Modeling and sensitivity analysis of fire emissions in southern Africa during SAFARI 2000

https://doi.org/10.1016/j.rse.2004.06.010Get rights and content

Abstract

This paper uses three recently generated southern African satellite burned area products for the month of September 2000 in a sensitivity study of regional biomass burning emissions for a number of trace gases and particulates. Differences in the extent and location of areas burned among products generated from Moderate Resolution Imaging Spectroradiometer (MODIS), Systeme Pour l'Observation de la Terre (SPOT-VEGETATION), and Along Track Scanning Radiometer (ATSR-2) data are significant and result in different emissions estimates for woodland and grassland land cover types. Due to the different emission profiles in woodlands and grasslands, favoring relatively more products of incomplete combustion in woodlands compared with products of complete combustion in grasslands in the late dry season, these changes are not proportional to the differences in the burned area amounts. The importance of accurate burned area information not just in terms of the total area but also in terms of its spatial distribution becomes apparent from our modeling results. This paper highlights the urgent need for satellite data producers to provide accuracy assessments associated with satellite-derived products. Preferably, these accuracy data will be spatially explicit, or defined in a way that can be applied in a spatially explicit modeling context, to enable emissions uncertainties to be defined with respect to different landscape units in support of greenhouse gas emissions reporting.

Introduction

Reliable burned area information is required by a number of users, including global change scientists modeling the source strength, transport, fate, and impacts of trace gas and aerosol emissions from vegetation fires. National governments are required to report their greenhouse gas emissions. Natural resources managers and policy makers can benefit from a synoptic view of fire activity. The savannas of Africa are thought to experience the most extensive biomass burning in the world, for example, contributing an estimated 49% of the carbon lost from fires worldwide Scholes & Andreae, 2000, Dwyer et al., 2000, Van der Werf et al., 2003. Savanna fires in southern Africa play an important role in the regional atmospheric distribution of trace gases and aerosols, ecosystem functioning, and biogeochemical cycling Frost & Robertson, 1987, Scholes et al., 1996.

The Southern African Regional Science Initiative (SAFARI 2000) was an international scientific campaign aimed to study land–atmosphere interactions in southern Africa (Swap et al., 2003). One of the main objectives of SAFARI 2000 was the characterization and quantification of regional emissions sources, including those from savanna burning. Within this context, we have developed a spatially explicit emissions model, which we apply here to estimate the pyrogenic emissions for a number of trace gases and particulates during the dry season field campaign in September 2000. In this paper, we perform a sensitivity analysis to examine the geospatial relationship between burned area and emissions. Three recently developed moderate-resolution satellite burned area products from the Moderate Resolution Imaging Spectroradiometer (MODIS), Systeme Pour l'Observation de la Terre (SPOT-VEGETATION), and Along Track Scanning Radiometer (ATSR-2) sensors provide the basis for generating and comparing new estimates of biomass burning emissions from woodland and grassland fires in southern Africa during September 2000. An emissions sensitivity analysis with respect to the woodland–grassland model parameterization is also performed.

Section snippets

Fire emissions modeling methodology

Estimates of pyrogenic gas emissions require information on burned area, fuel load (the amount of fuel per unit area), completeness of combustion (the proportion of the fuel consumed during the fire), and emission factors (characteristic of the amount of the specific atmospheric species produced during the burning). Emissions are computed using spatially explicit input data following the well-established Seiler and Crutzen (1980) model:Ex=i,jAi,jFi,jCCi,j(EFx)i,jwhere Ex=total pyrogenic

Intercomparison of MODIS, GBA-2000, and GLOBSCAR burned area products, southern Africa, September 2000

Table 1, Table 2 summarize the regional differences between the MODIS, GBA-2000, and GLOBSCAR burned area products for September 2000. The total southern African area considered is 9,269,225 km2. MODIS detects a regional September burned area amount of approximately 268,500 km2, GBA-2000 detects approximately 173,100 km2, and GLOBSCAR detects approximately 59,800 km2. The MODIS active fire product detects an approximate area of 126,400 km2, although as we noted above, this estimate is expected

Conclusions

This sensitivity study contributes to a better understanding of the relationship between the spatial distribution of burned areas and emissions. The model's predictions, regardless of the burned area product, are consistent with published field studies of emission patterns from woodland and grassland fires Hoffa et al., 1999, Ward et al., 1996. These published studies show that burning in woodlands favors emissions of products of incomplete combustion compared with grasslands. Changes in the

Acknowledgements

This study was carried out as part of SAFARI-2000. Funding in partial support of this research was provided by National Aeronautics and Space Administration (NASA) grants NAS-531365 and NAG-511251. Stefania Korontzi is also supported by the NASA's Earth System Graduate Research Fellowship. The anonymous reviewers are thanked for their helpful comments.

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