Akbar Rahmati

Mr. Akbar Rahmati

orcid

Research Focus & Metrics

Academic Career Length

6Years (2021-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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22 May 2022 in Water
Verified
Journal Article
Open access
PDF file
ABAydin Bakhtar
Aydin Bakhtar
ARAkbar Rahmati
Akbar Rahmati
Afshin Shayeghi MoghanlouAfshin Shayeghi Moghanlou
Afshin Shayeghi Moghanlou
JTJavad Teymoori
Javad Teymoori
NGNavid Ghajarnia
Navid Ghajarnia
PSPeyman Saemian
Peyman Saemian
Extreme precipitation events such as floods and droughts have occurred with higher frequency over the recent decades as a result of the climate change and anthropogenic activities. To understand and mitigate such events, it is crucial to investigate their spatio-temporal variations globally or regionally. Global precipitation products provide an alternative way to the in situ observations over such a region. In this study, we have evaluated the performance of the latest version of the Global Precipitation Measurement-Integrated Multi-satellitE Retrievals (GPM-IMERGV6.0 Final Run (GPM-IMERGF)). To this end, we have employed ten most common extreme precipitation indices, including maximum indices (Rx1day, Rx5day, CDD, and CWD), percentile indices (R95pTOT and R99pTOT), and absolute threshold indices (R10mm, R20mm, SDII, and PRCPTOT). Overall, the spatial distribution results for error metrics showed that the highest and lowest accuracy for GPM-IMERGF were reported for the absolute threshold indices and percentile indices, respectively. Considering the spatial distribution of the results, the highest accuracy of GPM-IMERGF in capturing extreme precipitations was observed over the western highlands, while the worst results were obtained along the Caspian Sea regions. Our analysis can significantly contribute to various hydro-metrological applications for the study region, including identifying drought and flood-prone areas and water resources planning.

21 November 2022 in Journal of Hydrology: Regional Studies
Verified
Journal Article
Open access
ARAkbar Rahmati
Akbar Rahmati
ABAydin Bakhtar
Aydin Bakhtar
Afshin Shayeghi MoghanlouAfshin Shayeghi Moghanlou
Afshin Shayeghi Moghanlou
Zahra KalantariZahra Kalantari
Zahra Kalantari
ABAlireza Massah Bavani
Alireza Massah Bavani
NGNavid Ghajarnia
Navid Ghajarnia

3 September 2021 in ESS Open Archive
Verified
Preprint
Open access
ARAkbar Rahmati
Akbar Rahmati
ABAydin Bakhtar
Aydin Bakhtar
Afshin Shayeghi MoghanlouAfshin Shayeghi Moghanlou
Afshin Shayeghi Moghanlou
Zahra KalantariZahra Kalantari
Zahra Kalantari
ABAli Reza Massah Bavani
Ali Reza Massah Bavani
NGNavid Ghajarnia
Navid Ghajarnia
Access to spatio-temporally consistent precipitation data is a key prerequisite for hydrological studies, especially in data-scarce regions. Different global precipitation products offer an alternative way to estimate precipitation over areas with inadequate gauge distributions. However, before use of the datasets, the accuracy of these global estimations must be carefully studied at local and regional scale. This study evaluated 14 global precipitation products against gauge observations 2003-2012 in Karun and Karkheh basins in southwest Iran. Different categorical and statistical indices, including Kling-Gupta Efficiency (KGE), bias, correlation coefficient, and variability ratio, at varying spatial and temporal resolution were used to evaluate the products. KGE results at both daily and monthly time steps suggested that TMPA-3B42V7.0 and MERRA-2 outperformed all other products, while CMORPH-BLDV1.0 and PERSIANN-CDR was the best-performing product at daily and monthly time steps, respectively. ERA5-Land showed the highest positive bias compared with in-situ observations, particularly for mountainous southeastern parts of Karun basin. Overall, bias-adjusted products obtained by merging ground-based observations in the estimations outperformed the unadjusted versions. The spatial distribution of statistical error metrics indicated that almost all products showed their greatest uncertainties for mountainous regions, due to complex precipitation processes in these regions. These results can significantly contribute to various horological and water resources planning measures in the study region, including early flood warning systems, drought monitoring, and optimal dam operations.

1 August 2026 in Journal of Hydrometeorology
Verified
Journal Article
Closed access
ARAkbar Rahmati
Akbar Rahmati
YMYannis Markonis
Yannis Markonis
MHMartin Hanel
Martin Hanel
CLChristos J. Lolis
Christos J. Lolis
AAAmir AghaKouchak
Amir AghaKouchak
Reliable assessment of Mediterranean precipitation remains challenging because gridded datasets differ in their construction, observational constraints, and representation of strong spatial variability. Although station-based studies show that precipitation characteristics and trends vary across the region, widely used gridded products have not been consistently evaluated against extensive station-derived references. Here, we assess seven products for 1981–2020 against two complementary station-derived benchmarks using mean annual precipitation, interannual variability, long-term slope, and annual maximum 1-day precipitation. The benchmarks combine published statistics from more than 23 000 stations in 27 countries with extreme precipitation records from HYADES (Archive of Yearly Maxima of Daily Precipitation Records), a global archive of annual maximum daily precipitation (RX1DAY) derived from Global Historical Climatology Network-Daily observations. After aggregation, the reference network represents 2096 grid cells and covers 52% of nondesert land cells in the study domain. Multi-Source Weighted-Ensemble Precipitation (MSWEP), Multi-Source Weather (MSWX), and the Global Precipitation Climatology Centre (GPCC) product show the most consistent performance for mean precipitation, variability, and slope. Across matched grid cells, typical product-level root-mean-square errors against the station-derived references are 60–80 mm for mean annual precipitation, 25 mm for interannual variability, and 1.5 mm yr −1 for slope. For RX1DAY, the European daily high-resolution gridded dataset (E-OBS) performs best ( R 2 = 0.57), whereas the other products reach 0.18–0.30 and generally underestimate the strongest extremes. A separate analysis for 2001–20 shows stronger product agreement for precipitation changes associated with wet-day frequency than with wet-day intensity. These findings support more informed dataset selection for Mediterranean drought, flood, and water resource assessments. Significance Statement: Global datasets are widely used to study changes in Mediterranean precipitation, but they do not describe precipitation equally well. We find that Multi-Source Weighted-Ensemble Precipitation (MSWEP), Multi-Source Weather (MSWX), and Global Precipitation Climatology Centre (GPCC) best represent average conditions and year-to-year variability across the region. European daily high-resolution gridded dataset (E-OBS) captures annual daily extremes more closely than the other products, although all datasets fail to capture the strongest events. Agreement is much weaker for long-term slopes, indicating greater interproduct uncertainty in estimated temporal changes than in mean-state precipitation characteristics. These differences mean that conclusions about drought risk, flood potential, and water availability can vary depending on the dataset used. Our results support more careful dataset selection in climate assessments and practical planning for water resources and related hazards across the Mediterranean region.

29 January 2026 in Environmental Modelling & Software
Verified
Journal Article
Closed access
ARAkbar Rahmati
Akbar Rahmati
MGMijael Rodrigo Vargas Godoy
Mijael Rodrigo Vargas Godoy
VTVishal Thakur
Vishal Thakur
JTJohanna R. Thomson
Johanna R. Thomson
MHMartin Hanel
Martin Hanel
YMYannis Markonis
Yannis Markonis

29 November 2023
Verified
Dataset
Closed access
ARAkbar Rahmati
Akbar Rahmati
MGMijael Rodrigo Vargas Godoy
Mijael Rodrigo Vargas Godoy
YMYannis Markonis
Yannis Markonis