THE BYRAM-KEETCH DROUGHT INDEX (BKDI) and DROUGHT FACTOR (DF)
The Byram-Keetch Drought Index (BKDI) attempts to measure the amount of precipitation necessary to
return the soil to full field capacity. It is a closed system ranging from 0 to 203 units (0 - 800 imperial)
and represents a moisture regime from 0 to 203 millimetres (0 - 8 inches) of water through the soil layer.
At 203 millimetres (8in) of water, the KBDI assumes saturation. Zero is the point of no moisture
deficiency and 203 (800) is the maximum drought that is possible. At any point along the scale, the index
number indicates the amount of net rainfall that is required to reduce the index to zero, or saturation.
The inputs for KBDI are weather station latitude, mean annual precipitation, maximum dry bulb
temperature, and the last 24 hours of rainfall. Reduction in drought occurs only when rainfall exceeds
5mm (0.20 inch) (called net rainfall).
Drought Factor (DF): A key component of the FFDI is the modelling of the dryness of the fuel. This is
expressed by the Drought Factor (DF), which ranges from 0 to 10. If this is multiplied by 10 and called a
percent, it gives the percentage of fine fuel that would be removed by a fire under the current conditions.
The DF is based on recent rainfall and on the Byram-Keetch Drought Index (BKDI).