Climate Change Data Portal
DOI | 10.1002/hyp.11085 |
Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling | |
Cui, Jiangpeng; Tian, Lide; Biggs, Trent W.; Wen, Rong | |
通讯作者 | Tian, LD (通讯作者) |
发表日期 | 2017 |
ISSN | 0885-6087 |
EISSN | 1099-1085 |
起始页码 | 1034 |
结束页码 | 1046 |
卷号 | 31期号:5 |
英文摘要 | The numerous lakes on the Tibetan Plateau play an important role in the regional hydrological cycle and water resources, but systematic observations of the lake water balance are scarce on the Tibetan Plateau. Here, we present a detailed study on the water cycle of Cona Lake, at the headwaters of the Nujiang-Salween River, based on 3 years (2011-2013) of observations of delta O-18 and delta H-2, including samples from precipitation, lake water, and outlet surface water. Short-term atmospheric water vapor was also sampled for isotope analyses. The delta H-2-delta O-18 relationship in lake water (delta H-2 = 6.67 delta O-18 - 20.37) differed from that of local precipitation (delta H-2 = 8.29 delta O-18 + 12.50), and the deuterium excess (d-excess) in the lake water (-7.5%) was significantly lower than in local precipitation (10.7%), indicating an evaporative isotope enrichment in lake water. The ratio of evaporation to inflow (E/I) of the lake water was calculated using both d-excess and delta O-18. The E/I ratios of Cona lake ranged from 0.24 to 0.27 during the 3 years. Observations of atmospheric water vapor isotopic composition (dA) improved the accuracy in E/I ratio estimate over a simple precipitation equilibrium model, though a correction factor method provided nearly identical estimates of E/I ratio. The work demonstrates the feasibility of d-excess in the study of the water cycle for lakes in other regions of the world and provides recommendations on sampling strategies for accurate calculations of E/I ratio. |
关键词 | STABLE-ISOTOPES DELTA-O-18TIBETAN PLATEAUMASS-BALANCEHYDROGEN ISOTOPESUNITED-STATESGREAT-LAKESPRECIPITATIONVAPORSOUTHAREA |
英文关键词 | deuterium excess; evaporation; lake; Tibetan Plateau; water balance |
语种 | 英语 |
WOS研究方向 | Water Resources |
WOS类目 | Water Resources |
WOS记录号 | WOS:000394901800006 |
来源期刊 | HYDROLOGICAL PROCESSES
![]() |
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/259037 |
推荐引用方式 GB/T 7714 | Cui, Jiangpeng,Tian, Lide,Biggs, Trent W.,et al. Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling[J]. 中国科学院青藏高原研究所,2017,31(5). |
APA | Cui, Jiangpeng,Tian, Lide,Biggs, Trent W.,&Wen, Rong.(2017).Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling.HYDROLOGICAL PROCESSES,31(5). |
MLA | Cui, Jiangpeng,et al."Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling".HYDROLOGICAL PROCESSES 31.5(2017). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。