Elucidating the role of vegetation in the initiation of rainfall‐induced shallow landslides: Insights from an extreme rainfall event in the Colorado Front Range. Issue 17 (14th September 2016)

• Record Type: Journal Article
• Authors: McGuire, Luke A.; Rengers, Francis K.; Kean, Jason W.; Coe, Jeffrey A.; Mirus, Benjamin B.; Baum, Rex L.; Godt, Jonathan W.
• Is Part Of: Geophysical research letters. Volume 43:Issue 17(2016)
• Page Start: 9084
• Page End: 9092
• Publication Date: 2016-09-14
• Subjects: debris flow -- vegetation -- landslide -- rainfall -- Front Range -- slope aspect; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2016GL070741
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: More than 1100 debris flows were mobilized from shallow landslides during a rainstorm from 9 to 13 September 2013 in the Colorado Front Range, with the vast majority initiating on sparsely vegetated, south facing terrain. To investigate the physical processes responsible for the observed aspect control, we made measurements of soil properties on a densely forested north facing hillslope and a grassland‐dominated south facing hillslope in the Colorado Front Range and performed numerical modeling of transient changes in soil pore water pressure throughout the rainstorm. Using the numerical model, we quantitatively assessed interactions among vegetation, rainfall interception, subsurface hydrology, and slope stability. Results suggest that apparent cohesion supplied by roots was responsible for the observed connection between debris flow initiation and slope aspect. Results suggest that future climate‐driven modifications to forest structure could substantially influence landslide hazards throughout the Front Range and similar water‐limited environments where vegetation communities may be more susceptible to small variations in climate. Key Points: Vegetation exerted a first‐order control on landslide initiation location during an extreme rainfall event Landslide initiation was controlled by variations in apparent cohesion due to roots rather than interception or bedrock permeability Climate change could substantially influence landslide hazards throughout semiarid portions of the southwestern U.S.