Assessment of MC&MCMC uncertainty analysis frameworks on SWAT model by focusing on future runoff prediction in a mountainous watershed via CMIP5 models

Author:

Ahmadi Armin1,Aghakhani Afshar Amirhosein2,Nourani Vahid33,Pourreza-Bilondi Mohsen4,Besalatpour A. A.5

Affiliation:

1. Department of Civil Engineering, Mashhad Branch, Islamic Azad University, Mashhad, Iran

2. Department of Water Engineering, Faculty of Civil Engineering, University of Tabriz, Tabriz, Iran

3. Center of Excellence in Hydroinformatics, Faculty of Civil Engineering, University of Tabriz, Tabriz, Iran and Near East University, Faculty of Civil and Environmental Engineering, Near East Boulevard, 99138, North Cyprus, via Mersin 10, Nicosia, Turkey

4. Department of Water Engineering, College of Agriculture, University of Birjand, Birjand, Iran

5. Inter3 GmbH Institut für Ressourcenmanagement, Otto-Suhr-Allee 59, 10585 Berlin, Germany

Abstract

Abstract The river situation in a dry or semi-dry area is extremely affected by climate change and precipitation patterns. In this study, the impact of climate alteration on runoff in Kashafrood River Basin (KRB) in Iran was investigated using the Soil and Water Assessment Tool (SWAT) in historical and three future period times. The runoff was studied by MIROC-ESM and GFDL-ESM2G models as the outputs of general circulation models (GCMs) in the Coupled Model Intercomparison Project Phase 5 (CMIP5) by two representative concentration pathway (RCP) scenarios (RCP2.6 and RCP8.5). The DiffeRential Evolution Adaptive Metropolis (DREAM-ZS) was used to calibrate the hydrological model parameters in different sub-basins. Using DREAM-ZS algorithm, realistic values were obtained for the parameters related to runoff simulation in the SWAT model. In this area, results show that runoff in GFDL-ESM2G in both RCPs (2.6 and 8.5) in comparing future periods with the historical period is increased about 232–383% and in MIROC-ESM tends to increase around 87–292%. Furthermore, GFDL-ESM2G compared to MIROC-ESM in RCP2.6 (RCP8.5) in near, intermediate, and far future periods shows that the value of runoff increases 59.6% (23.0%), 100.2% (35.1%), and 42.5% (65.3%), respectively.

Publisher

IWA Publishing

Subject

Management, Monitoring, Policy and Law,Atmospheric Science,Water Science and Technology,Global and Planetary Change

Reference73 articles.

1. Determination of monthly hydrological erosion severity and runoff in torogh dam watershed basin using SWAT and WEPP models;Iranian Journal of Science and Technology, Transactions of Civil Engineering,2017

2. Climate change forecasting in a mountainous data scarce watershed using CMIP5 models under representative concentration pathways;Theoretical and Applied Climatology,2017

3. Analyzing long-term spatial variability of blue and green water footprints in a semi-arid mountainous basin with MIROC-ESM model (case study: Kashafrood River Basin, Iran);Theoretical and Applied Climatology,2018

4. Assessing the uncertainty of the Xinanjiang rainfall-runoff model: effect of the likelihood function choice on the GLUE method;Journal of Hydrologic Engineering,2015

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