Hypsometry of Glacier AX010 in the Shorong region, Nepal Himalaya

This archive contains hypsometry (area-elevation distribution) of Glacier AX010 in the SHorong region, Nepal Himalaya. Description of the datasheetz: Elevation band covering +/- 10 m (m a.s.l.)For instance, z4930 means elevation band from 4920 to 4940h: Area (m^2)four digit with h: Year Median elevation (m a.s.l.) and total area (km^2) are summarized below.1978: 5218 / 0.5991991: 5215 / 0.5391999: 5194 / 0.4012008: 5196 / 0.3392023: 5175 / 0.185 Citation:Ageta Y, Ohata T, Tanaka Y, Ikegami K, Higuchi K (1980) Mass balance of Glacier AX010 in Shorong Himal, east Nepal during the summer monsoon season. Journal of the Japanese Society of Snow and Ice, 41, 34-41.Fujita K, Kadota T, Rana B, Kayastha RB, Ageta Y (2001) Shrinkage of Glacier AX010 in Shorong region, Nepal Himalayas in the 1990s. Bulletin of Glaciological Research, 18, 51-54.Fujita K, Nuimura T (2011) Spatially heterogeneous wastage of Himalayan glaciers. Proceedings of the National Academy of Sciences of the United States of America, 108(34), 14011-14014, doi:10.1073/pnas.1106242108Fujita K, Kayashta RB (in review) Temperature-driven shrinkage of a disappearing Himalayan glacier. The Cryoshpere.本归档数据集包含尼泊尔喜马拉雅山脉绍龙（SHorong）地区AX010冰川的高程面积分布（hypsometry，即面积-高程分布）数据。 数据集说明：高程带跨度为±10米（海拔高程，m a.s.l.）。例如，z4930代表4920至4940米的高程区间。h代表面积（单位：平方米，m²）；带有四位数字的h字段代表年份。 以下汇总了中位高程（单位：米海拔，m a.s.l.）与总面积（单位：平方千米，km²）数据： 1978年：5218 / 0.599 1991年：5215 / 0.539 1999年：5194 / 0.401 2008年：5196 / 0.339 2023年：5175 / 0.185 引用文献： Ageta Y, Ohata T, Tanaka Y, Ikegami K, Higuchi K (1980) 尼泊尔东部绍龙喜马拉雅地区AX010冰川夏季季风期物质平衡. 《日本雪冰学会志》, 41, 34-41. Fujita K, Kadota T, Rana B, Kayastha RB, Ageta Y (2001) 尼泊尔喜马拉雅山脉绍龙地区AX010冰川在20世纪90年代的退缩. 《冰川学研究通报》, 18, 51-54. Fujita K, Nuimura T (2011) 喜马拉雅冰川的空间异质性消融. 《美国国家科学院院刊》, 108(34), 14011-14014, doi:10.1073/pnas.1106242108 Fujita K, Kayashta RB (已投稿待刊) 温度驱动的喜马拉雅消亡冰川退缩机制. 《冰冻圈》(The Cryoshpere).