The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains

Glacier surges (GSs) are a manifestation of glacier instability and one of the most striking phenomena in the mountain cryosphere. Here, we utilize optical images acquired between 1973 and 2021 to map changes in glacier surface velocity and morphology and characterize differences in surface elevation using multi-source DEMs in the Tuanjie Peak (TJP), located in the Qilian Mountains (QLMs). These data provide valuable insights into the recent dynamic evolution of glaciers and hint at how they might evolve in the next few years. We identified a confirmed surge-type glacier (STG), three likely STGs, and three possible STGs. Our observations show that TJP GSs are generally long-term, although they are shorter in some cases. During the active phase, all glaciers exhibit thickened reservoir areas and thinned receiving areas, or vice-versa. The ice volume transfer was between 0.11 +/- 0.13 x 10(7) m(3) to 5.71 +/- 0.69 x 10(7) m(3). Although it was impossible to obtain integrated velocity profiles throughout the glacier surge process due to the limitations of available satellite imagery, our recent observations show that winter velocities were much higher than summer velocities, suggesting an obvious correlation between surge dynamics and glacial hydrology. However, the initiation and termination phase of GSs in this region was slow, which is similar to Svalbard-type STGs. We hypothesize that both thermal and hydrological controls are crucial. Moreover, we suggest that the regional warming trend may potentially increase glacier instability and the possibility of surge occurrence in this region.

Automated summary

This study examines glacier surges in the Tuanjie Peak region of the Qilian Mountains using optical images and multi-source DEMs. The researchers identify several confirmed and likely surge-type glaciers and analyze changes in surface velocity, morphology, and elevation. The findings suggest a correlation between surge dynamics and glacial hydrology, with the possibility of increased glacier instability in the region due to regional warming trends.