Comparison of artificial neural networks and reservoir models for simulating karst spring discharge on five test sites in the Alpine and Mediterranean regions

被引:14
作者
Cinkus, Guillaume [1 ]
Wunsch, Andreas [2 ]
Mazzilli, Naomi [3 ]
Liesch, Tanja [2 ]
Chen, Zhao [4 ]
Ravbar, Natasa [5 ]
Doummar, Joanna [6 ]
Fernandez-Ortega, Jaime [7 ,8 ]
Barbera, Juan Antonio [7 ,8 ]
Andreo, Bartolome [7 ,8 ]
Goldscheider, Nico [2 ]
Jourde, Herve
机构
[1] Univ Montpellier, Hydrosci Montpellier HSM, CNRS, IRD, F-34090 Montpellier, France
[2] Karlsruhe Inst Technol KIT, Inst Appl Geosci, Kaiserstr 12, D-76131 Karlsruhe, Germany
[3] Univ Avignon, UMR EMMAH AU INRAE 1114, F-84000 Avignon, France
[4] Tech Univ Dresden, Inst Groundwater Management, D-01062 Dresden, Germany
[5] Karst Res Inst, ZRC SAZU, Titov Trg 2, Postojna 6230, Slovenia
[6] Amer Univ Beirut, Dept Geol, POB 11-0236-26, Beirut, Lebanon
[7] Univ Malaga CEHIUMA, Dept Geol, Malaga 29071, Spain
[8] Univ Malaga CEHIUMA, Ctr Hydrogeol, Malaga 29071, Spain
关键词
HYDROLOGICAL MODELS; MULTIMODEL APPROACH; FUTURE CLIMATE; WATER; GROUNDWATER; CATCHMENT; AQUIFER; INPUT; BASIN; VULNERABILITY;
D O I
10.5194/hess-27-1961-2023
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Hydrological models are widely used to characterize, understand and manage hydrosystems. Lumped parameter models are of particular interest in karst environments given the complexity and heterogeneity of these systems. There is a multitude of lumped parameter modelling approaches, which can makeit difficult for a manager or researcher to choose. We therefore conducted a comparison of two lumped parameter modelling approaches: artificialneural networks (ANNs) and reservoir models. We investigate five karst systems in the Mediterranean and Alpine regions with different characteristics in terms of climatic conditions, hydrogeological properties and data availability. We compare the results of ANN and reservoir modelling approachesusing several performance criteria over different hydrological periods. The results show that both ANNs and reservoir models can accurately simulate karst spring discharge but also that they have different advantages and drawbacks: (i) ANN models are very flexible regarding the format and amountof input data, (ii) reservoir models can provide good results even with a few years of relevant discharge in the calibration period and (iii) ANN models seem robust for reproducing high-flow conditions, while reservoir models are superior in reproducing low-flow conditions. However, both modelling approaches struggle to reproduce extreme events (droughts, floods), which is a known problem in hydrological modelling. For researchpurposes, ANN models have been shown to be useful for identifying recharge areas and delineating catchments, based on insights into the input data. Reservoir models are adapted to understand the hydrological functioning of a system by studying model structure and parameters.
引用
收藏
页码:1961 / 1985
页数:25
相关论文
共 121 条
[1]   Revealing topoclimatic heterogeneity using meteorological station data [J].
Aalto, Juha ;
Riihimaki, Henri ;
Meineri, Eric ;
Hylander, Kristoffer ;
Luoto, Miska .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2017, 37 :544-556
[2]  
Abadi M., 2016, PREPRINT, DOI DOI 10.48550/ARXIV.1603.04467
[3]   Legacy, Rather Than Adequacy, Drives the Selection of Hydrological Models [J].
Addor, N. ;
Melsen, L. A. .
WATER RESOURCES RESEARCH, 2019, 55 (01) :378-390
[4]  
Allen R. G., 1998, FAO Irrigation and Drainage Paper
[5]   Karst groundwater protection:: First application of a Pan-European Approach to vulnerability, hazard and risk mapping in the Sierra de Libar (Southern Spain) [J].
Andreo, B ;
Goldscheider, N ;
Vadillo, I ;
Vías, JM ;
Neukum, C ;
Sinreich, M ;
Jiménez, P ;
Brechenmacher, J ;
Carrasco, F ;
Hötzl, H ;
Perles, MJ ;
Zwahlen, F .
SCIENCE OF THE TOTAL ENVIRONMENT, 2006, 357 (1-3) :54-73
[6]  
Andreo B., 2004, REV SOC GEOL ESPANA, V17, P187
[7]  
ARSO, ARCH MET DAT ARSO DA
[8]  
ARSO, 2021, ARCH HYDR DAT ARSO D
[9]   Karst groundwater: a challenge for new resources [J].
Bakalowicz, M .
HYDROGEOLOGY JOURNAL, 2005, 13 (01) :148-160
[10]  
Bergstrom S., 1992, Project Report, 32