2014
DOI: 10.1016/j.geomorph.2014.02.015
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Characterizing the primary material sources and dominant erosional processes for post-fire debris-flow initiation in a headwater basin using multi-temporal terrestrial laser scanning data

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Cited by 91 publications
(154 citation statements)
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References 67 publications
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“…Indeed, the suspended sediment flux from the Arroyo Seco subbasin was found by Warrick et al (2012) to be highly controlled by the coincidence of wildfire and large storms on the basis of two instances of nearly complete burning of the watershed's oak and chaparral shrublands. The role of fire in maintaining chaparral vegetation communities and dominating sediment production in the semi-arid foothills and low mountains typical of coastal central and southern California has been extensively reported (Hanes, 1971;Rice, 1982;Minnich, 1983;Florsheim et al, 1991;Mensing;Keeley and Fotheringham, 2003;Mortiz, 2003;Wohlgemuth and Hubbert, 2008;Zeedler, 2009, Hubbert et al, 2012;Staley et al, 2014). In contrast, the undammed Salinas River watershed is an order of magnitude larger than the Arroyo Seco, with about half the average relief, and extensive agricultural development consisting of irrigation agriculture in lowlands and extensive grasslands on lower foothill slopes.…”
Section: Discussionmentioning
confidence: 99%
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“…Indeed, the suspended sediment flux from the Arroyo Seco subbasin was found by Warrick et al (2012) to be highly controlled by the coincidence of wildfire and large storms on the basis of two instances of nearly complete burning of the watershed's oak and chaparral shrublands. The role of fire in maintaining chaparral vegetation communities and dominating sediment production in the semi-arid foothills and low mountains typical of coastal central and southern California has been extensively reported (Hanes, 1971;Rice, 1982;Minnich, 1983;Florsheim et al, 1991;Mensing;Keeley and Fotheringham, 2003;Mortiz, 2003;Wohlgemuth and Hubbert, 2008;Zeedler, 2009, Hubbert et al, 2012;Staley et al, 2014). In contrast, the undammed Salinas River watershed is an order of magnitude larger than the Arroyo Seco, with about half the average relief, and extensive agricultural development consisting of irrigation agriculture in lowlands and extensive grasslands on lower foothill slopes.…”
Section: Discussionmentioning
confidence: 99%
“…Increased surface runoff further exacerbates erosion from the destabilized hillslope. Indeed, the timing of high-intensity precipitation plays a large role in post-fire sediment flux augmentation (Inbar et al, 1998;Warrick et al, 2012;Staley et al;. Large storms produce precipitation intensities and volumes sufficient to traverse runoff regimes, from sheet flow, to rill and gully erosion, and mass wasting, which can very effectively erode wildfire destabilized hillslopes (Cannon, 2001;Moody et al, 2008).…”
Section: Internal and External Controlsmentioning
confidence: 99%
“…CANNON et al, 1998, 2001a, 2001b, São Paulo, v.18, n.1, (Jan-Mar) p. 81-106, 2017, 2011GARTNER et al, 2008;SANTI et al, 2008;PARISE e CANNON, 2012;STALEY et al, 2013STALEY et al, , 2014DE GRAFF, 2014;NYMAN et al, 2015). Por este motivo, e tendo em conta os incêndios fl orestais que defl agraram na área de estudo dois meses antes do desencadeamento dos fl uxos de detritos, considerou-se importante a integração da variável respeitante às áreas ardidas no verão de 2005.…”
Section: Modelação Das áReas De Rutura De Fl Uxos De Detritos Seleçãounclassified
“…Generally, lidar information complements rather than replaces field observations, with lidar observations leading to new hypotheses and process cognition (Roering et al, 2013). Broadly, lidar technology has been useful in studying geomorphic response to extreme events such as fire and storms (e.g., Pelletier and Orem, 2014;Sankey et al, 2013;Perignon et al, 2013;Staley et al, 2014), human activities (e.g., James et al, 2009), and past climatic and tectonic forcings (e.g., Roering, 2008;Belmont et al, 2011;West et al, 2014). Meter-and sub-meter-scale time-varying processes, often derived from TLS, have been quantified in the response of point bar and bank morphodynamics (Lotsari et al, 2014) and in the formation of micro-topography due to feedbacks with biota (e.g., Roering et al, 2010;Harman et al, 2014).…”
Section: Advances In Geomorphology Using Lidarmentioning
confidence: 99%