Hostname: page-component-cd9895bd7-hc48f Total loading time: 0 Render date: 2024-12-30T20:40:06.442Z Has data issue: false hasContentIssue false

Automated detection and temporal monitoring of crevasses using remote sensing and their implications for glacier dynamics

Published online by Cambridge University Press:  03 March 2016

Anshuman Bhardwaj*
Affiliation:
TERI University, New Delhi, India Sharda University, Greater Noida, India
Lydia Sam
Affiliation:
Sharda University, Greater Noida, India Defence Research & Development Organisation, New Delhi, India
Shaktiman Singh
Affiliation:
Sharda University, Greater Noida, India
Rajesh Kumar
Affiliation:
Sharda University, Greater Noida, India
*
Correspondence: Anshuman Bhardwaj <[email protected]>
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Detailed studies on temporal changes of crevasses and their linkage with glacier dynamics are scarce in the Himalayan context. Observations of temporally changing surficial crevasse patterns and their orientations are suggestive of the processes that determine seasonal glacier flow characteristics. In the present study, on a Himalayan valley glacier, changing crevasse patterns and orientations were detected and mapped on Landsat 8 images in an automated procedure using the ratio of Thermal Infrared Sensor (TIRS) band 10 to Optical Land Imager (OLI) shortwave infrared (SWIR) band 6. The ratio was capable of mapping even crevasses falling under mountain shadows. Differential GPS observations suggested an average error of 3.65% and root-mean-square error of 6.32m in crevasse lengths. A year-round observation of these crevasses, coupled with field-based surface velocity measurements, provided some interesting interpretations of seasonal glacier dynamics.

