1988
DOI: 10.2737/se-rp-273
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1988 Revisions to the 1978 National Fire-Danger Rating System

Abstract: National Fire-Danger Rating System does not work well in the humid environment of the Eastern United States. System modifications to correct problems and their operational impact on System users are described. A new set of 20 fuel models is defined and compared graphically with the 1978 fuel models. Technical documentation of System changes is provided.

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Cited by 133 publications
(86 citation statements)
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“…Since then there have been some minor adjustments (Burgan 1988 and an Energy Release Component (ERC). These two components are combined to produce the Burning Index, based on a suite of physics-based nonlinear dynamic equations.…”
Section: Datamentioning
confidence: 99%
“…Since then there have been some minor adjustments (Burgan 1988 and an Energy Release Component (ERC). These two components are combined to produce the Burning Index, based on a suite of physics-based nonlinear dynamic equations.…”
Section: Datamentioning
confidence: 99%
“…Studies of the interaction between fire-weather conditions and wildfire activity have focused on modeling short timescale meteorologic and wildfire behavior variability (Fujioka, 1997;Andrews and Queen, 2001). Modeling efforts have helped quantify the role of weather variability relative to fuel conditions and amounts and local topography (Deeming et al, 1977;Burgan, 1988;Pyne et al, 1996). The development of fire danger rating systems has allowed for the integration of longer-term (seasonal) climatic variability and shortterm meteorological variability into decision support tools for fire management.…”
Section: Introductionmentioning
confidence: 99%
“…Long-term weather determines the moisture content and combustibility of deeper organic layers and dead logs. The moisture content of these fuels is reflected by the NFDRS 1,000-hour time-lag fuel moisture (Deeming and others 1977), Canadian Duff Moisture Code and Drought Code (Hirsch 1996;Stocks and others 1989;Van Wagner 1987Wotton and others 2009), Keetch-Byram Drought Index (Burgan 1988(Burgan , 1993Fujioka and others 2008), or Palmer Drought Index. Wind is perhaps the single most important cause of spatial and temporal variation within boreal forests.…”
Section: Fire Behavior and Effects: Concepts And Models _____________mentioning
confidence: 99%