Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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
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ISSN | 1352-2310 |
EISSN | 1873-2844 |
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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