Charring temperatures are driven by the fuel types burned in a peatland wildfire
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The influence of leaf morphology on litter flammability and its utility for interpreting palaeofire.Charcoal reflectance reveals early holocene boreal deciduous forests burned at high intensities.Interpreting palaeofire evidence from fluvial sediments: a case study from Santa Rosa Island, California, with implications for the Younger Dryas Impact HypothesisFine-scale distribution of moisture in the surface of a degraded blanket bog and its effects on the potential spread of smouldering fire
P2860
Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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Charring temperatures are driven by the fuel types burned in a peatland wildfire
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P2860
P356
P1476
Charring temperatures are driven by the fuel types burned in a peatland wildfire
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P2093
Claire M Belcher
Victoria A Hudspith
P2860
P356
10.3389/FPLS.2014.00714
P407
P577
2014-01-01T00:00:00Z