My current research focuses on the investigation of the initiation and mobility of debris flows, which rank among the most complex and hazardous types of landslide phenomena. Given the unpredictability of debris flows, traditional in situ studies are not feasible, making experimental approaches essential. While the mechanics of debris flows and their initiation processes have been the subject of extensive research, there exists a notable gap in understanding the slope stability of buried ice, particularly in the context of retreating glaciers.

The disintegration of the cryosphere is associated with the melting of buried ice, which presents a new source of water that can elevate pore pressure, subsequently triggering landslides. This situation poses significant hazards to communities worldwide, necessitating urgent research. Addressing these concerns often relies on experimental setups, such as the large-scale experiments conducted at the USGS debris flow flume facility.