How do sediment yields from post-wildfire debris-laden flows depend on terrain slope, soil burn severity class, and drainage basin area? Insights from airborne-LiDAR change detection

Author:

Pelletier Jon D.1,Orem Caitlin A.1

Affiliation:

1. Department of Geosciences; University of Arizona; Tucson AZ USA

Funder

National Science Foundation

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference33 articles.

1. A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests;Allen;Forest Ecology and Management,2010

2. Rainfall and climate variation over a sloping New Mexico plateau during the North American monsoon;Bowen;Journal of Climate,1996

3. Predicting the probability and volume of postwildfire debris flows in the intermountain western United States;Cannon;Geological Society of America Bulletin,2010

4. Condon KE 2013 Quantifying Catchment-Scale Particulate Organic Matter (POM) Loss Following Fire, Relative to Background POM Fluxes

5. Physical Geomorphology of Debris Flows

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