Articles | Volume 9, issue 3
https://doi.org/10.5194/tc-9-865-2015
https://doi.org/10.5194/tc-9-865-2015
Research article
 | 
06 May 2015
Research article |  | 06 May 2015

Climate regime of Asian glaciers revealed by GAMDAM glacier inventory

A. Sakai, T. Nuimura, K. Fujita, S. Takenaka, H. Nagai, and D. Lamsal

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Cited articles

Adam, J. C., Clark, E. A., Lettenmaier, D. P., and Wood, E. F.: Correction of global precipitation products for orographic effects, J. Climate, 19, 15–38, 2006.
Ageta, Y. and Higuchi, K.: Estimation of mass balance components of summer-accumulation type glacier in the Nepal Himalaya, Geogr. Ann. A, 66, 249–255, 1984.
Aizen, V. B., Aizen, E. M., Joswiak, D. R., Fujita, K., Takeuchi, N., and Nikitin, S. A.: Climatic and atmospheric circulation pattern variability from ice-core isotope/geochemistry records (Altai, Tien Shan and Tibet), Ann. Glaciol., 43, 49–60, 2006a.
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Bajracharya, S. R. and Shrestha, B. (Eds.): The status of glaciers in the Hindu Kush-Himalayan region, International Centre for Integrated Mountain Development, Kathmandu, 2011.
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Short summary
Among meteorological elements, precipitation has a large spatial variability and less observation, particularly in high-mountain Asia, although precipitation in mountains is an important parameter for hydrological circulation. Based on the GAMDAM glacier inventory, we estimated precipitation contributing to glacier mass at the median elevation of glaciers, which is presumed to be at equilibrium-line altitude, by tuning adjustment parameters of precipitation.