Abstract

Abstract. A new methodology for the estimation of smoke-injection height from wild-land fires is proposed and evaluated. It is demonstrated that the approaches developed for estimating the plume rise from stacks, such as the formulas of G. Briggs, can be formally written in terms characterising the wild-land fires: fire energy, size and temperature. However, these semi-empirical methods still perform quite poorly because the physical processes controlling the uplift of the wildfire plumes differ from those controlling the plume rise from stacks. The proposed new methodology considers wildfire plumes in a way similar to Convective Available Potential Energy (CAPE) computations. The new formulations are applied to a dataset collected within the MISR Plume Height Project for about 2000 fire plumes in North America and Siberia. The estimates of the new method are compared with remote-sensing observations of the plume top by the MISR instrument, with two versions of the Briggs' plume-rise formulas, with the 1-D plume-rise model BUOYANT, and with the prescribed plume-top position (the approach widely used in dispersion modelling). The new method has performed significantly better than all these approaches. For two-thirds of the cases, its predictions deviated from the MISR observations by less than 500 m, which is the uncertainty of the observations themselves. It is shown that the fraction of "good" predictions is much higher (>80%) for the plumes reaching the free troposphere.

Highlights

  • Biomass burning is one of the major contributors of trace gases and aerosols to the atmosphere, which significantly affects its chemical and physical properties

  • Using the database of the Multi-angle Imaging SpectroRadiometer (MISR) Plume Height Project, Sofiev et al (2009) showed that more than 80 % of the fires observed in 2007–2008 over the US injected their smoke within the atmospheric boundary layer (ABL)

  • MISR is onboard the satellite Terra together with one of the MODIS devices, which provides a perfect co-location in space and time between the active-fire observations by MODIS and the fire plume heights measurements by MISR

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Summary

Introduction

Biomass burning is one of the major contributors of trace gases and aerosols to the atmosphere, which significantly affects its chemical and physical properties. A specific problem of the fire plumes is that the characteristics of this type of source differ from the parameters considered by the existing plume-rise formulations and models All such approaches require the diameter of the buoyant plume at the stack top (considered to have circular cross-section), temperature and velocity of the outgoing gases, their density, etc. (Briggs, 1984; Freitas et al, 2007; Nikmo et al, 1999; Weil, 1988) These quantities are hard to define for wild-land fires, which have strongly non-circular shape (rather a bow- or kidney-shape), wide overheated surface area with strongly-varying temperature in different parts of the burning area, no stack or definite release height, and strongly-varying initial velocity of fumes in different parts of the fire.

Existing plume-rise formulations
Input data for plume-rise computations
Methodology for injection height estimation adapted to wild-land fires
Adaptation of B69 and B84 for wild-land fires
Inter-comparison results
Prediction of free-troposphere plumes
Findings
Conclusions
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