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青藏高原东南部海洋型冰川物质平衡研究进展
赵银1(), 张勇1,2(), 刘时银3, 王欣1
Review of maritime glacier mass balance in the southeastern Tibetan Plateau
Yin ZHAO1(), Yong ZHANG1,2(), Shiyin LIU3, Xin WANG1

图1. 青藏高原东南部海洋型冰川分布(a),冰川面积随海拔高度变化特征(b)和不同面积等级冰川数量与面积特征(c),其中冰川数据来源于美国国家冰雪数据中心最新版本全球冰川编目数据30,图(b)中红线表示冰川面积随海拔高度呈正态分布

Fig. 1. Maritime glaciers in the southeastern Tibetan Plateau (a), glacier area-altitude distribution (b) and glacier distribution for different area size classes (c), glacier data are from RGI 6.030, red line in (b) denotes the normal distribution curve