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| 1 | 冰穹A冰川学研究进展及深冰芯计划展望显示文摘目前,在东南极冰盖分冰岭中心的冰穹A(Dome Argus,又称Dome A)开展冰川学及深冰芯研究已成为深入探讨南极冰盖演化和找寻地球最古老冰芯气候记录的热点。本文介绍了在冰穹A已获得的冰川学各项研究的进展,并结合国际冰芯科学研究计划(International Partnerships in Ice Core Sciences,IPICS)中有关寻找最古老冰芯的相关资料,对冰穹A的气象要素、地貌、冰厚、冰下地形、冰体流速、冰盖内部结构等环境特征进行综合归纳分析,讨论冰穹A冰川学的最新发展趋势,其对今后深冰芯钻探计划的潜在影响,以及冰穹A深冰芯钻探需考虑的问题和未来发展动向。 | 唐学远 孙波 李院生 崔祥斌 李鑫 | 2012 | 极地研究2012，24，1： | 10 |
| 2 | Overview of China's Antarctic research progress 1984–2016显示文摘It is more than 30 years since the first Chinese National Antarctic Research Expedition(CHINARE) landed in Antarctica in 1984, representing China's initiation in polar research. This review briefly summarizes the Chinese Antarctic scientific research and output accomplished over the past 30 years. The developments and progress in Antarctic research and the enhancement of international scientific cooperation achieved through the implementation of the CHINARE program have been remarkable. Since the 1980 s, four permanent Chinese Antarctic research stations have been established successively and 33 CHINAREs have been completed. The research results have been derived from a series of spatiotemporal observations in association with various projects and multidisciplinary studies in the fields of oceanography, glaciology, geology, geophysics, geochemistry, atmospheric science, upper atmospheric physics, Antarctic astronomy, biology and ecology, human medicine, polar environment observation, and polar engineering. | CHEN Liqi LIU Xiaohan BIAN Lingen CHEN Bo HUANG Hongliang HU Hongqiao LUO Wei SHI Guitao SHI Jiuxin XU Chengli YANG Guang ZHAO Yue ZHANG Shaohua | 2017 | Advances in Polar Science2017，28，3： | 9 |
| 3 | Chinese radioglaciological studies on the Antarctic ice sheet: progress and prospects显示文摘Chinese radioglaciological studies on the Antarctic ice sheet(AIS) began in 2004/05 when the 21 st Chinese National Antarctic Research Expedition(CHINARE 21) team arrived at Dome A for the first time and radio echo sounding(RES) was conducted along the inland traverse and in the Dome A region. Subsequently, more field surveys were conducted along the traverse and in the Dome A region using different radar systems targeting different scientific purposes, such as revealing the landscape of the Gamburtsev Subglacial Mountains by detailed grid RES, or locating a deep ice core drilling site by mapping and studying internal structures, bedrock topography and subglacial conditions in the Dome A region. Furthermore, the evolution of the AIS was inferred from the typical mountain glaciation topography beneath Dome A, and the age of the deep ice core at Kunlun Station was estimated through numerical modeling. Recently, the Snow Eagle 601 airplane was acquired and an airborne geophysical system was constructed to survey the AIS in Princess Elizabeth Land during CHINARE 32(2015/16) and CHINARE 33(2016/17) in order to fill the large data gap there. In this paper, we review both the recent progress of Chinese radioglaciological science in Antarctica and future proposed work. | CUI Xiangbin WANG Tiantian SUN Bo TANG Xueyuan GUO Jingxue | 2017 | Advances in Polar Science2017，28，3： | 6 |
