[1]姬鑫慧,叶庆华*,聂 维,等.基于TerraSAR/TanDEM-X监测岗日嘎布山脉东南段冰川冰面高程变化(2000—2014)[J].山地学报,2021,(5):631-645.[doi:10.16089/j.cnki.1008-2786.000626)]
　JI Xinhui,YE Qinghua*,NIE Wei,et al.Glacier Surface Elevation Change in Southeastern Mt. Kangri Karpo on Tibet during 2000—2014 Based on TerraSAR/TanDEM-X Data[J].Mountain Research,2021,(5):631-645.[doi:10.16089/j.cnki.1008-2786.000626)]
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基于TerraSAR/TanDEM-X监测岗日嘎布山脉东南段冰川冰面高程变化(2000—2014)()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2021年第5期
页码:
631-645
栏目:
山地环境
出版日期:
2021-09-25

文章信息/Info

Title:
Glacier Surface Elevation Change in Southeastern Mt. Kangri Karpo on Tibet during 2000—2014 Based on TerraSAR/TanDEM-X Data
文章编号:
1008-2786-(2021)5-631-15
作者:
姬鑫慧1; 2; 叶庆华1*; 聂 维3; 陈益民1; NAUMAN Ali1
1.中国科学院青藏高原研究所 青藏高原地球系统科学国家重点实验室,北京 100101; 2.中国科学院资源与环境学院,北京 100049; 3.南湖实验室 大数据技术研究中心,浙江 嘉兴 314000
Author(s):
JI Xinhui1; 2; YE Qinghua1*; NIE Wei3; CHEN Yimin1; NAUMAN Ali1
1. State Key Laboratory of Tibetan Plateau Earth System Science(LATPES), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101,China; 2. College of Resources and Environment, Chinese Academy of Sciences, Beijing 100049,China; 3. Research Center of Big Data Technology, Nanhu Laboratory, Jiaxing 314000, Zhejiang, China
关键词:
冰川变化;  TerraSAR/TanDEM-X;  雷达差分干涉测量(D-InSAR);  气候响应;  岗日嘎布山;  青藏高原
Keywords:
glacier change;  TerraSAR/TanDEM-X;  Differential Intereferometric Synthetic Aperture Radar(D-InSAR);  climate change;  Mt. Kangri Karpo;  the Qinghai-Tibet Plateau
分类号:
P343.6
DOI:
10.16089/j.cnki.1008-2786.000626)
文献标志码:
A
摘要:
岗日嘎布山区是海洋型山地冰川集中发育地区之一。海洋型冰川对气候变化敏感,藏东南多云雨天气使可用光学遥感影像数据少,限制了该地冰川变化遥感监测研究,雷达数据的应用为解决这一问题提供了有效途径。基于2000年SRTM DEM与2014年TerraSAR/TanDEM-X雷达数据,采用差分干涉测量(D-InSAR)方法,研究岗日嘎布山区东南段冰面高程变化及冰储量变化特征,得出如下结论:(1)研究区2000—2014年冰储量变化为-1.69±0.12 Gt,冰面高程年均变化为-0.86±0.13 m·a-1。(2)冰面高程变化整体与海拔高度呈正相关(皮尔森系数为0.93)。在3700～3900 m,随海拔升高冰面高程变化加剧; 在3900—5800 m,冰面高程变化逐渐趋于零; 在5800 m以上高海拔积累区,冰面高程变化为正值。(3)表碛覆盖冰川消融较快。表碛覆盖冰川区冰面高程变化为-1.71 m·a-1,裸冰区为-0.73 m·a-1。(4)结合波密、察隅和左贡站年均温与年降水变化可知,2000—2014年研究区年均温显著升高,年降水变化不明显,冰川快速消融是区域气温升高所致。本文可为青藏高原冰川时空变化研究提供基础数据支持。
Abstract:
Glaciers in Mt. Kangri Karpo of southeastern Qinghai-Tibet Plateau are marine glaciers, which are more sensitive to global climate change than continental ones. It is of great significant to investigate glacier coverage changes at Mt. Kangri Karpo for a better knowledge of climate change effects. Unfortunately, the frequent cloudy weather at Mt. Kangri Karpo limits the quality of optical images, which has become a bottleneck for glacier studies in the area. Differential Interferometric Synthetic Aperture Radar(D-InSAR), provides a more accurate way to study glacier elevation changes. Based on TerraSAR / TanDEM-X data in 2014 and SRTM DEM in 2000, this research studied geodetic glacier surface elevation change and geodetic glacier mass balance changes in the southeast of Mt. Kangri Karpo. The results showed that:(1)During 2000—2014, the glacier geodetic mass change was -1.69±0.12 Gt, i.e. the averaged glacier surface elevation change was -0.86±0.13 m·a-1.(2)The glacier surface elevation change had a positive correlation with the altitude. The Pearson coefficient was 0.93. At the altitude of 3700～3900 m·a.s.l., the glacier surface downwasting was more dramatic as the altitude increases. From 3900 m to 5800 m·a.s.l., glacier surface elevation change gradually increased from a negative value to zero. While above 5800 m·a.s.l., the glacier surface elevation change was always positive in the accumulation area.(3)The debris-covered glaciers melted faster(the average surface elevation change was by -1.71 m·a-1)than the exposed glaciers(-0.73 m·a-1).(4)According to the meteorological data at Bomi, Zayu and Zuogong stations, it showed that the annual mean air temperature had increased significantly during 2000—2014, while the annual precipitation did not present obvious change trend. Therefore, the rapid melting of glaciers was mainly caused by regional rising temperatures. This study provides basic data support for understanding the spatial-temporal glacier changes in the Qinghai-Tibet Plateau.

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备注/Memo

备注/Memo:
收稿日期(Received date):2020-10-25; 改回日期(Accepted date): 2021-07-30
基金项目(Foundation item):国家自然科学基金项目(91747201,41530748); 第二次青藏高原综合科学考察研究(2019QZKK0202); 中国科学院“十三五”信息化建设专项(XXH13505-06)[National Natural Science Foundation of China(91747201,41530748); The Second Comprehensive Scientific Investigation and Research on the Tibetan Plateau(2019QZKK0202); Informatization Construction of the 13th Five Year Plan of Chinese Academy of Sciences(XXH13505-06)]
作者简介(Biography):姬鑫慧(1996-),女,山西晋城人,硕士研究生,主要研究方向:冰川遥感。[JI Xinhui(1996-), female, born in Jincheng, Shanxi province, M.Sc. candidate, research on remote sensing of glaciers] E-mail: jixinhui@itpcas.ac.cn
*通讯作者(Corresponding author):叶庆华(1972),女,博士,研究员,研究方向:资源环境遥感与GIS应用。[YE Qinghua(1972-), female, Ph.D., professor, specialized in remote sensing in resources & environment change and its applications of GIS] E-mail: yeqh@itpcas.ac.cn
更新日期/Last Update: 2021-09-30