Assessment of Climate Variables under CMIP6 Future Climate Scenarios in a Semi-Arid Region of Northwestern Iran

نوع مقاله : مقاله پژوهشی

نویسندگان

1 Department of Natural Resources, Faculty of Agriculture and Natural Resources, Member of Water Management Research Center, University of Mohaghegh Ardabili, Ardabil, Iran

2 Ardabil Agricultural and Natural Resources Research and Education Center, Agricultural Research, Education and Extension Organization (AREEO), Ardabil, Iran

3 Department of Watershed Management, Faculty of Range and Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran

‎10.22052/deej.2026.258580.1140

چکیده

Climate change, largely driven by anthropogenic activities, has intensified the frequency and severity of extreme weather events, including floods, droughts, hailstorms, heatwaves, and anomalous cold spells. This study evaluates the performance of three CMIP6 models (ACCESS-CM2, MIROC6, and NESM3) in simulating daily precipitation and temperature for the flood-prone Gharesou watershed in Ardabil, Iran. The models were validated against observed data from 1984–2014 using statistical metrics, including Root Mean Square Error (RMSE), Percent Bias (PBIAS), and the Nash-Sutcliffe Efficiency (NSE). Following validation, future projections were downscaled and bias-corrected under SSP1-2.6, SSP2-4.5, and SSP3-7.0 scenarios using the delta change method. Based on the superior performance in PBIAS and NSE metrics across all stations—with minor exceptions in specific precipitation and maximum temperature parameters at the Ardabil and Namin stations—the ACCESS-CM2 model was selected for long-term projections. The results indicate a general downward trend in monthly precipitation, with localized exceptions during the June–August period in Ardabil, March–August at the Airport station, and July in Namin and Nir. A comparative analysis between observed and projected mean annual precipitation under the SSP1-2.6 scenario reveals site-specific variations: declines of 31.07 mm, 37.60 mm, and 116.69 mm at the Ardabil, Namin, and Nir stations, respectively, alongside a marginal increase of 1.44 mm at the Ardabil airport station. Furthermore, all scenarios project a consistent rise in mean annual maximum and minimum temperatures. Specifically, the projected increase in maximum temperature ranges from 1.2 °C (SSP2-4.5, Ardabil) to 2.05 °C (SSP1-2.6, Namin), while minimum temperatures are expected to rise by 3.65 °C (SSP2-4.5, Namin) to 7.75 °C (SSP1-2.6, Ardabil airport). These forecasts, characterized by decreasing precipitation and significant warming, underscore the likelihood of imminent climate-driven extremes. Consequently, these findings provide a critical foundation for water resource managers to develop targeted risk mitigation strategies and enhance environmental and hydrological resilience in the region.

کلیدواژه‌ها

موضوعات


عنوان مقاله [English]

Assessment of Climate Variables under CMIP6 Future Climate Scenarios in a Semi-Arid Region of Northwestern Iran

نویسندگان [English]

  • Raoof Mostafazadeh 1
  • Ali Nasiri Khiavi 2
  • Shahnaz Mirzaei 3
1 Department of Natural Resources, Faculty of Agriculture and Natural Resources, Member of Water Management Research Center, University of Mohaghegh Ardabili, Ardabil, Iran
2 Ardabil Agricultural and Natural Resources Research and Education Center, Agricultural Research, Education and Extension Organization (AREEO), Ardabil, Iran
3 Department of Watershed Management, Faculty of Range and Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
چکیده [English]