| 4 | Dome Argus: Ideal site for deep ice drilling显示文摘Located on the centre of ice drainage range, the highest Dome Argus (Dome A) of East Antarctic Ice Sheet (EAIS), could be represented as an ideal site for deep ice cores drilling containing oldest paleo-climate records. To select a suitable drilling site for deep ice core, it needs gather all information pertaining to the local meteorology, ice sheet landforms, ice thickness, subglacial topography of bed rocks, ice velocity, internal structures of ice sheet, etc. Based on the International Partnerships in Ice Core Sciences (IPICS), we present recent achievement of glaciological research and its perspective at Dome A in this paper. We system-atically discussed the merits and possible ventures of potential drilling sites around Dome A. Among all the candidates, we find that the Chinese Antarctic Kunlun Station is the best site for carrying out the first deep ice core drilling campaign. We emphasize and assess further the possibility to obtain a replicate core for studying dynamics and evolution of climate change. | TANG Xueyuan SUN Bo LIYuansheng LI Xin CUI Xiangbin | 2012 | Advances in Polar Science2012，23，1： | 5 |
| 5 | Climatology of stable isotopes in Antarctic snow and ice:Current status and prospects显示文摘Stable isotopic composition in Antarctic snow and ice is commonly regarded as one of invaluable palaeoclimate proxies and plays a critically important role in reconstructing past climate change.In this paper we summarized the spatial distribution and the controlling factors of δD,δ18O,d-excess and 17O-excess in Antarctic snow and ice,and discussed their reliability and applicability as palaeoclimate proxies.Recent progress in the stable isotopic records from Antarctic deep ice cores was reviewed,and perspectives on bridging the current understanding gaps were suggested. | HOU ShuGui WANG YeTang PANG HongXi | 2013 | Chinese Science Bulletin2013，58，10： | 4 |
| 6 | Glaciological observations at Dome Argus, East Antarctica显示文摘Dome Argus(Dome A) in East Antarctica is a potentially likely site to meet one of the major objectives of the International Partnerships in Ice Core Sciences(IPICS) on the oldest ice core, and thus has aroused wide public and scientific interest. Since 2004/2005, many glaciological investigations have been conducted in this region. These have included GPS and ground-penetrating radar surveys, snow pit and ice core drilling, stake network measurements, and meteorological observations. In this article, the main results of these glaciological investigations in the Dome A region are summarized. We present details of the surface mass balance on different timescales and its spatial variability, geochemical characteristics of the surface snow, and paleo-environment reconstruction of ice cores. Finally, perspectives on the prospects for future studies are suggested. | AN Chunlei WANG Yetang HOU Shugui | 2017 | Advances in Polar Science2017，28，4： | 3 |
