Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-25T03:20:32.018Z Has data issue: false hasContentIssue false

Glacial retreat in the Baspa basin, Himalaya, monitored with satellite stereo data

Published online by Cambridge University Press:  08 September 2017

Anil V. Kulkarni
Affiliation:
Space Applications Centre (ISRO), Ahmedabad 380 015, India E-mail: [email protected]
I. M. Bahuguna
Affiliation:
Space Applications Centre (ISRO), Ahmedabad 380 015, India E-mail: [email protected]
Rights & Permissions [Opens in a new window]

Abstract

Type
Correspondence
Copyright
Copyright © The Author(s) 2002

The Editor,

Journal of Glaciology

Sir,

The Himalaya contain one of the largest concentrations of glaciers outside of the polar regions. Meltwater from these glaciers forms an important source of run-off in northern India during the summer months. This run-off is likely to change, as extensive glacier retreat is reported in the Himalaya and other parts of the world (Reference Dhobal, Kumar and MundepiDhobal and others, 1995; Reference Holmlund and FuenzalidaHolmlund and Fuenzalida, 1995). Himalayan glacier retreat is normally difficult to study due to the rugged, mountainous terrain, but remote sensing offers a useful tool that can be used to assess information about glacier features such as accumulation area, snowline and moraine-dammed lakes (Reference KulkarniKulkarni, 1991). In this investigation, glacial retreat was estimated using high-resolution (5.8 m) stereo data from the Indian Remote Sensing Satellite-1C for the Baspa basin, a tributary of the Satluj River (Fig. 1).

Fig. 1. Baspa basin and glaciers. 1, Shaune Garang; 2, Bilare Bange; 3, Naradu Garang; 4, Janapa Garang; 5, Jorya Garang; 6, Karu Garang; 7, Baspa Bamak; 8, 53I11008.

An ortho-image is a map-aligned satellite image corrected for height distortion. The raw images contain geometric distortions due to satellite orbit, altitude variations, sensor geometry, tilt angle and terrain relief, but we correct for these distortions using ground-control points (GCP). GCP are stable ground features, which can easily be identified on topographic maps and satellite images. Digital photogrammetric techniques were used to generate a digital elevation model and ortho-images from raw images and the GCP.

Monitoring of glacier advance and retreat requires correct identification of the glacier snout. The snout is often an abrupt ice wall that can easily be identified when the glacier is viewed in a satellite stereo pair. Once identified, its location can be transferred to a topographic map by relating the snout position to nearby streams, lakes or other features. Snout positions for this study were verified with field observations carried out at Shaune Garang glacier.

The positions of glacier snouts for 1997–98 and 1962–63 were obtained from satellite images (Fig. 2) and Survey of India maps, respectively. All eight glaciers studied in the Baspa basin (Table 1) were in retreat. Retreat varied from 90 to 923 m. The lowest amount (90 m) was observed at Bilare Bange glacier, a small, low-altitude glacier. On satellite images it has a rough texture suggesting an extensive debris cover. Excessive debris can retard melting and protect a glacier from retreat (Reference ColbeckColbeck, 1988). Heavy debris cover makes small glaciers in the Himalaya less sensitive to climate change, in contrast to the Alps and Trans-Himalaya, where small glaciers react more quickly to changes in mass balance and climate change (Ding and Haeberli, 1996).

Fig 2. Retreat of Janapa Garang glacier.

Table 1. General characteristics and retreat of glaciers in the Baspa valley

Medium-size glaciers such as Naradu and Shaune Garang retreated 550–923 m. The mass balance on these glaciers is influenced by their area–altitude distribution. From 1987 to 1995 the equilibrium-line altitude (ELA) for Naradu glacier was 5030 m and its accumulation–area ratio (AAR) was 0.71, while the lower-altitude Shaune Garang glacier had an ELA of 4740 m and an AAR of 0.42, leading to a faster retreat rate on the lower glacier. Large glaciers such as Jorya Garang and Baspa Bamak retreated even less (425 and 380 m) than the medium-sized glaciers.

This study suggests that the 0.6 ± 0.2°C increase in global temperature of the last century (Reference HoughtonHoughton and others, 2001) has started to affect glaciers in the Himalaya. The rate of retreat is influenced by glacier size, area–altitude distribution and debris cover. In addition, the investigation has shown that satellite stereo data and ortho-images are useful for monitoring glacier retreat.

Acknowledgements

The authors would like to thank S. Nayak, Group Director, Marine and Water Resources Group, for suggestions and comments. We also thank M. Sturm, co-Chief Editor, Journal of Glaciology, for useful editorial suggestions.

12 November 2001

References

Colbeck, S. C. 1988. Snowmelt increase through albedo reduction. CRREL Spec. Rep. 88–26.Google Scholar
Dhobal, D. P., Kumar, S. and Mundepi, A. K. 1995. Morphology and glacier dynamics studies in monsoon–arid transition zone: an example from Chhota Shigri Glacier Himachal–Himalaya, India. Current Sci., 68(9), 936944.Google Scholar
Yongjian, Ding and Haeberli, W. 1996. Correspondence. Compilation of long-term glacier-fluctuation data in China and a comparison with corresponding records from Switzerland. J. Glaciol., 42(141), 390400.Google Scholar
Holmlund, P. and Fuenzalida, H. 1995. Anomalous glacier responses to 20th century climatic changes in Darwin Cordillera, southern Chile. J. Glaciol, 41(139), 465473.Google Scholar
Houghton, J. T. and 7 others, eds. 2001. The scientific basis: contribution of Working Group I to the third assessment report of the Intergovernmental Panel on Climate Change. Cambridge, etc., Cambridge University Press. Intergovernmental Panel on Climate Change.Google Scholar
Kulkarni, A. V. 1991. Glacier inventory in Himachal Pradesh using satellite data. J. Indian Soc. Remote Sensing, 19(3), 195203.Google Scholar
Figure 0

Fig. 1. Baspa basin and glaciers. 1, Shaune Garang; 2, Bilare Bange; 3, Naradu Garang; 4, Janapa Garang; 5, Jorya Garang; 6, Karu Garang; 7, Baspa Bamak; 8, 53I11008.

Figure 1

Fig 2. Retreat of Janapa Garang glacier.

Figure 2

Table 1. General characteristics and retreat of glaciers in the Baspa valley