We are please to announce that the GCD and paleofire R packages have been updated to their 4.0.2 and 1.2.2 versions, respectively. GCD major update from 3.X.X to 4.X.X version…
We are happy to share the last GPWG2 paper published as a perspective in Fire. This perspective is a product of the last GPWG2 workshop held in Montréal October 2017. We…
Levels of biomass burning in parts of the world are now higher than at any time in the past 22,000 years, according to our most recent fire history reconstructions from the…
Highlights: • 18 southern European charcoal records document 16,000 years of fire regime changes. • Since the Neolithic, land uses have artificially maintained high fire frequencies. • Human-induced decreases in…
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By adminNovember 18, 2015Posted inAnalyses
Abstract. The location, timing, spatial extent, and frequency of wildfires are changing rapidly in many parts of the world, producing substantial impacts on ecosystems, people, and potentially climate. Paleofire records…
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By adminNovember 18, 2014Posted inAnalyses
Abstract: We describe a new R package, paleofire, for analysis and synthesis of charcoal time series, such as those contained in the Global Charcoal Database (GCD), that are used to reconstruct…
This chapter provides a global perspective on palaeofire activity through the analysis of over 650 stratigraphic sedimentary charcoal records spanning the last 21000 years. Regional time series analysis provides empirical…
A mid- to late-Holocene synthesis of fire activity from the Mediterranean basin explores the linkages among fire, climate variability and seasonality through several climatic and ecological transitions. Regional fire histories…
Climate is an important control on biomass burning, but the sensitivity of fire to changes in temperature and moisture balance has not been quantified. We analyze sedimentary charcoal records to…
Understanding the causes and consequences of wildfires in forests of the western United States requires integrated information about fire, climate changes, and human activity on multiple temporal scales. We use…