Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8258
AuthorsFavalli, M.* 
Tarquini, S.* 
Fornaciai, A.* 
Boschi, E.* 
TitleDispersion index of topographic surfaces
Issue Date1-Jun-2012
Series/Report no./153-154(2012)
DOI10.1016/j.geomorph.2012.02.022
URIhttp://hdl.handle.net/2122/8258
KeywordsDispersion index
DEM
Lava flow
Geomorphic parameter
Mount Etna
Subject Classification04. Solid Earth::04.04. Geology::04.04.03. Geomorphology 
AbstractThe dispersion index (dσ) of topography is introduced. This index is a geomorphic parameter which characterizes each point of topography with respect to the stability/instability of the steepest descent path (SDP) originating from it. The procedure for calculating dσ is based on the assessment of SDP variations as the initial topography is also varied within a given elevation Δh, while a length scale L defines the maximum extent of the SDP. As a result, dσ can be derived for different ranges Δh and different bandwidths L. Since at each point the gravitational force would direct a surface flow along the SDP, dσ appears to have a strong influence on the behavior of gravity-driven mass flows, influencing local topographic widening, spreading or channelization. Considering Mount Etna (Italy) as a test case, we present maps of dσ for Δh = 3 m and L = 1, 2, 4 and 8 km, demonstrating also the relationship between the range Δh = 3 m and Etnean lava flows. Focusing on the 2001 lava flow, we show that the presented maps of dσ, besides being a tool for viewing morphologies, have interesting applications for hazard assessment related to lava flows.
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