2012
DOI: 10.3189/2012jog11j123
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From balance to imbalance: a shift in the dynamic behaviour of Chhota Shigri glacier, western Himalaya, India

Abstract: International audienceMass-balance and dynamic behaviour of Chhota Shigri Glacier have been investigated between 2002 and 2010 and compared to data collected in 1987/1989. During the period 2002/2010, the glacier experienced a negative glacier-wide mass balance of -0.67 ± 0.40 m/a w.e. Between 2003 and 2010, elevation and ice flow velocities are slowly decreasing in the ablation area leading to a 24 to 37% reduction in ice fluxes, an expected response of the glacier dynamics to its recent negative mass balance… Show more

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Cited by 186 publications
(146 citation statements)
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“…Mass-balance data for Chhota Shigri from 2002/03 to 2008/09 from the glaciological method are obtained from the literature 36,37 . Mass-balance estimates from field measurements for Hamtah glacier from 2001 to 2008 are taken from unpublished reports of the Geological Survey of India (GSI).…”
Section: In Situ Datamentioning
confidence: 99%
“…Mass-balance data for Chhota Shigri from 2002/03 to 2008/09 from the glaciological method are obtained from the literature 36,37 . Mass-balance estimates from field measurements for Hamtah glacier from 2001 to 2008 are taken from unpublished reports of the Geological Survey of India (GSI).…”
Section: In Situ Datamentioning
confidence: 99%
“…The ice thickness and bed topography results of Chhota Shigri were compared with the GPR measurements 15 . Maximum ice thickness and bed topography measurements are available for four cross-sections along the glacier (Figure 2 b).…”
mentioning
confidence: 99%
“…We applied the methodology to Chhota Shigri, one of the few well-studied glaciers in the Indian Himalaya for which GPR measurements are available 15 . The results obtained for Chhota Shigri were used to validate the methodology, which was thereafter applied to Drang Drung and Samudra Tapu.…”
mentioning
confidence: 99%
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“…However, the harsh topographic and weather conditions in the Himalayas are not favourable for detailed ground-based glaciological studies 1,7,8 . Due to limitations in field investigations [9][10][11][12] , remote sensing techniques such as the Accumulation Area Ratio (AAR) and Equilibrium Line Altitude (ELA) methods have been used to study the mass balance of glaciers in the Himalayas [13][14][15] . In addition, geodetic method (comparison of multi-temporal digital terrain models) has been used to estimate the glacier mass balance at basin and regional scales in the Himalayas 2,6,16,17 .…”
mentioning
confidence: 99%