Abstract
As part of the on-going annual mass balance measurements on Batal and Sutri Dhaka glaciers, observations were made during peak ablation (August–September) season in 2013 to understand the response of debris covered and clean-ice (debris free) glacier surface to melting processes. Though, both the Batal and Sutri Dhaka glaciers have almost similar geographical disposition, Batal shows extensive debris cover (90% of the ablation area), while the latter is free from debris (only 5% of the ablation area). The thickness of debris in Batal glacier is inversely proportional to altitude, whereas Sutri Dhaka mostly experienced debris-free zone except snout area. Observation revealed that the vertical gradient of ablation rate in ablation area is contrastingly opposite in these two glaciers, reflecting significant control of debris thickness and their distribution over glacier surface on the ablation rates. While different thickness (2–100 cm) of debris have attenuated melting rates up to 70% of total melting, debris cover of <2 cm thickness has accelerated melting up to 10% of the total melting. Estimated melt ratio reveals that about 90% of the ablation area has experienced inhibited melting in Batal glacier, whereas only less than 5% ablation area of Sutri Dhaka has undergone inhibited melting. Comparison of topographical maps of 1962 with successive satellite images of the area demonstrates a terminus retreat of 373 ± 33.5 m and 579 ± 33.5 m for Batal and Sutri Dhaka glaciers for the period 1962–2013, respectively.
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Acknowledgements
This work has been funded by National Centre for Antarctic and Ocean Research, Ministry of Earth Sciences, Government of India, under the program ‘Cryosphere and Climate’. We heartily acknowledge and thank to Dr Shailesh Nayak, Secretary, ESSO-MoES for his support to run the field expedition and giving valuable scientific suggestions for improving the quality of the paper. We also thank Dr S Rajan, Director, ESSO-NCAOR for his unconditional support. We thank the National Remote Sensing Centre (NRSC) and the United State Geological Survey (USGS) for providing satellite data and Survey of India for providing the toposheets for our study area. We thank our field assistant, Mr B B Adhikari and the porters who were involved in our field trips, and ABVIMAS, Manali for providing some of the facilities to carry out this work. We are also thankful to IITM, Pune for facilitating necessary instruments that enabled us to collect meteorological data during the field.
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Sharma, P., Patel, L.K., Ravindra, R. et al. Role of debris cover to control specific ablation of adjoining Batal and Sutri Dhaka glaciers in Chandra Basin (Himachal Pradesh) during peak ablation season. J Earth Syst Sci 125, 459–473 (2016). https://doi.org/10.1007/s12040-016-0681-2
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DOI: https://doi.org/10.1007/s12040-016-0681-2