Geomorphic and sedimentary effects of modern climate change: current and anticipated future conditions in the western United States
Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …
documented widely, but physical landscape responses are poorly understood thus far …
Modeling Post‐Wildfire Hydrologic Response: Review and Future Directions for Applications of Physically Based Distributed Simulation
Wildfire is a growing concern as climate shifts. The hydrologic effects of wildfire, which
include elevated hazards and changes in water quantity and quality, are increasingly …
include elevated hazards and changes in water quantity and quality, are increasingly …
Landslides after wildfire: Initiation, magnitude, and mobility
In the semiarid Southwestern USA, wildfires are commonly followed by runoff-generated
debris flows because wildfires remove vegetation and ground cover, which reduces soil …
debris flows because wildfires remove vegetation and ground cover, which reduces soil …
Postwildfire soil‐hydraulic recovery and the persistence of debris flow hazards
Deadly and destructive debris flows often follow wildfire, but understanding of changes in
the hazard potential with time since fire is poor. We develop a simulation‐based framework …
the hazard potential with time since fire is poor. We develop a simulation‐based framework …
Shallow landslides and vegetation at the catchment scale: A perspective
Shallow, rainfall-triggered landslides are an important catchment process that affect the rate
and calibre of sediment within river networks and create a significant hazard, particularly …
and calibre of sediment within river networks and create a significant hazard, particularly …
Forecasting the frequency and magnitude of postfire debris flows across southern California
Southern California has a long history of damaging debris flows after wildfire. Despite
recurrent loss, forecasts of the frequency and magnitude of postfire debris flows are not …
recurrent loss, forecasts of the frequency and magnitude of postfire debris flows are not …
Deriving Debris‐Flow Dynamics From Real‐Time Impact‐Force Measurements
Understanding the impact forces exerted by debris flows is limited by a lack of direct field
measurements and validated numerical models. In this study, we use real‐time impact‐force …
measurements and validated numerical models. In this study, we use real‐time impact‐force …
Hydrogeomorphic recovery and temporal changes in rainfall thresholds for debris flows following wildfire
Wildfire‐induced changes to soil and vegetation promote runoff‐generated debris flows in
steep watersheds. Postfire debris flows are most commonly observed in steep watersheds …
steep watersheds. Postfire debris flows are most commonly observed in steep watersheds …
Movement of sediment through a burned landscape: Sediment volume observations and model comparisons in the San Gabriel Mountains, California, USA
Post‐wildfire changes to hydrologic and geomorphic systems can lead to widespread
sediment redistribution. Understanding how sediment moves through a watershed is crucial …
sediment redistribution. Understanding how sediment moves through a watershed is crucial …
[HTML][HTML] The recurrence interval of post-fire debris-flow generating rainfall in the southwestern United States
Abstract In the southwestern United States, post-fire debris flows commonly initiate during
short bursts of intense rainfall. To date, the frequency of the rainfall rates has not been …
short bursts of intense rainfall. To date, the frequency of the rainfall rates has not been …