Climate Change Data Portal
DOI | 10.1111/jawr.12286 |
The Mass and Energy Exchange of a Tibetan Glacier: Distributed Modeling and Climate Sensitivity | |
Li, Binquan; Acharya, Kumud; Yu, Zhongbo; Liang, Zhongmin; Su, Fengge | |
通讯作者 | Li, BQ (通讯作者) |
发表日期 | 2015 |
ISSN | 1093-474X |
EISSN | 1752-1688 |
起始页码 | 1088 |
结束页码 | 1100 |
卷号 | 51期号:4 |
英文摘要 | Most glaciers in the Tibetan Plateau (TP) are not closely monitored for mass balance (MB) due to their inaccessibility, which makes it difficult to better understand the dynamics of glacial advancement or retreat. Surface energy budget, MB, and the resulting melt runoff were calculated for Zhadang glacier (5,710m above sea level) of the central TP. Energy balance was calculated on 30-m square grids for the summers of 2007 and 2008. On average, net radiation dominated the total energy source (66%) while the residual was supplied by sensible heat flux. More than 67% of the energy sink was available for melting on the glacier. Thus, less than 33% of the total energy was consumed by latent heat flux. A large and a slightly negative summer MB were calculated for the2007 and 2008 summers, respectively. The high sensitivity of the glacier to air temperature may indicate that the lower than average seasonal temperature was more important than the increased precipitation for the slightly negative MB in the summer of 2008. Comparisons of glacial melt runoff indicated that rainfall and snowmelt were the dominant contribution to total runoff in the glacierized basin and the ice melting is also very important. Glacial melt calculation provides a basis for quantifying glacial melt-runoff contribution to the river streamflow in the TP. |
关键词 | NAM CO BASINZHADANG GLACIERGLOBAL RADIATIONBALANCEMELTSURFACESTORGLACIARENTEMPERATUREICE |
英文关键词 | glacial mass balance; precipitation; runoff; climate variability; Tibetan Plateau |
语种 | 英语 |
WOS研究方向 | Engineering ; Geology ; Water Resources |
WOS类目 | Engineering, Environmental ; Geosciences, Multidisciplinary ; Water Resources |
WOS记录号 | WOS:000359017800016 |
来源期刊 | JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION |
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/258560 |
推荐引用方式 GB/T 7714 | Li, Binquan,Acharya, Kumud,Yu, Zhongbo,et al. The Mass and Energy Exchange of a Tibetan Glacier: Distributed Modeling and Climate Sensitivity[J]. 中国科学院青藏高原研究所,2015,51(4). |
APA | Li, Binquan,Acharya, Kumud,Yu, Zhongbo,Liang, Zhongmin,&Su, Fengge.(2015).The Mass and Energy Exchange of a Tibetan Glacier: Distributed Modeling and Climate Sensitivity.JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION,51(4). |
MLA | Li, Binquan,et al."The Mass and Energy Exchange of a Tibetan Glacier: Distributed Modeling and Climate Sensitivity".JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION 51.4(2015). |
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