Seasonal and annual kinematics of active rock glaciers under different climate regimes in the Western USA
- 1Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, Los Angeles, CA, USA (alhandwerger@g.ucla.edu)
- 2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA (alexander.handwerger@jpl.nasa.gov)
- 3Earth, Marine and Environmental Sciences, University of North Carolina, Chapel Hill, NC, USA (ckluet@unc.edu)
- 4Civil & Environmental Engineering, University of Washington, Seattle, WA, USA (gbrench@uw.edu)
- 5Earth and Climate Sciences, Middlebury College, Middlebury, VT, USA (jmunroe@middlebury.edu)
Rock glaciers are common landforms in many alpine permaforst landscapes that play an important role in alpine hydrology and landscape evolution, principally through the release of seasonal meltwater and the downslope transport of coarse material. Here, we use satellite-based interferometric synthetic aperture radar (InSAR) to identify and monitor rock glaciers in the Western USA. We focus on the movement of active and transitional rock glaciers in Utah (Uinta, Wasatch, and La Sal Mountains), and Wyoming (Wind River Mountains) between 2015 and 2022. Using the new framework established by the International Permafrost Association (IPA) Action Group, we identified 255 active and transitional rock glaciers in the ~3500 km2 Uinta Mountains, 45 rock glaciers in the ~200 km2 La Sal Mountains, 55 rock glaciers in the ~135 km2 Wasatch Mountains, and 120 rock glaciers in the ~3000 km2 Wind River Mountains. These rock glaciers currently occur under different climatic regimes based on data from the 30 year (1991-2020) normal Parameter-elevation Relationships on Independent Slopes Model (PRISM). The La Sals and Wasatch are warmer and wetter with a mean annual air temperature (MAAT) of ~3.0± 1.9 ˚C and 2.7 ± 1.1 ˚C and a mean annual precipitation (MAP) of ~92 ± 13 cm and ~130 ± 17 cm, respectively, whereas the Uintas and Wind Rivers are cooler and drier with a MAAT of ~0.24 ± 1.4 ˚C and -0.87 ± 1.4 ˚C and a MAP of ~87 ± 11 cm and ~81 ± 10 cm. The mean line-of-sight (LOS) velocities for individual rock glaciers range from ~1 to 10 cm/yr. We also examined the time-dependent relationship between the motion of the rock glaciers and local climatic drivers such as temperature and precipitation. We found that rock glaciers exhibit seasonal and annual velocity changes, likely driven by liquid water availability (from snowmelt and rainfall), with accelerated motion during summers and during wetter years. Our findings demonstrate the ability to use satellite InSAR to monitor rock glaciers over large areas and provide insight into the environmental factors that control their kinematics.
How to cite: Handwerger, A. L., Kluetmeier, C., Brencher, G., and Munroe, J. S.: Seasonal and annual kinematics of active rock glaciers under different climate regimes in the Western USA, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-9092, https://doi.org/10.5194/egusphere-egu23-9092, 2023.