Climate change, largely driven by anthropogenic activities, has intensified the frequency and severity of extreme weather events, including floods, droughts, hailstorms, heatwaves, and anomalous cold spells. This study evaluates the performance of three CMIP6 models (ACCESS-CM2, MIROC6, and NESM3) in simulating daily precipitation and temperature for the flood-prone Gharesou watershed in Ardabil, Iran. The models were validated against observed data from 1984–2014 using statistical metrics, including Root Mean Square Error (RMSE), Percent Bias (PBIAS), and the Nash-Sutcliffe Efficiency (NSE). Following validation, future projections were downscaled and bias-corrected under SSP1-2.6, SSP2-4.5, and SSP3-7.0 scenarios using the delta change method. Based on the superior performance in PBIAS and NSE metrics across all stations—with minor exceptions in specific precipitation and maximum temperature parameters at the Ardabil and Namin stations—the ACCESS-CM2 model was selected for long-term projections. The results indicate a general downward trend in monthly precipitation, with localized exceptions during the June–August period in Ardabil, March–August at the Airport station, and July in Namin and Nir. A comparative analysis between observed and projected mean annual precipitation under the SSP1-2.6 scenario reveals site-specific variations: declines of 31.07 mm, 37.60 mm, and 116.69 mm at the Ardabil, Namin, and Nir stations, respectively, alongside a marginal increase of 1.44 mm at the Ardabil airport station. Furthermore, all scenarios project a consistent rise in mean annual maximum and minimum temperatures. Specifically, the projected increase in maximum temperature ranges from 1.2 °C (SSP2-4.5, Ardabil) to 2.05 °C (SSP1-2.6, Namin), while minimum temperatures are expected to rise by 3.65 °C (SSP2-4.5, Namin) to 7.75 °C (SSP1-2.6, Ardabil airport). These forecasts, characterized by decreasing precipitation and significant warming, underscore the likelihood of imminent climate-driven extremes. Consequently, these findings provide a critical foundation for water resource managers to develop targeted risk mitigation strategies and enhance environmental and hydrological resilience in the region.

کلیدواژه‌ها [English]

