Abstract. The China–Pakistan Economic Corridor (CPEC) is one of the flagship
projects of the One Belt One Road Initiative, which faces threats from water
shortage and mountain disasters in the high-elevation region, such as
glacial lake outburst floods (GLOFs). An up-to-date high-quality glacial
lake dataset with parameters such as lake area, volume, and type, which is
fundamental to water resource and flood risk assessments and prediction of
glacier–lake evolutions, is still largely absent for the entire CPEC. This
study describes a glacial lake dataset for the CPEC using a threshold-based
mapping method associated with rigorous visual inspection workflows. This
dataset includes (1) multi-temporal inventories for 1990, 2000, and 2020
produced from 30 m resolution Landsat images and (2) a glacial lake
inventory for the year 2020 at 10 m resolution produced from Sentinel-2
images. The results show that, in 2020, 2234 lakes were derived from the
Landsat images, covering a total area of 86.31±14.98 km2 with a
minimum mapping unit (MMU) of 5 pixels (4500 m2), whereas 7560 glacial lakes
were derived from the Sentinel-2 images with a total area of 103.70±8.45 km2 with an MMU of 5 pixels (500 m2). The
discrepancy shows that Sentinel-2 can detect a large quantity of
smaller lakes compared to Landsat due to its finer spatial resolution. Glacial lake data in 2020 were validated by Google Earth-derived lake
boundaries with a median (± standard deviation) difference of
7.66±4.96 % for the Landsat-derived product and 4.46±4.62 %
for the Sentinel-derived product. The total number and area of glacial lakes
from consistent 30 m resolution Landsat images remain relatively stable
despite a slight increase from 1990 to 2020. A range of critical attributes
has been generated in the dataset, including lake types and mapping
uncertainty estimated by an improved equation of Hanshaw and Bookhagen (2014). This comprehensive
glacial lake dataset has the potential to be widely applied in studies on
water resource assessment, glacial lake-related hazards, and glacier–lake
interactions and is freely available at
https://doi.org/10.12380/Glaci.msdc.000001 (Lesi et al., 2022).