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DOI10.1002/hyp.11420
When to conduct an isotopic survey for lake water balance evaluation in highly seasonal climates
Cui, Jiangpeng; Tian, Lide; Gibson, John J.
通讯作者Tian, LD (通讯作者)
发表日期2018
ISSN0885-6087
EISSN1099-1085
起始页码379
结束页码387
卷号32期号:3
英文摘要One-time or short-term lake water isotopic surveys are often employed to evaluate regional lake water balance. However, it can be difficult to determine the optimal time-window for sampling to obtain a representative long-term perspective of lake water balance in settings influenced by seasonal variations in precipitation, evaporative loss, glacial/snow meltwater, and larger seasonal shifts in isotopic composition of precipitation. This is especially true for areas of the Tibetan Plateau that are influenced by the summer Indian monsoon. Although high-frequency sampling is always preferred as the most rigorous approach to characterize the water budget of lakes or watersheds, this may be impractical in remote regions and over large spatial scales. To assess the potential sensitivity of isotope balance characterization to seasonal variability, we used a weekly lake water isotope data set acquired over a period of 3years on the Tibetan Plateau to evaluate the potential inaccuracies that might have arisen from using isotopic data collected during narrower time-windows. For this assessment, we use weekly isotopic data collected during the study and assume that these sampling events were stand-alone one-time surveys. We then demonstrate the sensitivity of the isotope balance method in this setting, particularly for the rainy season that significantly underestimated the evaporation/inflow. In contrast, isotopic composition of the lake water was found to be more representative of long-term conditions when sampled in October on the Tibetan Plateau. To broaden our evaluation of seasonality effects over a range of climatic zones, published high-frequency isotopic data were also compiled, and a similar assessment was carried out for selected regions of the world. The synthesized data and model outputs, which confirm pronounced variations in lake water isotopic composition and evaporation/inflow across a range of seasonal climates, were used to determine optimal sampling windows for these specific regions.
关键词SOUTHERN TIBETAN PLATEAUSTABLE-ISOTOPEMASS-BALANCEHYDROGEN ISOTOPESDEUTERIUM-EXCESSNORTHERN CANADAUNITED-STATESEVAPORATIONDELTA-O-18OXYGEN
英文关键词isotopic survey; lake water balance; optimal sampling date; seasonal climate
语种英语
WOS研究方向Water Resources
WOS类目Water Resources
WOS记录号WOS:000423341300005
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/259305
推荐引用方式
GB/T 7714
Cui, Jiangpeng,Tian, Lide,Gibson, John J.. When to conduct an isotopic survey for lake water balance evaluation in highly seasonal climates[J]. 中国科学院青藏高原研究所,2018,32(3).
APA Cui, Jiangpeng,Tian, Lide,&Gibson, John J..(2018).When to conduct an isotopic survey for lake water balance evaluation in highly seasonal climates.HYDROLOGICAL PROCESSES,32(3).
MLA Cui, Jiangpeng,et al."When to conduct an isotopic survey for lake water balance evaluation in highly seasonal climates".HYDROLOGICAL PROCESSES 32.3(2018).
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