Estimating combustion of large downed woody debris from residual white ash

The production of residual white ash patches within wildfires represents near-complete combustion of the available fuel and releases a considerable quantity of gases to the atmosphere. These patches are generally produced from combustion of large downed woody debris (LDWD) such as fallen trees and snags. However, LDWD are generally ignored in calculations of fuel combusted within environments where surface fires dominate (e.g. southern African savannas). To assess the potential of fractional white ash cover as a remotely sensed measure of LDWD combustion, both the proportion of the surface covered by white ash and the combustion completeness required to produce white ash must be quantified. An aerial photograph of woodland savanna fires in north-western Zimbabwe was analysed to estimate the proportion of white ash cover within a typical satellite sensor pixel. The proportion loss on ignition (LOI) of wood samples from the study area was measured and combined with previous estimates of mean tree biomass. The proportion of white ash within the aerial photographs was 0.2% (± 0.06), which corresponded to an additional 67 320 kg ha −1 of biomass combusted above that typically recorded as combusted from a surface fire in this environment (∼7000 kg ha −1 ). This analysis should be repeated in other savannas and forests, where pre-fire fuel loads and post-fire fractional white ash cover may be higher.

[1]  D. Ward,et al.  Fuel biomass and combustion factors associated with fires in savanna ecosystems of South Africa and Zambia , 1996 .

[2]  C. Justice,et al.  SAFARI-2000 characterization of fuels, fire behavior, combustion completeness, and emissions from experimental burns in infertile grass savannas in western Zambia , 2003 .

[3]  A. Hudak,et al.  The relationship of field burn severity measures to satellite-derived Burned Area Reflectance Classification (BARC) maps , 2004 .

[4]  S. McNaughton,et al.  Grassland fire dynamics in the serengeti ecosystem, and a potential method of retrospectively estimating fire energy , 1989 .

[5]  Carol A. Wessman,et al.  DETECTING FIRE AND GRAZING PATTERNS IN TALLGRASS PRAIRIE USING SPECTRAL MIXTURE ANALYSIS , 1997 .

[6]  Andrew T. Hudak,et al.  Mapping fire scars in a southern African savannah using Landsat imagery , 2004 .

[7]  A. Lugo,et al.  The Quantity and Turnover of Dead Wood in Permanent Forest Plots in Six Life Zones of Venezuela 1 , 1998 .

[8]  N. Drake,et al.  FIRE IN AFRICAN SAVANNA: TESTING THE IMPACT OF INCOMPLETE COMBUSTION ON PYROGENIC EMISSIONS ESTIMATES , 2005 .

[9]  N. Zambatis,et al.  SAFARI‐92 characterization of biomass and fire behavior in the small experimental burns in the Kruger National Park , 1996 .

[10]  Jennifer Robinson,et al.  Fire from space : global fire evaluation using infrared remote sensing , 1991 .

[11]  T. Landmann,et al.  Characterizing sub-pixel Landsat ETM+ fire severity on experimental fires in the Kruger National Park, South Africa. , 2003 .

[12]  J. Settle,et al.  Mapping Vegetation, Soils, and Geology in Semiarid Shrublands Using Spectral Matching and Mixture Modeling of SWIR AVIRIS Imagery , 1999 .

[13]  T. Tietema,et al.  Biomass determination of fuelwood trees and bushes of Botswana, Southern Africa , 1993 .

[14]  José M. C. Pereira,et al.  A comparative evaluation of NOAA/AVHRR vegetation indexes for burned surface detection and mapping , 1999, IEEE Trans. Geosci. Remote. Sens..

[15]  David P. Turner,et al.  A Carbon Budget for Forests of the Conterminous United States , 1995 .

[16]  Sandra A. Brown Measuring carbon in forests: current status and future challenges. , 2002, Environmental pollution.

[17]  Martin J. Wooster,et al.  Texture based feature extraction: Application to burn scar detection in Earth observation satellite sensor imagery , 2002 .

[18]  R. Keane,et al.  Mapping wildland fuels for fire management across multiple scales: Integrating remote sensing, GIS, and biophysical modeling , 2001 .

[19]  E. Kasischke,et al.  Emissions of carbon dioxide, carbon monoxide, and methane from boreal forest fires in 1998 , 2002 .

[20]  G. Perry,et al.  Monthly burned area and forest fire carbon emission estimates for the Russian Federation from SPOT VGT , 2003 .

[21]  Yan Liu,et al.  Coarse woody debris in an old-growth deciduous forest on the Cumberland Plateau, southeastern Kentucky , 1991 .

[22]  Barbara L. Marks,et al.  Effects of silvicultural practices on carbon stores in Douglas-fir western hemlock forests in the Pacific Northwest, U.S.A.: results from a simulation model , 2002 .