SAR INTERFEROMETRY AND SPECKLE TRACKING APPROACH FOR GLACIER VELOCITY ESTIMATION USING ERS-1/2 AND TERRASAR-X SPOTLIGHT HIGH RESOLUTION DATA

被引:8
作者
Kumar, Vijay [1 ]
Venkataraman, G. [1 ]
Rao, Y. S. [1 ]
机构
[1] Indian Inst Technol, Ctr Studies Resources Engn, Bombay 400076, Maharashtra, India
来源
2009 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM, VOLS 1-5 | 2009年
关键词
Coherence loss; glaciers; SAR Interferometry; DInSAR; RADAR INTERFEROMETRY;
D O I
10.1109/IGARSS.2009.5417663
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Glacier retreat and advance is general phenomenon in Himalayan region due to change in climatic conditions For quantifying the global warming effects on local scale glacier system monitoring and estimating its dynamic geophysical parameters viz movement and volume change are Important In this study glacier movement estimation is attempted in north western Himalayan region using spaceborne InSAR technique, which is based on preserving the coherence between two acquisitions of the same scene It is observed that ERS-1/2 tandem data give high correlation over Gangotri glacier and Siachen glacier and movement in LOS direction is deciphered However, with the use of SAR Speckle tracking method two dimensional (Azimuth and range directions) velocities of glaciers can be obtained In this study attempt has been made to measure 2-D velocity components of Gangotri glacier New generation TerraSAR-X (TS-X) high resolution spotlight mode (HS). single look slant range complex (SSCs) data of 28(th) August. 2008, 08(th) September. 2008. 19th September. 2008 and 30(th) September. 2008 are exploited for this study Interferogram, coherence Image and intensity image are generated It is observed that Interferometric SSC data of 28(th) August, 2008 and 08th September, 2008 give some fringes outside glacier area and complete decorrelation is shown on the Gangotri glacier due to high movement of glacier
引用
收藏
页码:3757 / 3760
页数:4
相关论文
共 15 条
[1]  
Eineder M., 2003, P FRINGE 2003 WORKSH
[2]   Nonlinear subsidence rate estimation using permanent scatterers in differential SAR interferometry [J].
Ferretti, A ;
Prati, C ;
Rocca, F .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2000, 38 (05) :2202-2212
[3]   MAPPING SMALL ELEVATION CHANGES OVER LARGE AREAS - DIFFERENTIAL RADAR INTERFEROMETRY [J].
GABRIEL, AK ;
GOLDSTEIN, RM ;
ZEBKER, HA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B7) :9183-9191
[4]   SATELLITE RADAR INTERFEROMETRY FOR MONITORING ICE-SHEET MOTION - APPLICATION TO AN ANTARCTIC ICE STREAM [J].
GOLDSTEIN, RM ;
ENGELHARDT, H ;
KAMB, B ;
FROLICH, RM .
SCIENCE, 1993, 262 (5139) :1525-1530
[5]   Velocities and flux of the Filchner ice shelf and its tributaries determined from speckle tracking interferometry [J].
Gray, AL ;
Short, N ;
Mattar, KE ;
Jezek, KC .
CANADIAN JOURNAL OF REMOTE SENSING, 2001, 27 (03) :193-206
[6]   Ice-sheet velocity mapping: a combined interferometric and speckle-tracking approach [J].
Joughin, I .
ANNALS OF GLACIOLOGY, VOL 34, 2002, 2002, 34 :195-201
[7]   RADAR INTERFEROMETRIC MAPPING OF DEFORMATION IN THE YEAR AFTER THE LANDERS EARTHQUAKE [J].
MASSONNET, D ;
FEIGL, K ;
ROSSI, M ;
ADRAGNA, F .
NATURE, 1994, 369 (6477) :227-230
[8]   DEFLATION OF MOUNT ETNA MONITORED BY SPACEBORNE RADAR INTERFEROMETRY [J].
MASSONNET, D ;
BRIOLE, P ;
ARNAUD, A .
NATURE, 1995, 375 (6532) :567-570
[9]   THE DISPLACEMENT FIELD OF THE LANDERS EARTHQUAKE MAPPED BY RADAR INTERFEROMETRY [J].
MASSONNET, D ;
ROSSI, M ;
CARMONA, C ;
ADRAGNA, F ;
PELTZER, G ;
FEIGL, K ;
RABAUTE, T .
NATURE, 1993, 364 (6433) :138-142
[10]   Radar interferometry and its application to changes in the earth's surface [J].
Massonnet, D ;
Feigl, KL .
REVIEWS OF GEOPHYSICS, 1998, 36 (04) :441-500