A new retrogressive thaw slump (RTS) inventory in central Qinghai–Tibet Plateau (QTP) were generated based on visual interpretation of nine satellite images (WV-2, Google Earth image, Ziyuan-3, Gaofen-2, Gaofen-1) and field investigations. A total 459 RTSs were confirmed with an accumulative area of 1199.49 ha (in time slice of 2018-2020). To reduce the uncertainty in identifying the RTS boundaries, all of the images were spatially corrected based on a reference image, which was obtained on 29 December 2015. The RTS inventory published by Luo et al., (2022) and Xia et al., (2022) were refered when we conduct visual interpretation. Note: the RTSs were distingusihed into active RTSs (TYPE=Y) and non-active RTSs (TYPE=N). Those RTSs were neither active nor non-active RTSs when their area increase vary from 0 to 0.01 ha or less than 0 (TYPE=T). The field named "area_ha", "perime_km" are the area and perimeter of the RTSs in the attribute tables of shapefiles. The units of area and perimeters are hectare (ha) and kilometer (km), respectively. The field named "type" indicates the status of RTSs. The "Y" and "N" are means the RTS is belongs to active RTS and non-active, respectively.

{"references": ["Luo, J., Niu, F., Lin, Z., Liu, M., Yin, G., & Gao, Z. (2022). Inventory and frequency of retrogressive thaw slumps in permafrost region of the Qinghai\u2013Tibet Plateau. Geophysical Research Letters, 49(23), e2022GL099829. doi.org/10.1029/2022GL099829", "Xia, Z., Huang, L., Fan, C., Jia, S., Lin, Z., Liu, L., ... & Zhang, T. (2022). Retrogressive thaw slumps along the Qinghai\u2013Tibet Engineering Corridor: a comprehensive inventory and their distribution characteristics. Earth System Science Data, 14(9), 3875-3887."]}