Document Type : Research Paper

Authors

1 PhD student, Department of Physical Geography, University of Mohaghegh Ardabili

2 University of Mohaghegh Ardabili

3 Postdoctoral Research Associate, University of Mohaghegh Ardabili

Abstract

Climate change is a key factor in most weather-related disasters worldwide. Regarding its distinctive geographical location and diverse climate, Iran has the most variable climate in the world. The present study aims to investigate the effectiveness of the MPI-ESM-LR model from the CMIP5 model series in predicting the monthly temperature of Iran under representative concentration pathway scenarios (RCPs) with the CORDEX-WAS project. In this research, for the historical period of 1980-2005, the daily air temperature data of 49 synoptic stations of the country and the MPI-ESM-LR model under the CORDEX project were used. Likewise, for the future period, from the predicted temperature data of RCP 8.5, RCP 4.5, and RCP 2.6 scenarios of the mentioned model in three periods of the near-future (2021-2050), mid-future (2051-2075) and far-future (2076-2100) was used. Validation of the model was done with three statistical indices: r, RMSE, and MBE. The results revealed that the model has a good performance. The slope of the temperature trend in station data and model data has been increasing in the historical period and the future period in RCP8.5 and RCP4.5 in all months, the temperature trend slope has been observed in every decade. In all months, the maximum anomaly of temperature under the scenarios studied in all three future periods can be seen in the northwest and western highlands. The eastern and southeastern regions of Iran have indicated minimum temperature anomalies, except in RCP 2.6 and RCP 8.5, respectively, the southern coasts and the northeastern heights of the country also show minimum temperature anomalies. In the cold half of the year, the minimum area of temperature anomaly has been extended to the north-western heights and low-altitude interior regions of the country.

Highlights

Climate change is a key factor in most weather-related disasters worldwide. Regarding its distinctive geographical location and diverse climate, Iran has the most variable climate in the world. The present study aims to investigate the effectiveness of the MPI-ESM-LR model from the CMIP5 model series in predicting the monthly temperature of Iran under representative concentration pathway scenarios (RCPs) with the CORDEX-WAS project. In this research, for the historical period of 1980-2005, the daily air temperature data of 49 synoptic stations of the country and the MPI-ESM-LR model under the CORDEX project were used. Likewise, for the future period, from the predicted temperature data of RCP 8.5, RCP 4.5, and RCP 2.6 scenarios of the mentioned model in three periods of the near-future (2021-2050), mid-future (2051-2075) and far-future (2076-2100) was used. Validation of the model was done with three statistical indices: r, RMSE, and MBE. The results revealed that the model has a good performance. The slope of the temperature trend in station data and model data has been increasing in the historical period and the future period in RCP8.5 and RCP4.5 in all months, the temperature trend slope has been observed in every decade. In all months, the maximum anomaly of temperature under the scenarios studied in all three future periods can be seen in the northwest and western highlands. The eastern and southeastern regions of Iran have indicated minimum temperature anomalies, except in RCP 2.6 and RCP 8.5, respectively, the southern coasts and the northeastern heights of the country also show minimum temperature anomalies. In the cold half of the year, the minimum area of temperature anomaly has been extended to the north-western heights and low-altitude interior regions of the country.

