APPLIED GEOPHYSICS
 
        首页  |  版权声明  |  期刊介绍  |  编 委 会  |  收录情况  |  期刊订阅  |  下载中心  |  联系我们  |  English
应用地球物理  2016, Vol. 13 Issue (1): 203-208    DOI: 10.1007/s11770-016-0540-6
论文 最新目录 | 下期目录 | 过刊浏览 | 高级检索 Previous Articles  |  Next Articles  
东南极冰盖伊丽莎白公主地中国泰山站站址所在区域的冰厚、内部等时层、地表和冰下地形
唐学远,郭井学,孙波,王甜甜,崔祥斌
国家海洋局极地科学重点实验室,中国极地研究中心,上海 200136
Ice thickness, internal layers, and surface and subglacial topography in the vicinity of Chinese Antarctic Taishan station in Princess Elizabeth Land, East Antarctica
Tang Xue-Yuan1, Guo Jing-Xue1, Sun Bo1, Wang Tian-Tian1, and Cui Xiang-Bin1
1. SOA Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China.
 全文: PDF (664 KB)   HTML ( KB)   输出: BibTeX | EndNote (RIS)      背景资料
摘要 中国第21次(2004/2005,CHINARE 21)和第29次(2012/2013,CHINARE 29)南极科学考察在东南极冰盖伊丽莎白公主地中国泰山考察站站址所在区域,通过探地冰雷达和GPS进行了两次地球物理探测。使用中心频率分别为60MHz和150MHz的冰雷达探测,首次(2004/2005)获得该地区的冰厚与冰内部等时层结构。GPS观测显示以泰山站站址为中心约2km?2km范围内的冰盖表面地形起伏很小,海拔为2607?2636m。冰盖雷达断面显示该区域的平均冰厚为1900m,最大冰厚为1949m,最小冰厚为1856m。在泰山站站址下方冰厚为1870m。冰盖表面高程与冰厚数据联合分析发现该地区的冰下地形相对起伏剧烈,海拔为662?770m,反映出冰下地形为山地地貌。该2km?2km测量网格下方的冰量为7.6km3。60MHz冰雷达数据给出一条长17.6km,穿越泰山站的冰盖断面内部等时层结构图。从中识别分析出一些内部等时层,结果表明该处的冰盖内部等时层受到了冰流的扰动,内部等时层的几何形态暗示了泰山站所处的冰盖下方很可能经历了一个复杂的沉积过程。
服务
把本文推荐给朋友
加入我的书架
加入引用管理器
E-mail Alert
RSS
作者相关文章
唐学远
郭井学
孙波
王甜甜
崔祥斌
关键词东南极   泰山站   冰厚   内部等时层   冰雷达     
Abstract: We present the results of two ground-based radio-echo-sounding (RES) and GPS surveys performed in the vicinity of new Chinese Taishan station, Princess Elizabeth Land, East Antarctica, obtained in two austral summers during CHINARE 21 (2004/2005) and CHINARE 29 (2012/2013). The radar surveys measured ice thickness and internal layers using 60- and 150-MHz radar systems, and GPS measurements showed smooth surface slopes around the station with altitudes of 2607–2636 m above sea level (a.s.l.). Radar profiles indicate an average ice thickness of 1900 m, with a maximum of 1949 m and a minimum of 1856 m, within a square area measuring approximately 2 km × 2 km in the vicinity of the station. The ice thickness beneath the station site is 1870 m. The subglacial landscape beneath the station is quiet sharp and ranges from 662 to 770 m a.s.l., revealing part of a mountainous topography. The ice volume in the grid is estimated to be 7.6 km3. Along a 60-MHz radar profile with a length of 17.6 km at the region covering the station site, some disturbed internal layers are identified and traced; the geometry of internal layers within the englacial stratigraphy may imply a complex depositional process in the area.
Key wordsEast Antarctica   Taishan station   ice thickness   internal layers   ground-based radio echo sounding   
收稿日期: 2014-12-31;
基金资助:

本研究由国家自然科学基金(编号:41376192,40906101)、全球变化研究国家重大科学研究计划(973计划)(编号:2013CBA01804,2012CB957702)、国家海洋局极地考察办公室对外合作支持项目(编号:IC201214)、上海市自然科学基金(编号:13ZR1445300)、极地专项-南极周边海域物理海洋和海洋气象考察(编号:CHINARE2014-01-01)联合资助。

引用本文:   
唐学远,郭井学,孙波等. 东南极冰盖伊丽莎白公主地中国泰山站站址所在区域的冰厚、内部等时层、地表和冰下地形[J]. 应用地球物理, 2016, 13(1): 203-208.
TANG Xue-Yuan,GUO Jing-Xue,SUN Bo et al. Ice thickness, internal layers, and surface and subglacial topography in the vicinity of Chinese Antarctic Taishan station in Princess Elizabeth Land, East Antarctica[J]. APPLIED GEOPHYSICS, 2016, 13(1): 203-208.
 
