Fire-induced geomorphic changes, such as enhanced erosion and debris-flow activity, are
expected to increase with climate change owing to increases in fire activity and rainfall …

Moody et al., 2013). Wildfire can also impart physical changes to soil structure (Badía and
Martí, 2003; Nyman et al., 2013), increasing its susceptibility to downslope movement. Fine …

Coupled simulations of surface and variably saturated subsurface flow, termed integrated
hydrologic models (IHMs), can provide powerful insights into the complex dynamics of …

The rates at which sediment from the landscape is recruited to channel networks reflect
lateral geomorphic connectivity and have significant implications for biophysical river …

High-elevation mountain streams are commonly viewed as erosive environments, but they
can retain sediment along river corridors for thousands of years. In 2013, an extreme flood …

Wildfires can dramatically increase erosion rates over time scales on the order of several
years, yet few data firmly constrain the relative importance of post‐wildfire erosion in the …

After wildfire, hillslope and channel erosion produce large amounts of sediment and can
contribute significantly to long‐term erosion rates. However, pre‐erosion high‐resolution …

Abstract Between 2003 and 2013, drought, large wildfires, and record-breaking rainfall
contributed to debris flows in southeast Australia that appear to be unprecedented in spatial …

We used field-based case studies to examine how spatial heterogeneity influences the
response of river corridors to changes in water and sediment fluxes after wildfire. Spatial …

Lahar activity is one of the most important processes capable of mobilizing large volumes of
sediment and producing devastating effects on human populations and infrastructure …