2009
DOI: 10.1007/s10980-009-9443-8
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Effects of weather, fuel and terrain on fire severity in topographically diverse landscapes of south-eastern Australia

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Cited by 255 publications
(251 citation statements)
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“…The classification had at least 88% accuracy (Chafer et al 2004), with independent verification finding high levels of agreement (Hammill and Bradstock 2006). Bradstock et al (2010) subsequently utilised this severity mapping to examine the relative influence that weather, time since fire, topographic position, slope and aspect had on patterns of fire severity for the Mount Hall and Nattai fires, which occur at the low end of the precipitation gradient (Fig. 1).…”
Section: -1000mentioning
confidence: 99%
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“…The classification had at least 88% accuracy (Chafer et al 2004), with independent verification finding high levels of agreement (Hammill and Bradstock 2006). Bradstock et al (2010) subsequently utilised this severity mapping to examine the relative influence that weather, time since fire, topographic position, slope and aspect had on patterns of fire severity for the Mount Hall and Nattai fires, which occur at the low end of the precipitation gradient (Fig. 1).…”
Section: -1000mentioning
confidence: 99%
“…Six severity classes were mapped: (1) foliage and stems ,10 mm in the shrub and tree canopy layer consumed, (2) shrub foliage consumed and tree canopy partially scorched or consumed, (3) understorey shrub fire with complete tree canopy scorch, (4) understorey shrub fire with partial tree canopy scorch, (5) understorey shrub fire with no tree canopy scorch and (6) unburnt. Binary reclassification was undertaken as per Bradstock et al (2010) to permit two separate analyses focusing on (i) understorey fire (1: classes 3, 4, 5, 6; 0: classes 1, 2) and (ii) crown fire (1: class 1; 0: classes 2, 3, 4, 5, 6). Understorey fires (UF) are confined to the shrub and ground layers, with unburnt patches sometimes present.…”
Section: -1000mentioning
confidence: 99%
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