Evaporation variability of Nam Co Lake in the Tibetan Plateau and its role in recent rapid lake expansion
文献类型:期刊论文
作者 | Ma, Ning1; Szilagyi, Jozsef1; Niu, Guo-Yue1; Zhang, Yinsheng1; Zhang, Teng1; Wang, Binbin1; Wu, Yanhong1 |
刊名 | Journal of Hydrology
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出版日期 | 2016 |
卷号 | 537页码:27-35 |
关键词 | LASER-INDUCED INCANDESCENCE PARTICLE SOOT PHOTOMETER LIGHT-ABSORPTION MIXING STATE CHEMICAL-CHARACTERIZATION CHINA EMISSIONS POLLUTION EVENTS PM2.5 |
通讯作者 | Ma, Ning (ningma@itpcas.ac.cn) |
英文摘要 | Previous studies have shown that the majority of the lakes in the Tibetan Plateau (TP) started to expand rapidly since the late 1990s. However, the causes are still not well known. For Nam Co, being a closed lake with no outflow, evaporation (EL) over the lake surface is the only way water may leave the lake. Therefore, quantifying ELis key for investigating the mechanism of lake expansion in the TP. ELcan be quantified by Penman- and/or bulk-transfer-type models, requiring only net radiation, temperature, humidity and wind speed for inputs. However, interpolation of wind speed data may be laden with great uncertainty due to extremely sparse ground meteorological observations, the highly heterogeneous landscape and lake-land breeze effects. Here, evaporation of Nam Co Lake was investigated within the 1979-2012 period at a monthly time-scale using the complementary relationship lake evaporation (CRLE) model which does not require wind speed data. Validations by in-situ observations of E601B pan evaporation rates at the shore of Nam Co Lake as well as measured ELover an adjacent small lake using eddy covariance technique suggest that CRLE is capable of simulating ELwell since it implicitly considers wind effects on evaporation via its vapor transfer coefficient. The multi-year average of annual evaporation of Nam Co Lake is 635 mm. From 1979 to 2012, annual evaporation of Nam Co Lake expressed a very slight decreasing trend. However, a more significant decrease in ELoccurred during 1998-2008 at a rate of -12 mm yr-1. Based on water-level readings, this significant decrease in lake evaporation was found to be responsible for approximately 4% of the reported rapid water level increase and areal expansion of Nam Co Lake during the same period. © 2016 Elsevier B.V. |
学科主题 | Engineering; Geology; Water Resources |
类目[WOS] | Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources |
收录类别 | SCI ; EI |
语种 | 英语 |
WOS记录号 | WOS:20161302168578 |
源URL | [http://ir.radi.ac.cn/handle/183411/39560] ![]() |
专题 | 遥感与数字地球研究所_SCI/EI期刊论文_期刊论文 |
作者单位 | 1. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China 2. Department of Hydrology and Water Resources, University of Arizona, Tucson 3.AZ, United States 4. University of Chinese Academy of Sciences, Beijing, China 5. Department of Hydraulic and Water Resources Engineering, Budapest University of Technology and Economics, Budapest, Hungary 6. School of Natural Resources, University of Nebraska-Lincoln, Lincoln 7.NE, United States 8. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China 9. Key Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing, China |
推荐引用方式 GB/T 7714 | Ma, Ning,Szilagyi, Jozsef,Niu, Guo-Yue,et al. Evaporation variability of Nam Co Lake in the Tibetan Plateau and its role in recent rapid lake expansion[J]. Journal of Hydrology,2016,537:27-35. |
APA | Ma, Ning.,Szilagyi, Jozsef.,Niu, Guo-Yue.,Zhang, Yinsheng.,Zhang, Teng.,...&Wu, Yanhong.(2016).Evaporation variability of Nam Co Lake in the Tibetan Plateau and its role in recent rapid lake expansion.Journal of Hydrology,537,27-35. |
MLA | Ma, Ning,et al."Evaporation variability of Nam Co Lake in the Tibetan Plateau and its role in recent rapid lake expansion".Journal of Hydrology 537(2016):27-35. |
入库方式: OAI收割
来源:遥感与数字地球研究所
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