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Operating under the assumption that the synchronized germination response observed after fires represents a synchronized germination of cohorts from the seed bank, we examined populations that occurred over a 6 11 year interval at the same location (Fig. 2A,2B,2C) to determine if temporally-defined genetic structure occurred in the populations, but none were found.
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These fires represented a natural disturbance event that occurs at intervals of 100-300 years in this region [4].
This paper contrasts the physically deterministic travel/flow model of behaviour in fires, represented by prescriptive fire codes and performance-based fire engineering, with an occupant response model.
Middle dry season fires represent 86.21% of the total burned areas and 32.05% of fire occurrences, affecting larger amount of higher density tree surfaces than other burning periods.
While upholstered furniture, bedding, and mattress fires represent some of the most pressing causes of domestic fires and fire deaths, electrical fires answer for some 20% of all fires in homes and are a major cause of domestic fire losses.
Carbon emissions in savanna fires represent a much shorter-term C loss than forest fires, since the main fuel is dead herbaceous vegetation, representing just one or two years of growth [27, 41].
Fires represent a large and highly variable component of the US carbon budget.
These fires represented a natural disturbance event that occurs at intervals of 100-300 years in this region [ 4].
Carbon emissions in savanna fires represent a much shorter-term C loss than forest fires, since the main fuel is dead herbaceous vegetation, representing just one or two years of growth [ 27, 41].
While isotopic and tracer techniques could certainly aid in the reduction of uncertainty in regional C inverse modeling, fires represent a level of complexity in terrestrial C dynamics that deserve increased attention.
Fires represent a potentially large short-term release of carbon that is largely offset over longer time scales (decades) by the uptake of atmospheric carbon associated with forest regrowth.
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