| 7 | APPLICATION OF NOISE REDUCTION METHOD BASED ON CURVELET THRESHOLDING NEURAL NETWORK FOR POLAR ICE RADAR DATA PROCESSING显示文摘Due to the demand of data processing for polar ice radar in our laboratory, a Curvelet Thresholding Neural Network (TNN) noise reduction method is proposed, and a new threshold function with infinite-order continuous derivative is constructed. The method is based on TNN model. In the learning process of TNN, the gradient descent method is adopted to solve the adaptive optimal thresholds of different scales and directions in Curvelet domain, and to achieve an optimal mean square error performance. In this paper, the specific implementation steps are presented, and the superiority of this method is verified by simulation. Finally, the proposed method is used to process the ice radar data obtained during the 28th Chinese National Antarctic Research Expedition in the region of Zhongshan Station, Antarctica. Experimental results show that the proposed method can reduce the noise effectively, while preserving the edge of the ice layers. | Wang Wenpeng Zhao Bo Liu Xiaojun | 2013 | Journal of Electronics(China)2013，30，4： | 1 |
| 8 | 极地冰雪探测冰雷达技术发展回顾与展望显示文摘冰雷达是用于极地冰雪探测的主要技术手段,为研究极地冰雪的几何特征、内部结构、冰下地形地貌和冰底环境提供了重要的基础观测数据。20世纪50年代,人类首次发现特定频段的电磁波可以“穿透”南极冰盖,进而在60年代研制出用于极地冰盖冰下探测的冰雷达系统。之后60多年里,随着计算机、电子信息和卫星定位导航等技术的发展,冰雷达技术研究取得快速发展,形成了适用于极地冰盖、海冰及其上覆积雪不同探测需求的多样化冰雷达系统。本文在简要回顾了早期冰雷达技术发展的基础上,着重从极地冰盖深部探测、极地冰盖和海冰浅表层探测以及新型极地冰雪探测冰雷达技术3个方面,回顾总结了近10年来国内外主要进展。未来,为适应极地冰盖、海冰及其上覆积雪观测研究的多种需求,需要进一步提升冰雷达系统性能(探测深度、跨轨迹向分辨率、垂向分辨率等),并且研制满足新型平台(无人机、卫星等)搭载需求的小型、低功耗冰雷达系统,以及发展多通道、多频、多极化集同观测模式的综合冰雷达技术。 | 邢治瑞 稂时楠 赵博 窦银科 肖鹏 李霖 孙波 崔祥斌 | 2023 | 极地研究2023，35，4： | 0 |
| 9 | 基于深度学习算法的冰雷达图像冰面与基岩界面提取显示文摘极地冰盖底部的冰-基岩界面记录了冰盖的历史演变,反映了冰层的几何特征和冰底环境属性,是推断冰盖动力学和解释冰下地貌的重要指标。机载冰雷达是一种有效的极地冰盖探测方法,但雷达数据受探测环境和仪器自身局限性的影响,会包含各类噪声。为了高效准确地提取冰雷达图像中基岩界面和冰面、降低噪声干扰,利用2015—2016年度中国第32次南极科学考察在伊丽莎白公主地的航空冰雷达观测数据,基于深度学习的pix2pix算法建立了一种自动化提取雷达图像冰面和基岩界面的模型。实验结果表明,该模型提取冰面/基岩界面的精确率为0.863/0.948,峰值信噪比为24.814 dB,均高于以往的K-SVD和CycleGAN同类算法,能更有效地去除噪声、提高图像质量,更高精度地还原现在通用的人工提取效果。 | 邢治瑞 窦银科 李霖 杨望笑 张锋 崔祥斌 | 2023 | 极地研究2023，35，2： | 0 |
| 10 | 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、表面和冰下地形(英文)显示文摘中国第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。 | 唐学远 郭井学 孙波 王甜甜 崔祥斌 | 2016 | Applied Geophysics2016，13，1： | 0 |
| 11 | 东南极昆仑站周边沿“中国墙”的冰厚和冰下地形分布(英文)显示文摘冰厚和冰下地形是南极冰盖的基本特征参数,是南极冰盖底部环境和物质平衡研究的基础。2007/08年,中国第24次南极科学考察期间,运用深部探测冰雷达系统,在东南极位于Dome A区域的我国南极昆仑站周边,开展了沿'中国墙'的冰厚和冰下地形探测。结果显示:沿'中国墙'的冰厚主要分布在1600m-2800m之间,冰厚最大达到3444m,最小为1255m;冰下地形平均高程为1722m,但是最低仅有604 m;相较于分冰岭北侧,分冰岭南侧冰厚较大,冰下地形较低,并且发育了4个明显的冰下深谷。不过,没有发现Gamburtsev冰下山脉区域典型的冰底再冻结现象以及冰下湖和水体的存在。Bedmap 2中沿'中国墙'的冰厚和冰下地形数据与冰雷达测量结果存在一致性,但是分辨率和在冰下地形起伏剧烈区域的准确性上非常有限。通过冰雷达探测得到的沿'中国墙'的冰厚和冰下地形分布,进一步揭示了这一'不可接近区域'的冰盖特征,对于Dome A区域冰盖动力学研究和未来针对Gamburtsev冰下山脉的地质钻探以及深冰芯钻探选址具有重要参考价值。 | 崔祥斌 孙波 苏小岗 郭井学 | 2016 | Applied Geophysics2016，13，1： | 0 |
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