基于SAR偏移量跟踪法提取岗纳楼冰川流速

doi:10.13474/j.cnki.11-2246.2020.0350

测绘通报 ›› 2020, Vol. 0 ›› Issue (11): 33-38.doi: 10.13474/j.cnki.11-2246.2020.0350

基于SAR偏移量跟踪法提取岗纳楼冰川流速

张生鹏^1,2, 周中正³, 赵利江², 张永荥²

1. 青海师范大学地理科学学院, 青海西宁 810008;
2. 青海省基础测绘院, 青海西宁 810101;
3. 武汉大学, 湖北武汉 430079

收稿日期:2019-12-16 发布日期:2020-11-30
作者简介:张生鹏(1985-),男,博士生,工程师,研究方向为SAR及基础测绘新技术应用。E-mail:zhangshengpeng@qhcors.com
基金资助:
基于现代测绘基准体系成果及技术方法的科学研究（ZQJZ-2018003）

Extraction of Gangnalou glacier velocity based on SAR migration tracking method

ZHANG Shengpeng^1,2, ZHOU Zhongzheng³, ZHAO Lijiang², ZHANG Yongying²

1. School of Geographic Science, Qinghai Normal University, Xining 810008, China;
2. Qinghai Basic Surveying and Mapping Institute, Xining 810101, China;
3. School of Geodsy and Geomatics, Wuhan University, Wuhan 430079, China

Received:2019-12-16 Published:2020-11-30

摘要/Abstract

摘要： 冰川动态变化监测有助于反映全球和区域气候演变，保护自然环境和自然资源。近年来，基于SAR数据研究冰川运动已成为主流技术之一。基于SAR提取冰川流速主要包括合成孔径雷达干涉测量、多孔径雷达干涉和偏移量追踪法。本文采用SAR偏移量追踪法中的强度追踪法，提取青海省哈拉湖东北部岗纳楼冰川沿距离向、方位向的冰川流速。试验结果表明，距离向冰川运动速度提取效果较好，最大流速达15.36 m/a，流速从中轴向两侧递减，在冰舌末端趋于0；方位向提取的冰流速最大达18.27 m/a，但因电离层干扰，方位向流速图中存在一些方位向条纹。此外，由于冰流速在方位向分量小等因素的影响，本文研究提取的方位向流速精度低于距离向。

关键词: 合成孔径雷达, 岗纳楼冰川, 偏移量跟踪法, 冰川流速

Abstract: Glacier dynamic change monitoring helps to reflect global and regional climate change and protect the natural environment and natural resources. In recent years, the research on glacier movement based on SAR data has become one of the mainstream technologies. The extraction of glacier velocity based on SAR mainly includes synthetic aperture radar interferometry, multi-aperture radar interferometry and offset tracking. In this paper, the intensity tracking method of SAR migration tracking method is used to extract the glacier velocity along the distance and direction of Gangnalou glacier in the northeast of Hala lake, Qinghai province. The results show that the extraction effect of the range direction glacier velocity is better, the maximum velocity reaches 15.36 m/a, the velocity decreases from both sides of the central axis, and tends to 0 at the end of the ice tongue; the maximum velocity of the azimuth direction extraction ice velocity reaches 18.27 m/a, but there are some directional streaks in the azimuth velocity diagram due to the ionosphere interference. Inaddition, due to the small component of ice velocity in azimuth and other factors, the accuracy of azimuth velocity extracted in this study is lower than that in distance.

Key words: synthetic aperture radar, Gangnalou glacier, offset tracking method, glacier velocity

中图分类号:

P237

张生鹏, 周中正, 赵利江, 张永荥. 基于SAR偏移量跟踪法提取岗纳楼冰川流速[J]. 测绘通报, 2020, 0(11): 33-38.

ZHANG Shengpeng, ZHOU Zhongzheng, ZHAO Lijiang, ZHANG Yongying. Extraction of Gangnalou glacier velocity based on SAR migration tracking method[J]. Bulletin of Surveying and Mapping, 2020, 0(11): 33-38.

