Numerical simulation of the flow velocity and temperature of the Dongkemadi Glacier | |
Wu Zhen1; Liu Shiyin2; He Xiaobo2 | |
刊名 | ENVIRONMENTAL EARTH SCIENCES |
2016-03-01 | |
卷号 | 75期号:5页码:11 |
关键词 | Ice dynamic Velocity Temperature |
ISSN号 | 1866-6280 |
DOI | 10.1007/s12665-016-5262-9 |
通讯作者 | Wu Zhen(wuzhen@lzb.ac.cn) |
英文摘要 | The flow velocity and ice temperature of a glacier reflect the response of the glacier to climate change. However, because of the restrictions of observation conditions, it is often difficult to acquire the ice velocity and temperature field for the entire glacier profile. In this study, we use a two-dimensional ice flow model and energy balance model to simulate the ice velocity and temperature using field measurements made with ground penetrating radar for the profile of the small Dongkemadi Glacier, and verify the simulated surface velocity with interferometric synthetic aperture radar data. The simulation for the flow velocity shows that the velocity depends on the surface and bedrock slopes, glacier profile shape and mass supply way, and the surface velocity increases with an increase in the surface slope. Sensitivity analysis shows that the terrain and slope affect the profile velocity. Simulation results for temperature show that the ice-body temperature is highest in the lower ice body at a subglacial position altitude of 5520 m a.s.l. This location not only gathers melt water most easily but also undergoes the strongest effect of geothermal heat flow. The distributions of the ice velocity and ice-body temperature provide a good reference for research on glacier vulnerability assessment and the response of glaciers to climate change. |
收录类别 | SCI |
WOS关键词 | SHALLOW-ICE APPROXIMATION ; TIBETAN PLATEAU ; TIEN-SHAN ; MASS CONSERVATION ; SURGING GLACIER ; SHEET MODELS ; HIGHER-ORDER ; RIVER-BASIN ; DYNAMICS ; HIMALAYA |
WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Water Resources |
WOS类目 | Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources |
语种 | 英语 |
出版者 | SPRINGER |
WOS记录号 | WOS:000372171700034 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2557377 |
专题 | 寒区旱区环境与工程研究所 |
通讯作者 | Wu Zhen |
作者单位 | 1.China Earthquake Adm, Lanzhou Inst Seismol, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China |
推荐引用方式 GB/T 7714 | Wu Zhen,Liu Shiyin,He Xiaobo. Numerical simulation of the flow velocity and temperature of the Dongkemadi Glacier[J]. ENVIRONMENTAL EARTH SCIENCES,2016,75(5):11. |
APA | Wu Zhen,Liu Shiyin,&He Xiaobo.(2016).Numerical simulation of the flow velocity and temperature of the Dongkemadi Glacier.ENVIRONMENTAL EARTH SCIENCES,75(5),11. |
MLA | Wu Zhen,et al."Numerical simulation of the flow velocity and temperature of the Dongkemadi Glacier".ENVIRONMENTAL EARTH SCIENCES 75.5(2016):11. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论