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The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Articles | Volume XLIII-B3-2020
https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-1705-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-1705-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
22 Aug 2020
| 22 Aug 2020
CLOUD-BASED GEOSPATIAL PLATFORM IN SUPPORT OF SUSTAINABLE DEVELOPMENT GOALS 2030: HOW TO BE PREPARED FOR EARTHQUAKE DISASTERS?
S. Pirasteh
Department of Surveying and Geoinformatics, Faculty of Geosciences & Environmental Engineering, Southwest Jiaotong University (SWJTU), Chengdu, China
G. Shamsipour
Department of Surveying and Geoinformatics, Faculty of Geosciences & Environmental Engineering, Southwest Jiaotong University (SWJTU), Chengdu, China
G. Liu
Department of Surveying and Geoinformatics, Faculty of Geosciences & Environmental Engineering, Southwest Jiaotong University (SWJTU), Chengdu, China
R. Hajibagheri
Institute for Disaster Management (WIDM Inc.), GeoIME Inc. Mississauga, Canada
A. Ghasemzadeh
Institute for Disaster Management (WIDM Inc.), GeoIME Inc. Mississauga, Canada
M. Jokar
Institute for Disaster Management (WIDM Inc.), GeoIME Inc. Mississauga, Canada
H. Zarbakhsh
Institute for Disaster Management (WIDM Inc.), GeoIME Inc. Mississauga, Canada
F. Behnamfar
Institute for Disaster Management (WIDM Inc.), GeoIME Inc. Mississauga, Canada
J. Li
Department of Geography and Environmental Management, University of Waterloo, Canada
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Rock glaciers are abundant in high mountains in western China but have been ignored for 20 years. We used a new remote-sensing-based method to map active rock glaciers in the Chinese part of the Tien Shan and compiled an inventory of 261 active rock glaciers and included quantitative information about their locations, geomorphic parameters, and downslope velocities. Our dataset suggests that the lower limit of permafrost there is 2500–2800 m.
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