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DOI | 10.1002/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 |
ISSN | 0885-6087 |
EISSN | 1099-1085 |
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
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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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