Discussions https://doi.org/10.5194/essd-2020-71 Earth System Preprint. Discussion started: 7 September 2020 Science c Author(s) 2020. CC BY 4.0 License. Open Access Open Data 1 Consolidating the Randolph Glacier Inventory and the Glacier 2 Inventory of China over the Qinghai-Tibetan Plateau and th 3 Investigating Glacier Changes Since the mid-20 Century 4 Xiaowan Liu1,2,3, Zongxue Xu1,2, Hong Yang3,4, Xiuping Li5, Dingzhi Peng1,2 5 1College of Water Sciences, Beijing Normal University, Beijing, 100875, China 6 2Beijiing Key Laboratory of Urban Hydrological Cycle and Sponge City Technology, Beijing, 100875, China 7 3Eawag, Swiss Federal Institute of Aquatic Science and Technology, 8600 Dübendorf, Switzerland 8 4Department of Environmental Science, MGU University of Basel, Petersplatz 1, 4001, Switzerland 9 5Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China 10 Correspondence to: Zongxue Xu (
[email protected]) 11 Abstract. Glacier retreat in the Qinghai-Tibetan Plateau (QTP), the ‘third pole of the world’, has attracted the 12 attention of researchers worldwide. Glacier inventories in the 1970s and the 2000s provide valuable information 13 to infer changes in individual glaciers. However, individual glacier volumes are either missing, incomplete or have 14 large errors in these inventories, and thus, the use of these datasets to investigate changes in glaciers in QTP in the 15 past few decades has become a challenge, particularly in the context of climate change. In this study, individual 16 glacier volume data in the Randolph Glacier Inventory version 4.0 (RGI 4.0, 1970s) and the second Glacier 17 Inventory of China (GIC-Ⅱ, 2000s) are recalculated and consolidated using a slope-dependent algorithm based on 18 elevation datasets for the QTP.