.6. Similar results were found with respect to the light intensity within the mixed-layer. Moreover, the results suggested that surface withdrawal can be an effective adaptation strategy under strong climate warming (RCP 8.5) to reduce surface warming and avoid hypolimnetic warming. This study documents how global scale climate projections can be translated into site-specific climate impacts to derive adaptation strategies for reservoir operation. Moreover, our results illustrate that the most intense warming scenario, i.e. RCP 8.5, demands far-reaching climate adaptation while the mitigation scenario (RCP 2.6) does not require adaptation of reservoir management before 2100.

Identifiants

pubmed: 32798870
pii: S0048-9697(20)34895-6
doi: 10.1016/j.scitotenv.2020.141366
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

141366

Informations de copyright

Copyright © 2020 The Authors. Published by Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Chenxi Mi (C)

Helmholtz Centre for Environmental Research, Department of Lake Research, Magdeburg, Germany; College of Water Conservancy, Shenyang Agricultural University, Shenyang, China. Electronic address: chenxi.mi@ufz.de.

Tom Shatwell (T)

Helmholtz Centre for Environmental Research, Department of Lake Research, Magdeburg, Germany.

Jun Ma (J)

Hubei Key Laboratory of Ecological Restoration of River-Lakes and Algal Utilization, Hubei University of Technology, Wuhan, China.

Yaqian Xu (Y)

Hubei Key Laboratory of Ecological Restoration of River-Lakes and Algal Utilization, Hubei University of Technology, Wuhan, China.

Fangli Su (F)

College of Water Conservancy, Shenyang Agricultural University, Shenyang, China.

Karsten Rinke (K)

Helmholtz Centre for Environmental Research, Department of Lake Research, Magdeburg, Germany.

Classifications MeSH