Al‐Nassar et al. (2026) On the Temporal Variability of Precipitation in Iraq: Arid‐Wet Years and Extreme Events
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: International Journal of Climatology
- Year: 2026
- Date: 2026-04-06
- Authors: Ali Raheem Al‐Nassar, Josep Lluís Pelegrí, P. Masciangioli
- DOI: 10.1002/joc.70350
Research Groups
Not explicitly stated in the abstract.
Short Summary
This study analyzes long-term precipitation variability in Iraq, distinguishing between arid and wet years and characterizing extreme events, revealing that the Indian Ocean Dipole (IOD) significantly influences interannual variability by modulating autumn-winter moisture arrival.
Objective
- To examine the variability of precipitation in Iraq, focusing on the differences between arid and wet years and characterizing the intensity and synoptic drivers of extreme precipitation events.
Study Configuration
- Spatial Scale: Iraq (country-wide weighted mean, specific stations: Mosul, Rutba, Baghdad, Basrah).
- Temporal Scale:
- Monthly precipitation records: 84 years (1938–2023, excluding 2003 and 2004).
- Daily precipitation records (Baghdad): 19 years (2005–2023).
- Extreme value analysis for return periods up to 100 years.
Methodology and Data
- Models used:
- Extreme value analysis (Peak Over Threshold (POT), Block Maxima (BM))
- Probability Density Function (PDF) analysis
- Correlation analysis
- Data sources:
- Long-term station precipitation records (monthly from four stations, daily from Baghdad).
- Reanalysis weather data.
- Indian Ocean Dipole (IOD) index.
Main Results
- Annual precipitation (mean ± standard deviation) values were: Mosul (367 ± 140 mm), Rutba (107 ± 59 mm), Baghdad (138 ± 65 mm), and Basrah (136 ± 60 mm), with a weighted mean for Iraq of 182 ± 57 mm.
- Precipitation time series exhibit strong seasonality (maximum in winter, negligible in summer) and interannual variations spanning an order of magnitude.
- Arid and wet years, defined by annual precipitation below the 25th and above the 75th percentiles respectively, show substantial differences in their seasonal cycles.
- Monthly precipitation is significantly correlated with the Indian Ocean Dipole (IOD) index, indicating that IOD enhances autumn-winter precipitation by influencing moisture transport from the Red Sea, Arabian Sea, and Persian Gulf.
- 36 extreme precipitation events were identified in Baghdad (2005–2023), contributing 1452 mm (56%) of the total precipitation for that period, and were classified as jet streak, cut-off low, upper-air trough, or Rex block events.
- The frequency of extreme events does not increase during wet years, suggesting that seasonal IOD conditioning is the primary driver of arid-wet year variability.
- Extreme value analysis for daily data showed POT provided narrower high-confidence bands compared to BM, while for monthly data, both methods yielded similar mean and high-confidence values for return periods up to 100 years.
Contributions
- Provides a comprehensive, long-term analysis of precipitation variability across Iraq, including quantitative characterization of arid/wet years and extreme events.
- Establishes a significant correlation between monthly precipitation in Iraq and the Indian Ocean Dipole (IOD), identifying a key climatic driver for interannual variability.
- Classifies and quantifies the contribution of specific synoptic weather patterns (e.g., jet streak, cut-off low) to extreme precipitation events in the region.
- Offers robust extreme value analysis for both daily and monthly precipitation, providing critical return values for hydrological planning and risk assessment.
Funding
Not explicitly stated in the abstract.
Citation
@article{AlNassar2026Temporal,
author = {Al‐Nassar, Ali Raheem and Pelegrí, Josep Lluís and Masciangioli, P.},
title = {On the Temporal Variability of Precipitation in Iraq: Arid‐Wet Years and Extreme Events},
journal = {International Journal of Climatology},
year = {2026},
doi = {10.1002/joc.70350},
url = {https://doi.org/10.1002/joc.70350}
}
Original Source: https://doi.org/10.1002/joc.70350