Skip Navigation WFAS - Wildland Fire Assessment System

 WFAS
   Overview
   News
   Support
   Processing
   Disclaimer
   References
   Quick Links
 Fire Potential & Danger
   Fire Danger Rating
   Lightning Ignition Efficiency
   Haines Index
 Weather
   Fire Weather
   Map Data
   30-Day Forecast
 Moisture & Drought
   Dead Fuel Moisture - NFDRS
   AVHRR NDVI Greenness
   Keetch-Byram Drought Index
   Palmer Drought Index
 Experimental Products
   Gridded NFDRS Forecast
  · Fire Potential Index
   Oklahoma Fire Danger
   Live Fuel Moisture
 Static Maps
   Fire Weather Station Location
   NFDRS Fuel Model Map
 Other
   Links


Forest Service Logo
Fire Potential Index Last updated: August 06, 2002

Experimental Product Maps

Current Conditions

Forecast

Image Archive

Data Archive

Fire Potential Index

  • FPI
  • FPI, RG, 10h, fire danger (4 panel)

 

US48
US48

 

US48

 

 

The experimental fire potential index map uses satellite derived Relative Greenness, an NFDR fuel model map (both 1 km resolution), and an interpolated 10-hour timelag map as inputs to weight the relative influence of live and dead vegetation to fire potential. The scale ranges from 0 (low) to 100 (high). Except for 10-h moisture content, the calculations used in the National Fire Danger Rating System are not part of the Fire Potential Index.

Experimental Fire Potential The fire potential index is described by Burgan and others (1998). This paper was modified in 2000 to include more recent work. The revised paper is available online. The major modification consists of a new maximum live ratio map for the U.S. In the original formulation of the FPI algorithm, maximum live ratios were determined as a function of the live and dead loads assigned to each fuel model. However, this resulted in similar live ratios for fuel models that represent very different vegetation types--not a realistic situation. The effect was to overestimate the FPI in the eastern U.S. during summer, when the vegetation is normally very green. This dilemma was resolved by deriving a maximum live ratio map from the maximum NDVI map of the conterminous United States, under the assumption of a direct relationship between the two. A second modification was made to smooth the ten hour fuel moisture calculation near its upper and lower limits, thus avoiding calculation discontinuities.

If you have questions contact:

Bob Burgan, Retired
Missoula Fire Sciences Lab
PO Box 8089
Missoula, MT 59807
Ph: 406-728-0172
e-mail: firebug@centric.net


top of page