[1] Bianchi, C., Cafarella, L., Michelis, D. P., et al., 2003, Radio Echo Sounding (RES) investigations at Talos Dome (East Antarctica): Bedrock topography and ice thickness: Annals of Geophysics, 46, 1265−1270.
[2] Cui, X. B., Sun, B., Tian, G., et al., 2010a, Preliminary results of ice radar investigation along the traverse between Zhongshan and Dome A in East Antarctic ice sheet: Ice thickness and subglacial topography: Chinese Science Bulletin, 55(24), 2715−2722.
[3] Cui, X. B., Sun, B., Tian, G., et al., 2010b, Ice radar investigation at Dome A, East Antarctica: Ice thickness and subglacial topography: Chinese Science Bulletin, 55(4−5), 425−431.
[4] Ding, M., Xiao, C., Li, Y. S., et al., 2011, Spatial variability of surface mass balance along a traverse route from Zhongshan station to Dome A, Antarctica: Journal of Glaciology, 57, 658−666.
[5] Drews, R., Eisen, O., Weikusat, I., et al., 2009, Layer disturbances and the radio-echo free zone in ice sheets: The Cryosphere, 3, 195−203.
[6] Drews, R., Martín, C., Steinhage, D., et al., 2013, Characterizing the glaciological conditions at Halvfarryggen ice dome, Dronning Maud Land, Antarctica: Journal of Glaciology, 59(213), 9−20.
[7] Fujita S., Maeno, H., Uratsuka, S., et al., 1999, Nature of radio echo layering in the Antarctic ice sheet detected by a two-frequency experiment: Journal of Geophysical Research, 104(B6), 13013−13024.
[8] Fretwell, P., Pritchard, H. D., Vaughan, D. G., et al., 2013, Improved ice bed, surface and thickness datasets for Antarctica: The Cryosphere, 7, 375−393.
[9] Li, Y. S., Cole-Dai, J., and Zhou, L. Y., 2009, Glaciochemical evidence in an East Antarctica ice core of a recent (AD 1450-1850) neoglacial episode: Journal of Geophysical Research, 114(D08117).
[10] Ma, Y. F., Bian, L. G., Xiao, C. D., et al., 2010, Near surface climate of the traverse route from Zhongshan Station to Dome A, East Antarctica: Antarctic Science, 22(4), 443−459.
[11] Martín, C., Hindmarsh, R. C. A., and Navarro, F. J., 2006, Dating ice flow change near the flow divide at Roosevelt Island, Antarctica, by using a thermomechanical model to predict radar stratigraphy: Journal of Geophysical Research, 111(F1), F01011.
[12] Nereson, N. A., and Raymond, C. F., 2001, The elevation history of ice streams and the spatial accumulation pattern along the Siple Coast of West Antarctica inferred from ground-based radar data from three inter-ice-stream ridges: Journal of Glaciology, 47(157), 303−313.
[13] Pattyn, F., Matsuoka, K., and Berte, J., 2010, Glacio-meteorological conditions in the vicinity of the Belgian Princess Elisabeth Station, Antarctica: Antarctic Science, 22(01), 79−85.
[14] Siegert, M. J., Payne, A. J., and Joughin, I., 2003, Spatial stability of Ice Stream D and its tributaries, West Antarctica, revealed by radio-echo sounding and interferometry: Annals of Glaciology, 37, 377−382.
[15] Sun, B., Siegert, M. J., Mudd, S. M., et al., 2009, The Gamburtsev Mountains and the origin and early evolution of the Antarctic Ice Sheet: Nature, 459, 690−693.
[16] Tang, X. Y., Sun, B., Zhang, Z. H., et al., 2011, Structure of the internalisochronous layers at Dome A, East Antarctica: Science China Earth Sciences, 54(3), 445−450.
[17] Wesche, C., Eisen O., Oerter H., et al., 2007, Surface topography and ice flow in the vicinity of the EDML deep-drilling site, Antarctica: Journal of Glaciology, 53(182), 442−448.
[18] Zhang, S., Dong. C, E., Wang, Z., et al., 2008, Ice velocity from static GPS observations along the transect from Zhongshan station to Dome A, East Antarctica: Annals of Glaciology, 48(1), 113−118.
[1] 崔祥斌,孙波,苏小岗,郭井学. 东南极昆仑站周边沿“中国墙”的冰厚和冰下地形分布[J]. 应用地球物理, 2016, 13(1): 209-216.
版权所有 © 2011 应用地球物理
技术支持 北京玛格泰克科技发展有限公司