参考文献

[1] JACOB T, WAHR J, PFEFFER W T, et al. Recent contri-butions of glaciers and ice caps to sea level rise[J].Nature,2012,482(7386):514-518.
[2] 艾松涛, 王泽民, 鄂栋臣, 等. 利用GPS的北极冰川运动监测与分析[J].武汉大学学报(信息科学版),2012,37(11):1337-1340.
[3] BECHOR N B D, ZEBKER H A. Measuring two-dimen-sional movements using a single InSAR pair[J].Geophysical Research Letters,2006,33(16):16311.
[4] STROZZI T, LUCKMAN A, MURRAY T, et al. Glacier motion estimation using SAR offset-tracking procedures[J].IEEE Transactions on Geoscience & Remote Sensing, 2002, 40(11):2384-2391.
[5] JOUGHIN I. Estimation of ice-sheet topography and motion using interferometric synthetic aperture radar[D].Washington:University of Washington,1995.
[6] RIGNOT E. Changes in the velocity structure of the Green-land Ice Sheet[J].Science,2006,311(5763):986-990.
[7] 蒋宗立, 刘时银, 韩海东, 等. 基于SAR数据的山地冰川表面运动速度分析[J].遥感技术与应用,2011,26(5):640-646.
[8] 李佳, 李志伟, 汪长城, 等.SAR偏移量跟踪技术估计天山南依内里切克冰川运动[J].地球物理学报,2013,56(4):1226-1236.
[9] 仲伟凡,唐远彬,殷腾箐.基于纹理特征的SAR影像各拉丹冬冰川信息提取[J].测绘与空间地理信息,2015,38(10):187-189.
[10] 刘爽,童小华.基于多源遥感影像的南极Lambert流域冰川运动速度提取与精度验证[J].同济大学学报(自然科学版),2018,46(3):118-124.
[11] 郭铌,张杰,梁芸.西北地区近年来内陆湖泊变化反映的气候问题[J].冰川冻土,2003,25(2):211-214.
[12] ROTT H, STUEFER M, SIEGEL A, et al. Mass fluxes and dynamics of Moreno glacier,Southern Patagonia icefield[J].Geophysical Research Letters,1998,25(9):1407-1410.
[13] GRAY A L, MATTAR K E, VACHON P W, et al. InSAR results from the RADARSAT antarctic mapping mission data:estimation of glacier motion using a simple registration procedure[C]//IEEE International Geoscience & Remote Sensing Symposium.[S.l.]:IEEE,1998.
[14] REMI M, ERIC R. Flow of glaciar moreno, argentina, from repeat-pass shuttle imaging radar images:comparison of the phase correlation method with radar interferometry[J].Journal of Glaciology,1999,45(149):93-100.
[15] GRAY A L, MATTAR K E, SOFKOG. Influence of ionos-pheric electron density fluctuations on satellite radar interferometry[J].Geophysical Research Letters,2000,27(10):1451-1454.
[16] GRAY A L, SHORT N, MATTAR K E, et al. Velocities and flux of the filchner ice shelf and its tributaries determined from speckle tracking interferometry[J].Canadian Journal of Remote Sensing,2001,27(3):193-206.
[17] GEUDTNER D, TORRES R, SNOEIJ P, et al. Sentinel-1 system capabilities and applications[C]//Proceedings of 2014 IEEE International Geoscience and Remote Sensing Symposium.[S.l.]:IEEE,2014.
[18] YAGVE-MARTÍNEZ N, PRATS-IRAOLA P, RODRÍGUEZ GONZÁLEZ F, et al. Interferometric processing of sentinel-1 TOPS data[J].IEEE Transactions on Geoscience and Remote Sensing,2016,54(4):2220-2234.
[19] 吴文豪,哨兵雷达卫星TOPS模式干涉处理研究[D].武汉:武汉大学,2016.
[20] 丁一凡,程晓,程铖,等.基于偏移追踪的青藏高原卓琼冰川流速监测及成因分析[J].地球物理学报,2017,60(5):40-48.
[21] 李鹏,李振洪,施闯,等,中国地区30 m分辨率SRTM质量评估[J].测绘通报,2016(9):24-28.

基于SAR偏移量跟踪法提取岗纳楼冰川流速

Extraction of Gangnalou glacier velocity based on SAR migration tracking method

RichHTML

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	许广河, 何小锋, 王国瑞, 扈志勇, 程霞, 李小琼. 黄河流域宁夏(西吉县)段滑坡灾害的InSAR识别及成因分析[J]. 测绘通报, 2022, 0(6): 104-107.
[2]	杨映新, 洪武胜, 吴曼乔. 利用Sentinel-1影像监测土地回填导致的地表形变[J]. 测绘通报, 2021, 0(6): 67-70.
[3]	何正枫, 张继贤, 黄国满, 盛辉军. 尼泊尔Mw7.8地震对珠峰区域内冰川形变及流速的影响[J]. 测绘通报, 2021, 0(5): 43-48,101.
[4]	孙玉铮, 谢先明, 梁小星. 一种容积信息滤波局部迭代相位解缠方法[J]. 测绘通报, 2021, 0(2): 40-43.
[5]	洪兆阳, 金双根. 利用时序PS-InSAR监测青藏高原冻土区地表形变[J]. 测绘通报, 2021, 0(1): 35-40.
[6]	蒋留兵, 杨凯, 车俐. 地基合成孔径雷达对目标三维形变的监测[J]. 测绘通报, 2020, 0(3): 35-38,68.
[7]	胡东明, 隋立春, 丁明涛. 困难地区InSAR技术和加权融合的DEM生成[J]. 测绘通报, 2020, 0(2): 142-146.
[8]	刘龙龙, 张继贤, 王世杰, 赵争. 新型FMCW地基SAR和三维激光扫描仪在大坝变形监测中的应用[J]. 测绘通报, 2019, 0(3): 76-80.
[9]	张元迪, 焦瑞莉, 朱云龙, 吴世玉. GNSS-R海面目标成像仿真方法研究[J]. 测绘通报, 2019, 0(2): 86-90,107.
[10]	刘龙龙, 张继贤, 赵争, 康琪, 郗晓菲. GB-SAR变形监测技术研究现状与展望[J]. 测绘通报, 2019, 0(11): 1-7.
[11]	付波霖, 耿仁方, 李颖, 高二涛, 范冬林. 多频率InSAR提取沼泽湿地DEM精度对比分析[J]. 测绘通报, 2019, 0(10): 1-7.
[12]	张莹, 李爱霞, 赵红. 改进球形张量投票的SAR图像边缘提取[J]. 测绘通报, 2018, 0(9): 59-63.
[13]	陈磊, 赵学胜. 结合InSAR的矿区大梯度变形监测技术进展[J]. 测绘通报, 2018, 0(7): 18-23.
[14]	白玉, 姜东民, 裴加军, 张宁, 白郁. 改进的ELU卷积神经网络在SAR图像舰船检测中的应用[J]. 测绘通报, 2018, 0(1): 125-128.
[15]	王鹏, 邢诚, 徐亚明. GB-SAR导轨倾角引起的影像坐标投影变换误差分析[J]. 测绘通报, 2017, 0(8): 25-30.