  • Delta change factor
  • Bias correction
  • ACCESS-CM2 model
  • SSP1-2.6 scenario
  • Gharesou watershed
  • Alimohamadian, L., Mostafazadeh, R., & Mirzaei Hassanlu, A. (2026). Estimating the variability of climate temperature extremes using statistical distributions over a diverse climatic region. Geomatics, Natural Hazards and Risk17(1), 2608251.
  • Anandhi, A., Frei, A., Pierson, D. C., Schneiderman, E. M., Zion, M. S., Lounsbury, D., & Matonse, A. H. (2011). Examination of change factor methodologies for climate change impact assessment. Water Resources Research47(3).
  • Ansari, S., Dehban, H., Zareian, M., & Farokhnia, A. (2022). Investigation of temperature and precipitation changes in the Iran's basins in the next 20 years based on the output of CMIP6 model. Iranian Water Research Journal16(1), 11-24.
  • Asgari, E., Mostafazadeh, R., & Talebi Khiavi, H. (2025). Projecting the climate change impact on water yield in a cold mountainous watershed, ardabil. Journal of the Earth and Space Physics50(4), 165-177.
  • Ashfaq, M., Rastogi, D., Kitson, J., Abid, M. A., & Kao, S. C. (2022). Evaluation of CMIP6 GCMs over the CONUS for downscaling studies. Journal of Geophysical Research: Atmospheres, 127(21), e2022JD036659.
  • Azad, N., & Ahmadi, A. (2024). Assessment of CMIP6 models and multi-model averaging for temperature and precipitation over Iran. Scientific Reports, 14(1), 24165.
  • Azari, M., Saghafian, B., Moradi, H. R., & Faramarzi, M. (2017). Effectiveness of soil and water conservation practices under climate change in the Gorganroud Basin, Iran. CLEAN–Soil, Air, Water45(8), 1700288.
  • Coelho, G. D. A., Ferreira, C. M., Johnston, J., Kinter III, J. L., Dollan, I. J., & Maggioni, V. (2022). Potential impacts of future extreme precipitation changes on flood engineering design across the contiguous United States. Water Resources Research58(4), e2021WR031432.
  • Dadashi, R., Esmali-Ouri, A., Mostafazadeh, R., & Haji, K. (2024). Multi-criteria evaluation of the environmental carrying capacity (ECC) of Gharesou watershed in Ardabil province to optimal utilization of watershed resource. Environmental Earth Sciences83(4), 131.
  • Dannenberg, M. P., Wise, E. K., & Smith, W. K. (2019). Reduced tree growth in the semiarid United States due to asymmetric responses to intensifying precipitation extremes. Science advances5(10), eaaw0667.
  • Dawson, C. W., Abrahart, R. J., & See, L. M. (2007). HydroTest: a web-based toolbox of evaluation metrics for the standardised assessment of hydrological forecasts. Environmental Modelling & Software22(7), 1034-1052.
  • Döscher, R., Acosta, M., Alessandri, A., Anthoni, P., Arneth, A., Arsouze, T., ... & Zhang, Q. (2021). The EC-earth3 Earth system model for the climate model intercomparison project 6. Geoscientific Model Development Discussions2021, 1-90.
  • Esgandari, R., Esmali Ouri, A., Mostafazadeh, R., & Choobeh, S. (2024). Assessment of temporal and spatial variations of precipition climate extreme indexes in the central part of Ardabil province. Journal of Environmental Science Studies, 9(1), 8119-8133.
  • Estoque, R. C., Ooba, M., Togawa, T., & Hijioka, Y. (2020). Projected land-use changes in the Shared Socioeconomic Pathways: Insights and implications. Ambio49(12), 1972-1981.
  • Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., & Taylor, K. E. (2016). Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. Geoscientific Model Development9(5), 1937-1958.
  • Fowler, H. J., Blenkinsop, S., & Tebaldi, C. (2007). Linking climate change modelling to impacts studies: recent advances in downscaling techniques for hydrological modelling. International Journal of Climatology: A Journal of the Royal Meteorological Society27(12), 1547-1578.
  • Gimechi, S., Mostafazadeh, R., & Alimohamadian, L. (2025). Analysis of extreme precipitation trends and probability distributions across return periods in northwest Iran. Geografický časopis/Geographical Journal, 77(1), 43-55.
  • Golshan, M., Kavian, A., Esmali, A., & Ziegler, A. D. (2020). Runoff and sediment yield modeling in data-sparse catchments in the Garehsoo River basin, northern Iran. Environmental Earth Sciences79(14), 351.
  • Hawkins, E., & Sutton, R. (2009). The potential to narrow uncertainty in regional climate predictions. Bulletin of the American Meteorological Society90(8), 1095-1108.
  • Hay, L. E., Wilby, R. L., & Leavesley, G. H. (2000). A comparison of delta change and downscaled GCM scenarios for three mountainous basins in the United States 1. JAWRA Journal of the American Water Resources Association36(2), 387-397.
  • Hazbavi, Z., Azizi, E., Ghabelnezam, E., Sharifi, Z., Davudirad, A., & Fathololoumi, S. (2025). Enhancing Watershed Management Through the Characterization of the River Restoration Index (RRI): A Case Study of the Samian Watershed, Ardabil Province, Iran. Earth6(1), 6.
  • Hussain, S., Mubeen, M., Nasim, W., Mumtaz, F., Abdo, H. G., Mostafazadeh, R., & Fahad, S. (2024). Assessment of future prediction of urban growth and climate change in district Multan, Pakistan using CA-Markov method. Urban Climate53, 101766.
  • Intergovernmental Panel on Climate Change (IPCC). (2013). Climate Change 2013 - The Physical Science Basis. Working Group I Contribution to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. 1552p.
