| نویسندگان | Carlo De Michele |
| نشریه | Acta Geophysica |
| شماره صفحات | 1-16 |
| شماره سریال | 73 |
| شماره مجلد | 3 |
| ضریب تاثیر (IF) | 0.91 |
| نوع مقاله | Full Paper |
| تاریخ انتشار | 2025 |
| نوع نشریه | چاپی |
| کشور محل چاپ | هلند |
| نمایه نشریه | ISI،JCR،Scopus |
چکیده مقاله
The quantity and quality of water resources are significantly impacted by climate change. In this research, the performance of 26
climate models used for predicting precipitation in the baseline period (1988–2018) was evaluated, and the models were ranked
and weighted. Then, an analysis was conducted on the trend of precipitation changes during the period of 2031 to 2050 under the
SSP1-2.6, SSP2-4.5, and SSP5-8.5 scenarios. The LARS-WG 7.0 model was implemented for the downscaling of precipitation
data of the GCM models. Additionally, a comparison was made between the scenarios and models of the Sixth Assessment Report
(AR6) in estimating future precipitation. Furthermore, besides investigating the certainty of model results regarding precipitation,
the uncertainty of precipitation in different months of the year was examined. Six models with the best performance—MIROC6,
INM-CM5-0, FGOALS-G3, KACE-1–0-G, BCC-CSM2-MR, and INM-CM4-8—were selected after evaluating their performance
and ranking in the baseline period using four evaluation criteria: R2,
RMSE, NSE, and CRM. Consequently, the prediction results
from these six models were utilized to monitor precipitation changes during the future period (2031–2050). The KACE-1–0-G
model under the SSP5-8.5 scenario is predicted to have the highest increase in precipitation compared to the baseline period,
with a difference of 34.7 mm occurring in April. Similarly, the MIROC6 model under the SSP5-8.5 scenario is projected to have
the highest decrease in precipitation compared to the baseline period, with a difference of 26 mm in May. The results show that
annual precipitation will decrease under all three scenarios compared to the baseline period. Under the SSP5-8.5 scenario, annual
precipitation is estimated at 261.3 mm, while under the SSP2-4.5 scenario, it is 264.6 mm, and under the SSP1-2.6 scenario, it is
290.9 mm. When comparing uncertainty, February has the lowest uncertainty in estimating precipitation under all three scenarios
due to having a higher bandwidth range for predictions. August experiences the lowest precipitation change, while February
has the highest precipitation change. In terms of model uncertainty comparison across all three scenarios, it was found that the
MIROC6 model exhibits less uncertainty due to having a lowest bandwidth range for predictions.
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