Arid
DOI10.1016/j.atmosenv.2019.116892
Chemo-isotopes (O-18 & H-2) signatures and HYSPLIT model application: Clues to the atmospheric moisture and air mass origins
Bagheri, Rahim; Bagheri, Fatemeh; Karami, Gholam Hossein; Jafari, Hadi
通讯作者Bagheri, Rahim
来源期刊ATMOSPHERIC ENVIRONMENT
ISSN1352-2310
EISSN1873-2844
出版年2019
卷号215
英文摘要The first ever systematic study on spatio-temporal variation of the chemo-isotopic compositions of the precipitation in Iran was carried out in a hydrological year (2016-2017) at 7 sites located in Bojnourd area, northeast of Iran. The main aims were to determine the moisture and air mass sources and, in particular, to evaluate the effect of atmospheric conditions on isotope compositions. The isotopic value of the precipitation fluctuates seasonally with higher values in summer and lower values in winter at the all sites. Stable isotope values of the precipitation samples within the local scale resulted a Bojnourd meteoric water line (BMWL): delta D = 6.4 x delta O-18 + 1.2 (R-2 = 0.93, n = 75), with a lower slope and intercept than the global meteoric water line (GMWL) due to isotope kinetic fractionation effects during precipitation in semi-arid region with lower humidity. The air temperature can be suggested as the main controlling factor that impacts the stable isotope compositions of precipitation in the study area. The large rainfall events totally displayed the highest slope, intercept and d-excess values nearly similar to the snowfall samples, indicating the re-evaporation effects on the low rainfall amounts. Precipitations during summer season (Jun-August) with higher isotopes and lower d-excess values mainly originated from the polar and Caspian Sea air moistures. While, moisture contributing to high d-excess and low isotope precipitation during January was mainly transported by the Mediterranean air moisture. The air-mass trajectories that affect the precipitation in autumn (September-December) and spring (March-May) displayed multiple sources, originating from the polar, Mediterranean and Caspian Sea air moistures. Trajectory analysis by HYSPLIT modeling allowed the association of moisture sources with the isotopic compositions of the precipitation. Based on the sea salt contribution for Na+ and Cl-, a sea effect is recognized especially from Caspian Sea and Mediterranean region, despite the long distance at the present study. The correlation between EC and the ions indicate that ion compositions in the precipitation and atmosphere of the study area are mainly effected by dust of soil and sea salt and to some extent from secondary evaporation during rainfall. The hydrochemical investigations confirmed the air masses trajectories which resulted from the isotopic characteristics.
英文关键词Stable isotopes Meteoric water line Precipitation source Iran
类型Article
语种英语
国家Iran
收录类别SCI-E
WOS记录号WOS:000487567600008
WOS关键词CHEMICAL-COMPOSITION ; STABLE-ISOTOPES ; WATER-VAPOR ; DEUTERIUM EXCESS ; WET DEPOSITION ; DELTA-D ; PRECIPITATION ; RAINWATER ; CHINA ; HYDROCHEMISTRY
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/214513
作者单位Shahrood Univ Technol, Fac Earth Sci, Shahrood, Iran
推荐引用方式
GB/T 7714
Bagheri, Rahim,Bagheri, Fatemeh,Karami, Gholam Hossein,et al. Chemo-isotopes (O-18 & H-2) signatures and HYSPLIT model application: Clues to the atmospheric moisture and air mass origins[J],2019,215.
APA Bagheri, Rahim,Bagheri, Fatemeh,Karami, Gholam Hossein,&Jafari, Hadi.(2019).Chemo-isotopes (O-18 & H-2) signatures and HYSPLIT model application: Clues to the atmospheric moisture and air mass origins.ATMOSPHERIC ENVIRONMENT,215.
MLA Bagheri, Rahim,et al."Chemo-isotopes (O-18 & H-2) signatures and HYSPLIT model application: Clues to the atmospheric moisture and air mass origins".ATMOSPHERIC ENVIRONMENT 215(2019).
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