Methods are presented to relate temperature-residence-time at the soil
surface, i.e., time above 150 degrees C as an estimation of the sever
ity of a fire,, with measurements made during an experimental fire or
on two past hoc measurements. The experiment was carried out in a shru
bland dominated by the woody-legume Cytisus striatus subsp. eriocarpus
, in Central Spain. Temperature-sensitive paints, and steam-releasing
open-calorimeters were used as fire-meters during the burn. Post hoc m
easurements used were estimations of heat output per unit area, and me
asurements of the minimum diameter of branches of Cytisus remaining af
ter the fire. Time above 150 degrees C was obtained from measurements
made with thermocouples placed at the soil surface in 20 contiguous 1
x 1 m squares of the burn plot. All other measurements were made at ea
ch 1 x 1 m in the 22 x 3 m rectangle surrounding, and including, the t
hermocouple squares. Various simple and multiple regression models wer
e constructed to predict time above 150 degrees C from each of the fou
r measurements made during or after the fire. Maximum coefficients of
determination obtained for regressions were 0.61 and 0.62 for water ma
ss loss from open-calorimeters and branch diameter, respectively. Usin
g all the variables in a multiple regression model, time above 150 deg
rees C was related to water mass loss from open-calorimeters and heat
output per unit area with a coefficient of determination of 0.77. It i
s concluded that estimations of time above 150 degrees C at the soil s
urface during the passage of fire may be possible based on simple devi
ces, such as open-calorimeters, or on biological indicators, such as m
inimum branch diameters. Additionally, combining two methods (open-cal
orimeters, estimations of heat output per unit area) may allow the rec
onstruction of the time above 150 degrees C during the fire at a scale
of 1 m(2), an important characteristic of a burn to understand ecosys
tem response to fire.