Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3173
DC FieldValueLanguage
dc.contributor.authorallToyos, G.; Department of Geography, University of Cambridge, Cambridge, UKen
dc.contributor.authorallOramas Dorta, D.; Department of Geography, Coventry University, Coventry, UKen
dc.contributor.authorallOppenheimer, C.; Department of Geography, University of Cambridge, Cambridge, UKen
dc.contributor.authorallPareschi, M. T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallSulpizio, R.; Dipartimento Geomineralogico, Universita di Bari, Bari, Italyen
dc.contributor.authorallZanchetta, G.; Dipartimento di Scienze della Terra, Universita di Pisa, Pisa, Italyen
dc.date.accessioned2007-12-13T09:15:40Zen
dc.date.available2007-12-13T09:15:40Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/3173en
dc.description.abstractBased on the debris flow events that occurred in May 1998 in the area of Sarno, Southern Italy, this paper presents an approach to simulate debris flow maximum run-out. On the basis of the flow source areas and an average thickness of 1•2 m of the scarps, we estimated debris flow volumes of the order of 104 and 105 m3. Flow mobility ratios (ΔΗ/L) derived from the x, y, z coordinates of the lower-most limit of the source areas (i.e. apex of the alluvial fan) and the distal limit of the flows ranged between 0•27 and 0•09. We performed regression analyses that showed a good correlation between the estimated flow volumes and mobility ratios. This paper presents a methodology for predicting maximum run-out of future debris flow events, based on the developed empirical relationship. We implemented the equation that resulted from the calibration as a set of GIS macros written in Visual Basic for Applications (VBA) and running within ArcGIS. We carried out sensitivity analyses and observed that hazard mapping with this methodology should attempt to delineate hazard zones with a minimum horizontal resolution of 0•4 km. The developed procedure enables the rapid delineation of debris flow maximum extent within reasonable levels of uncertainty, it incorporates sensitivities and it facilitates hazard assessments via graphic user interfaces and with modest computing resources.en
dc.language.isoEnglishen
dc.publisher.nameJohn Wiley & Sons, Ltden
dc.relation.ispartofEarth Surface Processes and Landformsen
dc.relation.ispartofseries10/32 (2007)en
dc.subjectdebris flowsen
dc.subjectvolumeen
dc.subjectmobilityen
dc.subjectGISen
dc.subjecthazard assessmenten
dc.titleGIS-assisted modelling for debris flow hazard assessment based on the events of May 1998 in the area of Sarno, Southern Italy: Part I. Maximum run-outen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1491 - 1502en
dc.subject.INGV05. General::05.08. Risk::05.08.02. Hydrogeological risken
dc.identifier.doi10.1002/esp.1472en
dc.description.obiettivoSpecifico4.3. TTC - Scenari di pericolosità vulcanicaen
dc.description.obiettivoSpecifico5.4. TTC - Sistema Informativo Territorialeen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorToyos, G.en
dc.contributor.authorOramas Dorta, D.en
dc.contributor.authorOppenheimer, C.en
dc.contributor.authorPareschi, M. T.en
dc.contributor.authorSulpizio, R.en
dc.contributor.authorZanchetta, G.en
dc.contributor.departmentDepartment of Geography, University of Cambridge, Cambridge, UKen
dc.contributor.departmentDepartment of Geography, Coventry University, Coventry, UKen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentDipartimento Geomineralogico, Universita di Bari, Bari, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Universita di Pisa, Pisa, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Geography, University of Cambridge, Cambridge, England-
crisitem.author.deptDepartment of Geography, Coventry University, Coventry, UK-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptCIRISIVU, c/o Dipartimento Geomineralogico, Universita' di Bari-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0003-4506-7260-
crisitem.author.orcid0000-0002-3930-5421-
crisitem.author.orcid0000-0002-7080-9599-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
ESPL_Toyos et al_2007.pdf538.65 kBAdobe PDF
Show simple item record

WEB OF SCIENCETM
Citations 50

21
checked on Feb 10, 2021

Page view(s) 50

170
checked on Apr 20, 2024

Download(s)

21
checked on Apr 20, 2024

Google ScholarTM

Check

Altmetric