Journal of Geographical Sciences >
Surface velocity estimations of ice shelves in the northern Antarctic Peninsula derived from MODIS data
Author: Chen Jun, PhD Candidate, specialized in Remote Sensing and glaciology. E-mail: gischen@126.com
*Corresponding author: Ke Changqing, Professor, E-mail: kecq@nju.edu.cn
Received date: 2015-05-03
Accepted date: 2015-07-31
Online published: 2016-02-25
Supported by
National Nature Science Foundation of China, No.41371391
Chinese National Antarctic and Arctic Research Expedition, No.CHINARE2015-02-02
Specialized Research Fund for the Doctoral Program of Higher Education of China, No.20120091110017
A Project Funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD)
And this work was partially supported by Collaborative Innovation Center of Novel Software Technology and Industrialization
Copyright
The ice shelves in the northern Antarctic Peninsula are highly sensitive to variations of temperature and have therefore served as indicators of global warming. In this study, we estimate the velocities of the ice shelves in the northern Antarctic Peninsula using co-registration of optically sensed images and correlation module (COSI-Corr) in the Environment for Visualizing Images (ENVI) based on Moderate Resolution Imaging Spectroradiometer (MODIS) images during 2000-2012, from which we conclude that the ice flow directions generally match the peninsulas pattern and the crevasse, ice flows mainly eastward into the Weddell Sea. The spatial pattern of velocity field exhibits an increasing trend from the western grounding line to the maximum at the middle part of the ice shelf front on Larsen C with a velocity of approximately 700 ma-1, and the velocity field shows relatively higher values in its southerly neighboring ice shelf (e.g. Smith Inlet). Additionally, ice flows are relatively quicker in the outer part of the ice shelf than in the inner parts. Temporal changes in surface velocities show a continuous increase from 2000 to 2012. It is worth noting that, the acceleration rate during 2000-2009 is relatively higher than that during 2009-2012, while the ice movement on the southern Larsen C and Smith Inlet shows a deceleration from 2009 to 2012.
CHEN Jun , *KE Changqing , ZHOU Xiaobing , SHAO Zhude , LI Lanyu . Surface velocity estimations of ice shelves in the northern Antarctic Peninsula derived from MODIS data[J]. Journal of Geographical Sciences, 2016 , 26(2) : 243 -256 . DOI: 10.1007/s11442-016-1266-3
Figure 1 Location of the study area in the Antarctica. The underlying images are MODIS mosaics that are preprocessed by Haran et al. (2005). |
Figure 2 The ice shelf fronts in 2000, 2003, 2006, 2009 and 2012, respectively. The underlying images are MODIS mosaic in 2000. |
Table 1 MODIS L1B images used for the velocity estimation and their parameters |
Period1 | Period2 | Period3 | Period4 | Period5 |
---|---|---|---|---|
27-MAR-2000 (13:15) | 10-FEB-2003 (12:45) | 3-JAN-2006 (12:30) | 8-APR-2009 (14:15) | 19-JAN-2012 (13:25) |
29-MAR-2000 (13:05) | 20-MAR-2003 (13:45) | 5-JAN-2006 (14:45) | 1-JAN-2009 (13:10) | 25-JAN-2012 (12:50) |
24-AUG-2000 (14:15) | 8-APR-2003 (14:15) | 7-JAN-2006 (14:20) | 21-FEB-2012 (14:10) | |
26-AUG-2000 (15:40) | 18-APR-2003 (14:50) | 20-FEB-2006 (12:15) | 19-AUG-2012 (13:50) | |
24-SEP-2000 (11:55) | 11-DEC-2003 (14:50) | 10-NOV-2006 (12:35) | 23-AUG-2012 (13:25) |
Table 2 Root mean square errors of displacement measurements obtained using the cross-correlation coefficient (CCC) over stable bare rocks |
Image pairs | RMSEE-W (m) | RMSES-N (m) |
---|---|---|
2000/2003 | 54 | 62 |
2003/2006 | 46 | 56 |
2006/2009 | 61 | 71 |
2009/2012 | 47 | 52 |
Mean | 52 | 60 |
Figure 3 Spatial pattern of surface velocity of ice shelves in the northern Antarctic Peninsula during four periods (a. 2000/2003, b. 2003/2006, c. 2006/2009, and d. 2009/2012). The arrows in black indicate flow vector with quantities and directions at the 50 sample points with the best contrast on MODIS images (Figure 4). The underlying images are MODIS mosaic in 2006. |
Figure 4 Sketch map of 50 sample points. The ice at the sample points in blue shows a continuous acceleration; at the sample points in red shows that there is not any significant change in velocity; and at the sample points in green shows a deceleration from the period 2006-2009 to the period 2009-2012. The underlying images are MODIS mosaic in 2009. |
Figure 5 The mean velocity of 50 sample points with latitude and longitude during four periods |
Figure 6 Variation of mean velocity of 50 sample points during 2000-2012 |
The authors have declared that no competing interests exist.
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