Uncrewed aircraft system landing zone in Bridger Mountains
Detailed Description
The Uncrewed Aircraft System (UAS) landing zone with the study site in the background. Bridger Mountains, MT.
Sources/Usage
Public Domain.
Related
USGS Snow and Avalanche Project
Snow avalanches are a widespread natural hazard to humans and infrastructure as well as an important landscape disturbance affecting mountain ecosystems. Forecasting avalanche frequency is challenging on various spatial and temporal scales, and this project aims to fill a gap in snow science by focusing on reconstructing avalanche history on the continental mountain range scale - throughout the...
Assessing the seasonal evolution of snow depth spatial variability and scaling in complex mountain terrain
Dynamic natural processes govern snow distribution in mountainous environments throughout the world. Interactions between these different processes create spatially variable patterns of snow depth across a landscape. Variations in accumulation and redistribution occur at a variety of spatial scales, which are well established for moderate mountain terrain. However, spatial patterns of snow depth v
Authors
Zachary Miller, Erich Peitzsch, Eric A. Sproles, Karl W. Birkeland, Ross T. Palomaki
Related
USGS Snow and Avalanche Project
Snow avalanches are a widespread natural hazard to humans and infrastructure as well as an important landscape disturbance affecting mountain ecosystems. Forecasting avalanche frequency is challenging on various spatial and temporal scales, and this project aims to fill a gap in snow science by focusing on reconstructing avalanche history on the continental mountain range scale - throughout the...
Assessing the seasonal evolution of snow depth spatial variability and scaling in complex mountain terrain
Dynamic natural processes govern snow distribution in mountainous environments throughout the world. Interactions between these different processes create spatially variable patterns of snow depth across a landscape. Variations in accumulation and redistribution occur at a variety of spatial scales, which are well established for moderate mountain terrain. However, spatial patterns of snow depth v
Authors
Zachary Miller, Erich Peitzsch, Eric A. Sproles, Karl W. Birkeland, Ross T. Palomaki