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Prediction of future groundwater levels under representative concentration pathway scenarios using an inclusive multiple model coupled with artificial neural networks
Semnan Univ, Dept Water Engn, Semnan, Iran..
KTH, School of Architecture and the Built Environment (ABE), Sustainable development, Environmental science and Engineering, Water and Environmental Engineering.ORCID iD: 0000-0002-7978-0040
Stockholm Univ, Bolin Ctr Climate Res, Dept Phys Geog, SE-10691 Stockholm, Sweden.;Polytech Inst Coimbra, Coimbra Agr Tech Sch, Res Ctr Nat Resources Environm & Soc CERNAS, P-3045601 Coimbra, Portugal..
Hong Kong Polytech Univ, Dept Civil & Environm Engn, Hong Kong, Peoples R China..
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2022 (English)In: Journal of Water and Climate, ISSN 2040-2244, Vol. 13, no 10, p. 3620-3643Article in journal (Refereed) Published
Abstract [en]

Groundwater (GW) plays a key role in water supply in basins. As global warming and climate change affect groundwater level (GWL), it is important to predict it for planning and managing water resources. This study investigates the GWL of the Yazd-Ardakan Plain basin in Iran for the base period of 1979-2005 and predicts for periods of 2020-2059 and 2060-2099. Lagged temperature and rainfall are used as inputs to hybrid and standalone artificial neural network (ANN) models. In this study, the rat swarm algorithm (RSA), particle swarm optimisation (PSO), salp swarm algorithm (SSA), and genetic algorithm (GA) are used to adjust ANN models. The outcomes of these models are then entered into an inclusive multiple model (IMM) as an ensemble model. In this study, the output of climate models is also inserted into the IMM model to improve the estimation accuracy of temperature, rainfall, and GWL. The monthly average temperature for the base period is 12.9 degrees C, while average temperatures for 2020-2059 under RCP 4.5 and RCP 8.5 scenarios are 14.5 and 15.1 degrees C, and for 2060-2099 they are 16.41 and 18.5 degrees C under the same scenarios, respectively. In future periods, rainfall is low in comparison with the base period. Lagged rainfall and temperature of the base period are inserted into ANN-RSA, ANN-SSA, ANN-PSO, ANN-GA, and ANN models to predict GWL for the base period. Outputs of IMM, ANN, and the five hybrid models (ANN-RSA, ANN-SSA, ANN-PSO, and ANN-GA) indicate that root mean square errors (RMSE) are 2.12, 3.2, 4.58, 6.12, 6.98, and 7.89 m, respectively, in the testing level. It is found that GWL depletion in 2020-2059 under RCP 4.5 and RCP 8.5 scenarios are 0.60-0.88 m and 0.80-1.16 m, and in 2060-2099 under the same scenarios they are 1.49-1.97 m and 1.75-1.98 m, respectively. The results highlight the need to prevent overexploitation of GW in the Ardakan-Yazd Plain to avoid water shortages in the future.

Place, publisher, year, edition, pages
IWA Publishing , 2022. Vol. 13, no 10, p. 3620-3643
Keywords [en]
climate models, RCP scenarios, soft computing models, sustainable water resource management
National Category
Geotechnical Engineering
Identifiers
URN: urn:nbn:se:kth:diva-321625DOI: 10.2166/wcc.2022.198ISI: 000875744100007Scopus ID: 2-s2.0-85140892383OAI: oai:DiVA.org:kth-321625DiVA, id: diva2:1712299
Note

QC 20221121

Available from: 2022-11-21 Created: 2022-11-21 Last updated: 2022-11-21Bibliographically approved

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Kalantari, Zahra

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