Fire-fuel-climate linkages in the northwestern USA during the Holocene
Submitted by shompa on Tue, 2006-12-26 12:57
Variations in fire regimes can be inferred from changes in the abundance of sedimentary charcoal found in lake and bog sediments. When analysed with pollen data, inferences can be made about past vegetation dynamics and climate as well. The analysis of high-resolution charcoal records generally
involves the decomposition of charcoal influx into (a) a slowly varying
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Publication Date:
26/12/2006