Type
Paper
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s) 2016

References

Bhardwaj, A and 6 others (2015a) Applicability of Landsat 8 data for characterizing glacier facies and supraglacial debris. Int. J. Appl. Earth Obs. Geoinf., 38, 5164 (doi: 10.1016/j.jag.2014.12.011)Google Scholar
Bhardwaj, A and 7 others (2015b) A Lake Detection Algorithm (LDA) using Landsat 8 data: a comparative approach in glacial environment. Int. J. Appl. Earth Obs. Geoinf., 38, 150163 (doi: 10.1016/j.jag.2015.01.004)Google Scholar
Bindschadler, RA and Scambos, TA (1991) Satellite-image derived velocity field of an Antarctic ice stream. Science, 252(5003), 242246 (doi: 10.1126/science.252.5003.242)Google Scholar
Dowdeswell, JA and Collin, RL (1990) Fast-flowing outlet glaciers on Svalbard ice caps. Geology, 18(8), 778781 (doi: 10.1130/0091-7613(1990)018<0778:FFOGOS>2.3.CO;2)Google Scholar
Eder, K, Reidler, C, Mayer, C and Leopold, M (2008) Crevasse detection in alpine areas using ground penetrating radar as a component for a mountain guide system. Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., 37(B8), 837842 Google Scholar
Hambrey, MJ and Muller, F (1978) Structures and ice deformation in the White Glacier, Axel Heiberg Island, Northwest Territories, Canada. J. Glaciol., 20(82), 4166 Google Scholar
Harper, JT, Humphrey, NF and Pfeffer, WT (1998) Crevasse patterns and the strain-rate tensor: a high resolution comparison. J. Glaciol., 44, 6877 Google Scholar
Holdsworth, G (1969) Primary transverse crevasses. J. Glaciol., 8, 107129 Google Scholar
RLeB, Hooke (2005) Principles of glacier mechanics. Cambridge University Press, Cambridge, 106107 Google Scholar
Hughes, T (1983) On the disintegration of ice shelves: the role of fracture. J. Glaciol., 29(101), 98117 Google Scholar
Joshi, PK, Ghosh, A, Chakraborty, A, Sharma, R and Joshi, A (2013) Landsat again – continuing remote sensing, monitoring, mapping and measuring. Curr. Sci., 105(6), 761763 Google Scholar
Lever, JH, Delaney, AJ, Ray, LE, Trautmann, E, Barna, LA and Burzynski, AM (2013) Autonomous GPR surveys using the Polar Rover Yeti. J. Field Robotics, 30(2), 194215 (doi: 10.1002/rob.21445)Google Scholar
Lu, D, Mausel, P, Brondizio, E and Moran, E (2002) Assessment of atmospheric correction methods for Landsat TM data applicable to Amazon basin LBA research. Int. J. Remote Sens., 23(13), 26512671 (doi: 10.1080/01431160110109642)Google Scholar
Luckman, A, Jansen, D, Kulessa, B, King, EC, Sammonds, P and Benn, DI (2012) Basal crevasse in Larsen C ice shelf and implications for their global abundance. Cryosphere, 6(1), 113123 (doi: 10.5194/tc-6-113-2012)Google Scholar
Mitchell, A (2005) The ESRI guide to GIS analysis, vol. 2. ESRI Press, Redland, CA Google Scholar
Naesset, E (2001) Effects of differential single- and dual-frequency GPS and GLONASS observations on point accuracy under forest canopies. Photogramm. Eng. Remote Sens., 67(9), 10211026 Google Scholar
Paterson, WSB (1994) The physics of glaciers, 3rd edn. Elsevier Science, Oxford and New York, 187190 Google Scholar
Retzlaff, R and Bentley, CR (1993) Timing of stagnation of Ice Stream C, West Antarctica, from short pulse radar studies of buried surface crevasses. J. Glaciol., 39, 495506 Google Scholar
Rifman, SS (1973) Digital rectification of ERTS multispectral imagery. NASA Spec. Publ. 327, 11311142 Google Scholar
Shabtaie, S and Bentley, CR (1987) West Antarctic ice streams draining into the Ross Ice Shelf: configuration and mass balance. J. Geophys. Res., 92, 13111336 (doi: 10.1029/JB092iB02p01311)Google Scholar
Singh, KK and 6 others (2013) Crevasses detection in Himalayan glaciers using ground-penetrating radar. Curr. Sci., 105(9), 12881295 Google Scholar
Taurisano, A, Tronstad, S, Brandt, O and Kohler, J (2006) On the use of ground penetrating radar for detecting and reducing crevasse hazard in Dronning Maud Land, Antarctica. Cold Reg. Sci. Technol., 45, 166177 (doi: 10.1016/j.coldregions.2006.03.005)Google Scholar
Van der Veen, CJ (1998) Fracture mechanics approach to penetration of surface crevasses on glaciers. Cold Reg. Sci. Technol., 27, 3147 (doi: 10.1016/S0165-232X(97)00022-0)Google Scholar
Vaughan, DG (1993) Relating the occurrence of crevasses to surface strain rates. J. Glaciol., 39(132), 255266 Google Scholar
Vornberger, PL and Whillans, IM (1986) Surface features of Ice Stream B, Marie Byrd Land, West Antarctica. Ann. Glaciol., 8, 168170 Google Scholar
Vornberger, PL and Whillans, IM (1990) Crevasse deformation and examples from Ice Stream B, Antarctica. J. Glaciol., 36, 39 Google Scholar
Whillans, IM and Tseng, YH (1995) Automatic tracking of crevasses on satellite images. Cold Reg. Sci. Technol., 23, 201214 (doi: 10.1016/0165-232X(94)00009-M)Google Scholar
Whillans, IM, Jackson, M and Tseng, YH (1993) Velocity pattern in a transect across Ice Stream B, Antarctica. J. Glaciol., 39, 562572 Google Scholar
Zamora, R and 7 others (2007) Crevasse detection in glaciers of southern Chile and Antarctica by means of ground penetrating radar. IAHS Publ. 318 (Assembly in Foz do lguaçu 2005 – Glacier Mass Balance Change and Meltwater Discharge)Google Scholar
Zhang, Y (2004) Understanding image fusion. Photogramm. Eng. Remote Sens., 70(6), 657661 Google Scholar
Zhou, C, Dongchen, E, Wang, Z and Sun, J (2008) Remote sensing application in Antarctic inland areas. Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., 37(B8), 819824 Google Scholar