Projection changes of extreme precipitation with different return periods in Iran based on the ensemble approach of 10 CMIP6 models in the near future

جغرافیا و مخاطرات محیطی

Article 9, Volume 13, Issue 3 - Serial Number 51, November 2024, Pages 214-246   

Document Type: Research Article

DOI: 10.22067/geoeh.2024.86464.1456

Authors

Sakineh Khansalari¹; Seyede Atefeh Mohammadi²; Zahra Ghassabi^{* 1}; Hassan Salehi³

¹Assistant Professor in Research Institute of Meteorology and Atmospheric Science, Tehran, Iran.

²Research Institute of Meteorology and Atmospheric Science, Tehran, Iran.

³Kohgiluyeh and Boyer-Ahmad province Meteorological Administration, Yasuj, Iran.

Abstract

In the current study, changes in the amount of extreme precipitation with different return periods for the period 2026–2050 were analyzed using the weighted combination of 10 CMIP6 models under different scenarios. The spatial and temporal ranking of the historical simulation performance of the 10 CMIP6 models in Iran was used to determine the weights for each model. Subsequently, a rank-based weighting method was employed to project extreme precipitation levels in the study area.
For extreme precipitation analysis, the best statistical distribution was selected for each station based on historical data. In 84% of the stations, the Log-Pearson Type 3 distribution was identified as the best fit using the chi-square test for both the historical period (1990–2014) and future scenarios.
A comparison between the results of extreme precipitation for the historical and future periods revealed that the percentage of change in projected extreme precipitation was notably higher under the SSP2-4.5 scenario compared to the other two scenarios. Moreover, with longer return periods, the percentage increase in extreme precipitation was greater, and the spatial extent of its occurrence also expanded. The greatest increases in projected extreme precipitation, exceeding 25%, were observed in the SSP1-2.6 scenario in Gorgan, Babolsar, Bojnord, Arak, Isfahan, and Zahedan stations. In the SSP2-4.5 scenario, the largest increases were recorded in Gorgan, Sanandaj, Hamedan, Arak, Kashan, Isfahan, Shiraz, Fasa, Minab, Bushehr, Bandar Abbas, Bandar Lengeh, and Abu Musi stations. Under the SSP5-8.5 scenario, the greatest increases occurred in Bojnord, Birjand, Arak, Kashan, and Semnan stations.
A significant increase in extreme precipitation was consistently observed in Arak station across all three scenarios. For the 200-year return period, extreme precipitation at Arak station increased by approximately 70% under the SSP1-2.6 and SSP2-4.5 scenarios, and by about 50% under the SSP5-8.5 scenario.

Keywords

Extreme Precipitation Events; Climate Projection Models; Return Period Analysis; CMIP6 Models; Shared Socioeconomic Pathways (SSPs); Statistical Downscaling

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