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dc.contributor.authorFuller, Jonathan
dc.date.accessioned2018-09-29T00:30:31Z
dc.date.available2018-09-29T00:30:31Z
dc.date.issued2012-01-13
dc.identifier.citationFuller, Jonathan, 2012, Theoretical and Practical Deficiencies in the FEMA FAN Methodology: Arizona Geological Survey Contributed Report CR-12-B, 30 p.
dc.identifier.urihttp://hdl.handle.net/10150/629407
dc.descriptionThe FAN model, developed by the Federal Emergency Management Agency (FEMA, 1990) was one of the earliest attempts to generate a mathematical model of alluvial fan flooding that incorporated the impact of channel avulsions on flood risk. The FAN model implements a methodology for delineating alluvial fan flooding hazards first proposed by Dawdy (1979), and later modified by FEMA based on recommendations made by DMA (1985).2 The FEMA FAN methodology has been criticized in the literature (McGinn, 1979; Burkham, 1988; French, 1987, 1992; Fuller, 1990; NRC, 1996) since its inception, but remains a key component of FEMA’s floodplain delineation guidelines for alluvial fans (2003). Reaction to the FEMA methodology by floodplain managers has been mixed.
dc.language.isoen
dc.relation.ispartofseriesCR-12-B
dc.relation.urlhttps://library.azgs.arizona.edu/
dc.rightsArizona Geological Survey. All rights reserved.
dc.subjectArizona Geological Survey Contributed Reports
dc.subjectRecent
dc.subjectBasin and Range Province
dc.subjectflood model
dc.subject100-year flood zone
dc.subjectfloodplain
dc.subjectalluvial fan
dc.subjectFEMA
dc.subjectflood
dc.titleTheoretical and Practical Deficiencies in the FEMA FAN Methodology
csdgm.bounding.west-114.807
csdgm.bounding.east-109.05
csdgm.bounding.north34.196
csdgm.bounding.south31.3326
dc.description.collectioninformationDocuments in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
refterms.dateFOA2018-09-29T00:30:31Z


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