  • Intergovernmental Panel on Climate Change (IPCC). (2021). Climate Change 2021: The physical science basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change; technical summary.
  • Intergovernmental Panel on Climate Change (IPCC). (2023). Climate Change 2021 – The Physical Science Basis: Working Group I Contribution to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press.
  • Iranshahi, M., Ebrahimi, B., Yousefi, H., & Moridi, A. (2023). Investigating the effects of climate change on temperature and precipitation using neural network and CMIP6 (Case study: Aleshtar and Khorramabad Stations). Water and Irrigation Management12(4), 821-845.
  • Khansalari, S., & Mohammadi, A. (2024). Probabilistic projection of extreme precipitation changes over Iran by the CMIP6 multi-model ensemble. Climatic Change177(7), 115.
  • Khordadi, M. J., Alizadeh, A., Nassiri Mahallati, M., & Hooshmand, D. (2014). An evaluation of the impact of climate change on climatic parameters and dry and wet spells in the next 100 years using combining IDW and change factor methods (A case study in Tehran-Karaj subbasin). Journal of Geography and Regional Development21, 157-178.
  • Liu, J., Jiang, L., Zhang, X., Druce, D., Kittel, C. M., Tøttrup, C., & Bauer-Gottwein, P. (2021). Impacts of water resources management on land water storage in the North China Plain: Insights from multi-mission earth observations. Journal of Hydrology603, 126933.
  • Luo, Q., & Yu, Q. (2012). Developing higher resolution climate change scenarios for agricultural risk assessment: progress, challenges and prospects. International journal of biometeorology56(4), 557-568.
  • Maraun, D. (2016). Bias correcting climate change simulations-a critical review. Current Climate Change Reports2(4), 211-220.
  • Meresa, H., Tischbein, B., & Mekonnen, T. (2022). Climate change impact on extreme precipitation and peak flood magnitude and frequency: observations from CMIP6 and hydrological models. Natural Hazards111(3), 2649-2679.
  • Moriasi, D. N., Arnold, J. G., Van Liew, M. W., Bingner, R. L., Harmel, R. D., & Veith, T. L. (2007). Model evaluation guidelines for systematic quantification of accuracy in watershed simulations. Transactions of the ASABE50(3), 885-900.
  • Mostafazadeh, R., Amini, H., & Adhami, M. (2025). Snow cover changes and affecting hydro-climate variables in Sabalan Mountainous region in Northwest Iran.  Researches in Earth Sciences, 16(Special Issue), 18-30.
  • Naserabadi, F., Esmali Ouri, A., Akbari, H., & Rostamian, R. (2014). A sensitivity analysis of SWAT model in Ghareh Su watershed, Ardabil. Watershed Engineering and Management5(4), 255-265.
  • Ouyang, F., Zhu, Y., Fu, G., Lü, H., Zhang, A., Yu, Z., & Chen, X. (2015). Impacts of climate change under CMIP5 RCP scenarios on streamflow in the Huangnizhuang catchment. Stochastic environmental research and risk assessment29(7), 1781-1795.
  • Rogelj, J., Popp, A., Calvin, K. V., Luderer, G., Emmerling, J., Gernaat, D., ... & Tavoni, M. (2018). Scenarios towards limiting global mean temperature increase below 1.5 C. Nature climate change8(4), 325-332.
  • Stocker, T.F., Qin, D., Plattner, G.K., Tignor, M., Allen, S.K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P.M. (2013). Climate Change 2013, the Physical Science Basis. Intergovernmental Panel on Climate Change, 222p.
  • Su, B., Huang, J., Gemmer, M., Jian, D., Tao, H., Jiang, T., & Zhao, C. (2016). Statistical downscaling of CMIP5 multi-model ensemble for projected changes of climate in the Indus River Basin. Atmospheric Research178, 138-149.
  • Teutschbein, C., & Seibert, J. (2012). Bias correction of regional climate model simulations for hydrological climate-change impact studies: Review and evaluation of different methods. Journal of hydrology456, 12-29.
  • Voldoire, A., Saint‐Martin, D., Sénési, S., Decharme, B., Alias, A., Chevallier, M., ... & Waldman, R. (2019). Evaluation of CMIP6 deck experiments with CNRM‐CM6‐Journal of Advances in Modeling Earth Systems11(7), 2177-2213.
  • Wang, H., Jiang, P., Zhang, R., Zhao, J., Si, W., Fang, Y., & Zhang, N. (2023). The changing precipitation storm properties under future climate change. Hydrology Research54(4), 580-590.
  • Wang, Q., Sun, Y., Guan, Q., Du, Q., Zhang, Z., Zhang, J., & Zhang, E. (2024). Exploring future trends of precipitation and runoff in arid regions under different scenarios based on a bias-corrected CMIP6 model. Journal of Hydrology630, 130666.
  • Wu, Y., Ju, H., Qi, P., Li, Z., Zhang, G., & Sun, Y. (2023). Increasing flood risk under climate change and social development in the Second Songhua River basin in Northeast China. Journal of Hydrology: Regional Studies48, 101459.
  • Zareian, M. J., Dehban, H., & Gohari, A. (2023). Evaluation of the Accuracy of CMIP6 Models in Estimating the Temperature and Precipitation of Iran Based on a Network Analysis. Water and Irrigation Management, 12 (4), 783-797.
  • Zarrin, A., & Dadashi-Roudbari, A. (2021). Projection of future extreme precipitation in Iran based on CMIP6 multi-model ensemble: A. Zarrin, A. Dadashi-Roudbari. Theoretical and Applied Climatology144(1), 643-660.