In many major Asian river basins, glaciers and seasonal snow play special role in regional water cycle as the principal meltwater resources. Climate Change (CC) in the past 50 years had profound impact on the water storage capacity of glaciers and seasonal snow, which in turn affected the amount of meltwater entering stream flow. The materials at this site present the results of the first comprehensive basin-scale assessment of the storage properties of glaciers and seasonal snow, and their contribution to Mean Annual River Flow (MAF) in six major Asian river basins: the Indus, Ganges, Brahmaputra, Amu Darya, Syr Darya and Mekong, which was carried at IWMI in 2012-2013. These are supplementary materials illustrating the states of melt water resources at two time slices: 1961-90 (baseline) and 2001-2010 (current) and the differences in their states between these two time periods. The key findings, methodology and accuracy ranges of the meltwater resources assessment can be found in issues 149 and 150 of IWMI Research reports series (Savoskul and Smakhtin, 2013-a, 2013-b)