An overview of the atmospheric moisture transport effect on stable isotopes (δ18O, δ 2H) and D excess contents of precipitation in Iran

• Published in: Theoretical and applied climatology Vol. 138; no. 1-2; pp. 47 - 63
• Main Authors: Heydarizad, Mojtaba, Raeisi, Ezzat, Sori, Rogert, Gimeno, Luis
• Format: Journal Article
• Language: English
• Published: Vienna Springer Vienna 01.10.2019; Springer Nature B.V
• Subjects: Air masses; Aquatic Pollution; Atmospheric models; Atmospheric moisture; Atmospheric Protection/Air Quality Control/Air Pollution; Atmospheric Sciences; Climate science; Climatology; Drought; Earth and Environmental Science; Earth Sciences; High seas; Isotopes; Meteoric water; Moisture; Original Paper; Population growth; Population studies; Precipitation; Sea surface; Sea surface temperature; Stable isotopes; Stations; Surface temperature; Trajectories; Waste Water Technology; Water; Water Management; Water Pollution Control; Water shortages; Water temperature; Iran; Persian Gulf; Precipitation; HYSPLIT model; Iran; Moisture source; Stable isotopes
• ISSN: 0177-798X; 1434-4483
• DOI: 10.1007/s00704-019-02798-9

Iran faces a water shortage crisis due to its long and frequent droughts and rapid population growth. In this study, moisture sources have been determined in 161 precipitation events from 12 stations using a Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model. Ten main moisture sources have been identified among which the Persian Gulf and the Persian Gulf with terrestrial sources are dominant. Backward trajectory outputs demonstrate that the precipitation events in the stations in the north of Iran originate mostly from the Caspian Sea and terrestrial sources. These precipitation events are mostly plotted on the Global Meteoric Water Line (GMWL) or between GMWL and Eastern Mediterranean Meteoric Water Line (EMMWL). Precipitation events in the middle and south of Iran stations receive moisture mostly from the Persian Gulf and terrestrial sources and they are mostly plotted on EMMWL. Linking backward trajectory models with precipitation events (δ 18 O and δ 2 H) determines the general isotope characteristics of each moisture source. Most of the precipitation events originate from high sea surface temperature (SST) water bodies and are plotted on EMMWL. However, precipitation events originating from lower SST water bodies are mostly plotted on GMWL and between GMWL and EMMWL. Plotting the average (δ 18 O and δ 2 H) in the studied stations on the meteoric water lines of the regions located on the dominant air masses trajectories toward Iran confirms the dominant moisture sources for the studied stations and also other obtained results by stable isotope technique and HYSPLIT model in this study.