Assessment of future variability in extreme precipitation and the potential effects on the wadi flow regime

• Published in: Environmental monitoring and assessment 2015-10, Vol.187 (10), p.626-626, Article 626
• Main Authors: Gunawardhana, Luminda Niroshana, Al-Rawas, Ghazi A., Kazama, So, Al-Najar, Khalid A.
• Format: Article
• Language: English
• Subjects: 21st century; Airports; Atmospheric Protection/Air Quality Control/Air Pollution; Catchment areas; Climate Change; Drought; Earth and Environmental Science; Ecology; Ecotoxicology; Environment; Environmental Management; Environmental monitoring; Environmental Monitoring - methods; Extreme weather; Flood control; Floods; Flow duration; Forecasting; General circulation models; High flow; Hydrology; Models, Theoretical; Monitoring/Environmental Analysis; Oman; Precipitation; Rain; Rainfall-runoff relationships; Runoff; Temperature
• ISSN: 0167-6369; 1573-2959
• DOI: 10.1007/s10661-015-4851-5

The objective of this study is to investigate how the magnitude and occurrence of extreme precipitation events are affected by climate change and to predict the subsequent impacts on the wadi flow regime in the Al-Khod catchment area, Muscat, Oman. The tank model, a lumped-parameter rainfall-runoff model, was used to simulate the wadi flow. Precipitation extremes and their potential future changes were predicted using six-member ensembles of general circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5). Yearly maxima of the daily precipitation and wadi flow for varying return periods were compared for observed and projected data by fitting the generalized extreme value (GEV) distribution function. Flow duration curves (FDC) were developed and compared for the observed and projected wadi flows. The results indicate that extreme precipitation events consistently increase by the middle of the twenty-first century for all return periods (49–52 %), but changes may become more profound by the end of the twenty-first century (81–101 %). Consequently, the relative change in extreme wadi flow is greater than twofolds for all of the return periods in the late twenty-first century compared to the relative changes that occur in the mid-century period. Precipitation analysis further suggests that greater than 50 % of the precipitation may be associated with extreme events in the future. The FDC analysis reveals that changes in low-to-moderate flows (Q60–Q90) may not be statistically significant, whereas increases in high flows (Q5) are statistically robust (20 and 25 % for the mid- and late-century periods, respectively).