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DOI | 10.1016/j.quaint.2020.09.052 |
Stable isotopes of precipitation in Nepal Himalaya highlight the topographic influence on moisture transport | |
Acharya, Sunil; Yang, Xiaoxin; Yao, Tandong; Shrestha, Dibas | |
通讯作者 | Yang, XX (通讯作者) |
发表日期 | 2020 |
ISSN | 1040-6182 |
EISSN | 1873-4553 |
起始页码 | 22 |
结束页码 | 30 |
卷号 | 565 |
英文摘要 | The Nepal Himalaya is a transition zone for pollutants transport from the South Asia onto the Tibetan Plateau, with the moist convection identified as dominating the chemical composition that would be transported onto the Plateau. Yet little is known regarding the atmospheric water vapor transport over this region, and how the summer monsoon flows would interact with local topography, with traces detectable from ground sample and observations. The stable oxygen and hydrogen isotopes in precipitation (delta O-18(p) and delta D-p) are important tracers for understanding various hydrological processes. This study reports, for the first time, stable isotope data in daily precipitation at five stations along a north-south transect on the southern slope of Himalaya, with altitudes ranging from 102 m to 5050 m above sea level (a.s.l). The altitude effect of delta O-18(p) across the region of interest is apparent with an altitudinal lapse rate as 0.17 parts per thousand/100 m. Seasonal trends in delta O-18(p) and dDp show low values during June-September and higher values during October-May at all of the study sites, with the noticeable decrease of delta O-18(p) during summer indicative of the presence of the Indian monsoon over the eastern Nepal Himalaya. The average d-excess values in the summer precipitation increase with altitudes til 3800 m a.s.l before decreasing afterward to 5050 m a.s.l. This corroborates with previous meteorological discovery in the region, and probably confirms the replacement of prevailing westerly by the southerly monsoon flows during summer monsoon season. |
关键词 | DEUTERIUM EXCESSTIBETAN PLATEAUSURFACE WATERSMONSOONSOUTHERNDELTA-O-18O-18PALEOELEVATIONSIMULATIONCONVECTION |
英文关键词 | Stable isotopes in precipitation; Altitude; Monsoon; Southern slope of himalaya |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000591580600003 |
来源期刊 | QUATERNARY INTERNATIONAL |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259889 |
推荐引用方式 GB/T 7714 | Acharya, Sunil,Yang, Xiaoxin,Yao, Tandong,et al. Stable isotopes of precipitation in Nepal Himalaya highlight the topographic influence on moisture transport[J]. 中国科学院青藏高原研究所,2020,565. |
APA | Acharya, Sunil,Yang, Xiaoxin,Yao, Tandong,&Shrestha, Dibas.(2020).Stable isotopes of precipitation in Nepal Himalaya highlight the topographic influence on moisture transport.QUATERNARY INTERNATIONAL,565. |
MLA | Acharya, Sunil,et al."Stable isotopes of precipitation in Nepal Himalaya highlight the topographic influence on moisture transport".QUATERNARY INTERNATIONAL 565(2020). |
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