Digital elevation model of King Edward VII Peninsula, West Antarctica, from SAR interferometry and ICESat laser altimetry

被引:13
作者
Baek, S [1 ]
Kwoun, OI
Braun, A
Lu, Z
Shum, CK
机构
[1] Ohio State Univ, Lab Space Geodesy & Remote Sensing, Columbus, OH 43210 USA
[2] US Geol Survey Natl Ctr, Earth Resources Observat Syst Data Ctr, Sci Applicat Int Corp, Sioux Falls, SD 57198 USA
[3] Univ Calgary, Dept Geomat Engn, Calgary, AB T2N 1N4, Canada
基金
美国国家科学基金会;
关键词
glaciology; Ice; Cloud and Land Elevation Satellite (ICESat); snow and ice; space geodetic surveys; synthetic aperture radar (SAR);
D O I
10.1109/LGRS.2005.853623
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a digital elevation model (DEM) of King Edward VII Peninsula, Sulzberger Bay, West Antarctica, developed using 12 European Remote Sensing (ERS) synthetic aperture radar (SAR) scenes and 24 Ice, Cloud, and land Elevation Satellite (ICESat) laser altimetry profiles. We employ differential interfer-ograms from the ERS tandem mission SAR scenes acquired in the austral fall of 1996, and four selected ICESat laser altimetry profiles acquired in the austral fall of 2004, as ground control points (GCPs) to construct an improved geocentric 60-m resolution DEM over the grounded ice region. We then extend the DEM to include two ice shelves using ICESat profiles via Kriging. Twenty additional ICESat profiles acquired in 2003-2004 are used to assess the accuracy of the DEM. After accounting for radar penetration depth and predicted surface changes, including effects due to ice mass balance, solid Earth tides, and glacial isostatic adjustment, in part to account for the eight-year data acquisition discrepancy, the resulting difference between the DEM and ICESat profiles is -0.57 +/- 5.88 m. After removing the discrepancy between the DEM and ICESat profiles for a final combined DEM using a bicubic spline, the overall difference is 0.05 +/- 1.35 m.
引用
收藏
页码:413 / 417
页数:5
相关论文
共 22 条
[1]  
[Anonymous], GLAS ICESAT L2 ANTAR
[2]  
BRAUN A, 2004, I NAV ION 60 ANN M D
[3]   Analysis of the 1993-95 Bering Glacier (Alaska) surge using differential SAR interferometry [J].
Fatland, DR ;
Lingle, CS .
JOURNAL OF GLACIOLOGY, 1998, 44 (148) :532-546
[4]   SATELLITE RADAR INTERFEROMETRY - TWO-DIMENSIONAL PHASE UNWRAPPING [J].
GOLDSTEIN, RM ;
ZEBKER, HA ;
WERNER, CL .
RADIO SCIENCE, 1988, 23 (04) :713-720
[5]   Influence of ionospheric electron density fluctuations on satellite radar interferometry [J].
Gray, AL ;
Mattar, KE ;
Sofko, G .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (10) :1451-1454
[6]  
Hensley S., 2001, DIGITAL ELEVATION MO, P143
[7]   Penetration depths inferred from interferometric volume decorrelation observed over the Greenland ice sheet [J].
Hoen, EW ;
Zebker, HA .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2000, 38 (06) :2571-2583
[8]  
Jezek KC, 2002, RAMP AMM 1 SAR IMAGE
[9]   Measurement of ice-sheet topography using satellite radar interferometry [J].
Joughin, I ;
Winebrenner, D ;
Fahnestock, M ;
Kwok, R ;
Krabill, W .
JOURNAL OF GLACIOLOGY, 1996, 42 (140) :10-22
[10]   Ice sheet motion and topography from radar interferometry [J].
Kwok, R ;
Fahnestock, MA .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1996, 34 (01) :189-200