Keywords

Main Subjects

Ahmadi, H., Azizzadeh, J., (2020). The impacts of climate change based on regional and global climate models (RCMs and GCMs) projections (case study: Ilam province). Modeling Earth Systems and Environment, 6: 685–696
Ashraf Vaghefi, S., Keykhai, M., Jahanbakhshi, F., Sheikholeslami, J., Ahmadi, A., Yang, H., Abbaspour, K.C. (2019). The future of extreme climate in Iran. Scientific Reports, 9(1464): 1-11
Bhuyan, D.I., Mohymenul, I., Bhuiyan, E.K., (2018). A Trend Analysis of Temperature and Rainfall to Predict Climate Change for Northwestern Region of Bangladesh. American Journal of Climate Change, 7: 115-134.
Carvalho, D., Cardoso Pereira, S., Rocha, A., (2020). Future surface temperature changes for the Iberian Peninsula according to EUROCORDEX climate projections. Clim. Dyn, 56(1–2): 123–138.
Cheruy, F., Dufresne, J.L., Hourdin, F., Ducharne, A., (2014). Role of clouds and land-atmosphere coupling in midlatitude continental summer warm biases and climate change amplification in CMIP5 simulations. Geophysical Research Letters, 41: 6493–6500.
Darand, M., (2020). Future changes in temperature extremes in climate variability over Iran. Meteorological Applications, 27(6): 1-16.
Di Sante, F., Coppola, E., Giorgi, F., (2021). Projections of river floods in Europe using EURO-CORDEX, CMIP5 and CMIP6 simulations. Int. J. Climatol, 41: 3203–3221.
Edwards, P.N., (2011). History of climate modeling. Wiley Interdisciplinary Reviews: Climate Change, 2: 128–139.
Eyni-Nargeseh, H., Deihimfard, R., Rahimi-Moghaddam, S., Mokhtassi-Bidgoli, A., (2019). Analysis of growth functions that can increase irrigated wheat yield under climate change. Meteorological Applications, 27(1): 1-10.
Fallah-Ghalhari, G., Shakeri, F., Dadashi-Roudbari, A., (2019). Impacts of climate changes on the maximum and minimum temperature in Iran. Theoretical and Applied Climatology, 138(3-4): 1539-1562.
Fischer, E.M., Knutti, R., (2016). Observed heavy precipitation increase confirms theory and early models. Nat. Clim. Change, 6: 986–991.
Ghazi, B., Jeihouni, E., (2022). Projection of temperature and precipitation under climate change in Tabriz, Iran. Arabian Journal of Geosciences, 15(7): DOI: 10.1007/s12517-022-09848-z.
Giorgetta, M.A., Jungclaus, J., Reick, Ch., et al (2013). Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the Coupled Model Intercomparison Project phase 5. J. Adv. Model. Earth Syst, 5: 572–597.
Guo, D.L., Wang, H.J. (2016). Comparison of a very-fine-resolution GCM with RCM dynamical downscaling in simulating climate in China. Adv. Atmos. Sci, 33: 559–570.
Hagemann, S., Göttel, H., Jacob, D., Lorenz, P., Roeckner, E., (2009). Improved regional scale processes reflected in projected hydrological changes over large European catchments. Climate Dynamics, 32(6): 767-781.
Hamed, M.M., Nashwan, M.S., Shahid, S., (2022). Inconsistency in historical simulations and future projections of temperature and rainfall: A comparison of CMIP5 and CMIP6 models over Southeast Asia. Atmospheric Research, 265: 1-14.
Hassan, I., Kalin, R.M., White, C.J., Aladejana, J.A. (2020). Selection of CMIP5 GCM Ensemble for the Projection of Spatio-Temporal Changes in Precipitation and Temperature over the Niger Delta, Nigeria. Water, 12(2), 385.
IPCC, (2013). Climate Change 2013: The Physical Science Basis. Cambridge University Press, 1535 pp.
Kohyama, T., Hartmann, D.L., Battisti, D., (2017). La Niña–like Mean-State Response to Global Warming and Potential Oceanic Roles. Journal of Climate, 30(11): 4207-4225.
Miri, M., Masoompour Samakosh, J., Raziei, T., Jalilian, A., Mahmodi, M., (2021). Spatial and Temporal Variability of Temperature in Iran for the Twenty-First Century Foreseen by the CMIP5 GCM Models. Pure and Applied Geophysics, 178: 169-184.
Muller, W.A., Baehr, J., Haak, H., Jungclaus, J.H., Kroger, J., Matei, D., et al, (2012). Forecast skill of multi-year seasonal means in the decadal prediction system of the Max Planck Institute for Meteorology. Geophysical Research Letters, 39 (22): 1-7.
Myhre, G., Alterskjær, K., Stjern, C.W. et al. (2019). Frequency of extreme precipitation increases extensively with event rareness under global warming. Scientific Reports, 9: 1-10.
Nayak, S., Mandal, M., Maity, S., (2018). RegCM4 simulation with AVHRR land use data towards temperature and precipitation climatology over Indian region. Atmospheric Research, 214(1): 163-173.
Ndiaye, PM., Bodian, A., Diop, L., Dezetter, A., Guilpart, E., Deme, A., Ogilvie, A. (2021). Future trend and sensitivity analysis of evapotranspiration in the Senegal River Basin. Journal of Hydrology: Regional Studies, 35: 1-23.
Pathak, R., Sahany, S., Mishra, S. K., Dash, S.K., (2019). Precipitation biases in CMIP5 models over the South Asian Region. Scientific Reports, 9(1): 1-13.
Rahimi, J., Laux, P., Khalili, A. (2020). Assessment of climate change over Iran: CMIP5 results and their presentation in terms of Koppen–Geiger climate zones. Theor Appl Climatol, 141: 183–199.
Rehman, N., Adnan, M., Ali, S. (2018). Assessment of CMIP5 climate models over South Asia and climate change projections over Pakistan under representative concentration pathways. International Journal of Global Warming, 16 (4): 381-415.
Shakeri, H., Motiee, H., McBean, E. (2020). Projection of important climate variables in large cities under the CMIP5–RCP scenarios using SDSM and fuzzy downscaling models. Journal of Water and Climate Change, 1802-1823.
Shi, Y., Wang, G., Gao, X.J. (2018). Role of resolution in regional climate change projections over China. Climate Dyn, 51: 2375–2396.
Shrestha, S., Bajracharya, AR., Mukand, S.B. (2016). Assessment of risks due to climate change for the Upper Tamakoshi Hydropower Project in Nepal. Climate Risk Management, 14: 27–41.
Su, F., Duan, X., Chen, D., Hao, Z., Cuo, L. (2013). Evaluation of the Global Climate Models in the CMIP5 over the Tibetan Plateau. Journal of climate, 26: 3187-3208.
Taylor, K.E., Stouffer, R.J., Meehl, G.A. (2012). An Overview of CMIP5 and the Experiment Design. Bulletin of the American Meteorological Society, 93: 485–498.
Usta, D.F.B., Teymouri, M., Chatterjee, U. (2022). Assessment of temperature changes over Iran during the twenty-first century using CMIP6 models under SSP1-26, SSP2-4.5, and SSP5-8.5 scenarios. Arabian Journal of Geosciences, 15 (416), doi.org/10.1007/s12517-022-09709-9.
Wang, C., Zhang, L., Lee, S.K., Wu, L., Mechoso, C. (2014). A global perspective on CMIP5 climate model biases. Nature Climate Change, 201–205.
Yan, L., Liu, X. (2014). Has climatic warming over the Tibetan Plateau paused or continued in recent years. J. Earth Ocean Atmos. Sci, 1(1): 13-28.
Yang, X., Wood, E.F., Sheffield, J., Ren, L., Zhang, M., Wang, Y., (2018). Bias correction of historical and future simulations of precipitation and temperature for China from CMIP5 models. Journal of Hydrometeorology, 19(3): 609-623.
Zhang, D.F., Han, Z.Y., Shi, Y. (2017). Comparison of climate projections between driving CSIRO-MK3.6.0 and downscaling simulation of RegCM4.4 over China. Advances in Climate Change Research, 8(4): 245-255