Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling
文献类型：期刊论文
| 作者 | Cui, JP (Cui, Jiangpeng)1,2; Tian, LD (Tian, Lide)1,3,4; Biggs, TW (Biggs, Trent W.)5; Wen, R (Wen, Rong)1; Tian, LD |
| 刊名 | HYDROLOGICAL PROCESSES
 |
| 出版日期 | 2017 |
| 卷号 | 31期号:5页码:1034-1046 |
| 关键词 | ISOTOPE MASS-BALANCE SOUTHERN TIBETAN PLATEAU STABLE-ISOTOPES GREAT-LAKES HYDROGEN ISOTOPES SATELLITE DATA CLIMATE-CHANGE UNITED-STATES RIVER-BASIN DELTA-D |
| DOI | 10.1002/hyp.11085 |
| 文献子类 | Article |
| 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. |
| 学科主题 | 自然地理学 |
| WOS研究方向 | Water Resources |
| 语种 | 英语 |
| WOS记录号 | WOS:000394901800006 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/8328]  |
| 专题 | 青藏高原研究所_图书馆 |
| 通讯作者 | Tian, LD |
| 作者单位 | 1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Plateau Environm Change & Land Su, Beijing 100101, Peoples R China. 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China. 3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China. 4.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China. 5.San Diego State Univ, Dept Geog, 5500 Campanile Dr, San Diego, CA 92182 USA. |
| 推荐引用方式 GB/T 7714 | Cui, JP ,Tian, LD ,Biggs, TW ,et al. Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling[J]. HYDROLOGICAL PROCESSES,2017,31(5):1034-1046. |
| APA | Cui, JP ,Tian, LD ,Biggs, TW ,Wen, R ,&Tian, LD.(2017).Deuterium-excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling.HYDROLOGICAL PROCESSES,31(5),1034-1046. |
| MLA | Cui, JP ,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):1034-1046. |
入库方式： OAI收割
来源：青藏高原研究所
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