ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., III-8, 71-78, 2016
https://doi.org/10.5194/isprs-annals-III-8-71-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
 
07 Jun 2016
REMOTELY-SENSED GLACIER CHANGE ESTIMATION: A CASE STUDY AT LINDBLAD COVE, ANTARCTIC PENINSULA
K. D. Fieber1, J. P. Mills1, P. E. Miller2, and A. J. Fox3 1School of Civil Engineering and Geosciences, Newcastle University, NE1 7RU, UK
2James Hutton Institute, Craigiebuckler, Aberdeen, AB15 8QH, UK
3British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Keywords: Glacier Change, Antarctic Peninsula, Photogrammetry, WorldView-2, Archival Photography, DEM, Surface Matching Abstract. This study builds on existing literature of glacier change estimation in polar regions and is a continuation of efforts aimed at unlocking the information encapsulated in archival aerial photography of Antarctic Peninsula glaciers. Historical aerial imagery acquired in 1957 over three marine-terminating glaciers at Lindblad Cove on the West Coast of Trinity Peninsula is processed to extract digital elevation models (DEMs) which are subsequently compared to DEMs generated from present day (2014) WorldView-2 satellite stereo-imagery. The new WorldView-2 images offer unprecedented sub-metre resolution of the Antarctic Peninsula and are explored here to facilitate improved registration and higher accuracy analysis of glacier changes. Unlike many studies, which focus on glacier fronts or only restricted regions of glaciers, this paper presents a complete coverage of elevation changes across the glacier surfaces for two of the studied glaciers. The study utilises a robust least squares matching technique to ensure precise registration of the archival and modern DEMs, which is applied due to lack of existing ground control in this remote region. This case study reveals that, while many glaciers in polar regions are reported as experiencing significant mass loss, some glaciers are stable or even demonstrate mass gain. All three glaciers reported here demonstrated overall mean increases in surface elevation, indicative of positive mass balance ranging from 0.6 to 5.8 metre water equivalent between 1957 and 2014.
Conference paper (PDF, 2011 KB)


Citation: Fieber, K. D., Mills, J. P., Miller, P. E., and Fox, A. J.: REMOTELY-SENSED GLACIER CHANGE ESTIMATION: A CASE STUDY AT LINDBLAD COVE, ANTARCTIC PENINSULA, ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., III-8, 71-78, https://doi.org/10.5194/isprs-annals-III-8-71-2016, 2016.

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