Monthly blue water footprint caps in a river basin to achieve sustainable water consumption: The role of reservoirs.

Blue water scarcity Environmental flow requirement Reservoir storage Sustainable blue water footprint

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:
10 Feb 2019
Historique:
received: 30 06 2018
revised: 02 09 2018
accepted: 07 09 2018
entrez: 13 10 2018
pubmed: 13 10 2018
medline: 13 10 2018
Statut: ppublish

Résumé

The blue water footprint (WF) measures the consumption of runoff in a river basin. In order to ensure sustainable water consumption, setting a monthly blue WF cap, that is an upper-limit to the blue WF in a river basin each month, can be a suitable policy instrument. The blue WF cap in a river basin depends on the precipitation that becomes runoff and the need to maintain a minimum flow for sustaining ecosystems and livelihoods. Reservoirs along the river generally smooth runoff variability and thus raise the WF cap and reduce blue water scarcity during the dry season. Previous water scarcity studies, considering the ratio of actual blue WF to the blue WF cap under natural background conditions, have not studied this effect of reservoir storages. Here we assess how water reservoirs influence blue WF caps over time and how they affect the variability of blue water scarcity in a river basin. We take the Yellow River Basin over the period January 2002-July 2006 as case study and consider data on observed storage changes in five large reservoirs along the main stream. Results indicate that reservoirs redistribute the blue WF cap and blue water scarcity levels over time. Monthly blue WF caps were generally lowered by reservoir storage during the flood season (July-October) and raised by reservoir releases over the period of highest crop demand (March-June). However, with water storage exceeding 20% of natural runoff in most rainy months, reservoirs contribute to "scarcity in the wet months", which is to be understood as a situation in which environmental flow requirements related to the occurrence of natural peak flows are no longer met.

Identifiants

pubmed: 30308863
pii: S0048-9697(18)33532-0
doi: 10.1016/j.scitotenv.2018.09.090
pii:
doi:

Types de publication

Journal Article

Langues

eng

Pagination

891-899

Informations de copyright

Copyright © 2018 Elsevier B.V. All rights reserved.

Auteurs

La Zhuo

Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China; National Engineering Research Centre for Water Saving Irrigation at Yangling, Yangling 712100, China. Electronic address: zhuola@nwafu.edu.cn.

Arjen Y Hoekstra (AY)

Twente Water Centre, University of Twente, P.O. Box 217, 7500AE Enschede, the Netherlands; Institute of Water Policy, Lee Kuan Yew School of Public Policy, National University of Singapore, 259770, Singapore.

Pute Wu (P)

Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China; National Engineering Research Centre for Water Saving Irrigation at Yangling, Yangling 712100, China. Electronic address: gjzwpt@vip.sina.com.

Xining Zhao (X)

Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China; National Engineering Research Centre for Water Saving Irrigation at Yangling, Yangling 712100, China.

Classifications MeSH