The Alaska Reference Database originated as the standalone Alaska Fire Effects Reference Database, a ProCite reference database maintained by former BLM-Alaska Fire Service Fire Ecologist Randi Jandt. It was expanded under a Joint Fire Science Program grant for the FIREHouse project (The Northwest and Alaska Fire Research Clearinghouse). It is now maintained by the Alaska Fire Science Consortium and FRAMES, and is hosted through the FRAMES Resource Catalog. The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.
Type
Topic
Year
Displaying 2526 - 2550 of 2574
Polley, Briske, Morgan, Wolter, Bailey, Brown
The amplified “greenhouse effect” associated with increasing concentrations of greenhouse gases has increased atmospheric temperature by 1°C since industrialization (around 1750), and it is anticipated to cause an additional 2°C increase by mid-century. Increased biospheric…
Year: 2013
Type: Document
Source: FRAMES, TTRS
Seedre, Taylor, Brassard, Chen, Jogiste
Corresponding with the increasing global resource demand, harvesting now affects millions of hectares of boreal forest each year, and yet our understanding of harvesting impacts on boreal carbon (C) dynamics relative to wildfire remains unclear. We provide a direct comparison of…
Year: 2014
Type: Document
Source: FRAMES
Oris, Asselin, Ali, Finsinger, Bergeron
Forest fires are an important disturbance in the boreal forest. They are influenced by climate, weather, topography, vegetation, surface deposits and human activities. In return, forest fires affect the climate through emission of gases and aerosols, and changes in surface…
Year: 2014
Type: Document
Source: FRAMES, TTRS
Natali, Schuur, Webb, Hicks Pries, Crummer
A large pool of organic carbon (C) has been accumulating in the Arctic for thousands of years because cold and waterlogged conditions have protected soil organic material from microbial decomposition. As the climate warms, this vast and frozen C pool is at risk of being thawed,…
Year: 2014
Type: Document
Source: FRAMES
Knapp, Briggs, Collins, Archer, Bret-Harte, Ewers, Peters, Young, Shaver, Pendall, Cleary
Shrub encroachment into grass-dominated biomes is occurring globally due to a variety of anthropogenic activities, but the consequences for carbon (C) inputs, storage and cycling remain unclear. We studied eight North American graminoid-dominated ecosystems invaded by shrubs,…
Year: 2008
Type: Document
Source: FRAMES
Fan, Neff, Harden, Zhang, Veldhuis, Czimczik, Winston, O'Donnell
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. However, the movement of liquid water, which plays an important role in the heat transport of temperate soils, has been under-represented in boreal studies. Two different heat…
Year: 2011
Type: Document
Source: FRAMES
A 2200-year record of permafrost dynamics and carbon cycling in a collapse-scar bog, Interior Alaska
Recent high-latitude warming is increasing the vulnerability of permafrost to thaw, which is amplified by local disturbances such as fire. However, the long-term ecological effects and carbon dynamics are not well understood. Here we present a 2200-year record of pollen, plant…
Year: 2013
Type: Document
Source: FRAMES, TTRS
Attiwill, Binkley
In many parts of the world both the area and intensity of wild-land fires have increased alarmingly. Not only are fires increasing in number, but the nature of these fires is also changing. We see mega-fires of increasing size and intensity in many parts of the world including…
Year: 2013
Type: Document
Source: FRAMES, TTRS
This report is a scientific assessment of the current condition and likely future condition of forest resources in the United States relative to climatic variability and change. It serves as the U.S. Forest Service forest sector technical report for the National Climate…
Year: 2013
Type: Document
Source: FRAMES
Dore, Montes-Helu, Hart, Hungate, Koch, Moon, Finkral, Kolb
Carbon uptake by forests is a major sink in the global carbon cycle, helping buffer the rising concentration of CO2 in the atmosphere, yet the potential for future carbon uptake by forests is uncertain. Climate warming and drought can reduce forest carbon uptake by reducing…
Year: 2012
Type: Document
Source: FRAMES
O'Donnell, Harden, McGuire, Romanovsky
In the boreal region, soil organic carbon (OC) dynamics are strongly governed by the interaction between wildfire and permafrost. Using a combination of field measurements, numerical modeling of soil thermal dynamics, and mass-balance modeling of OC dynamics, we tested the…
Year: 2011
Type: Document
Source: FRAMES, TTRS
Kolden, Abatzoglou
Boreal forest fires are an important source of terrestrial carbon emissions, particularly during years of widespread wildfires. Most carbon emission models parameterize wildfire impacts and carbon flux to area burned by fires, therein making the assumption that fires consume a…
Year: 2012
Type: Document
Source: FRAMES
Patterson, McMahon, Ward
Data on the optical absorption properties (expressed as a specific absorption, Ba) of the smoke emissions from fires with forest fuels have been determined for a series of low-intensity field fires and a series of laboratory scale fires. The Ba data have been used to estimate…
Year: 1986
Type: Document
Source: FRAMES, TTRS
Turetsky, Donahue, Benscoter
For millennia, peatlands have served as an important sink for atmospheric CO2 and today represent a large soil carbon reservoir. While recent land use and wildfires have reduced carbon sequestration in tropical peatlands, the influence of disturbance on boreal peatlands is…
Year: 2011
Type: Document
Source: FRAMES, TTRS
van Bellen, Garneau, Bergeron
The global boreal forests comprise large stocks of organic carbon that vary with climate and fire regimes. Global warming is likely to influence several aspects of fire and cause shifts in carbon sequestration patterns. Fire severity or forest floor depth of burn is one…
Year: 2010
Type: Document
Source: FRAMES
Bremond, Carcaillet, Favier, Ali, Paitre, Bégin, Bergeron, Richard
An original method is proposed for estimating past carbon emissions from fires in order to understand long-term changes in the biomass burning that, together with vegetation cover, act on the global carbon cycle and climate. The past carbon release resulting from paleo-fires…
Year: 2010
Type: Document
Source: FRAMES, TTRS
Flannigan, Krawchuk, de Groot, Wotton, Gowman
Wildland fire is a global phenomenon, and a result of interactions between climate-weather, fuels and people. Our climate is changing rapidly primarily through the release of greenhouse gases that may have profound and possibly unexpected impacts on global fire activity. The…
Year: 2009
Type: Document
Source: FRAMES
Bachelet, Neilson, Hickler, Drapek, Lenihan, Sykes, Smith, Sitch, Thonicke
Simulations of potential vegetation distribution, natural fire frequency, carbon pools, and fluxes are presented for two DGVMs (Dynamic Global Vegetation Models) from the second phase of the Vegetation/Ecosystem Modeling and Analysis Project. Results link vegetation dynamics to…
Year: 2003
Type: Document
Source: FRAMES
Lenihan, Bachelet, Neilson, Drapek
A modeling experiment was designed to investigate the impact of fire management, CO2 emission rate, and the growth response to CO2 on the response of ecosystems in the conterminous United States to climate scenarios produced by three different General Circulation Models (GCMs)…
Year: 2008
Type: Document
Source: FRAMES
Guggenheim
Description not entered.
Year: 1999
Type: Document
Source: FRAMES
Kurz, Apps, Comeau, Trofymow
The Carbon Budget Model of the Canadian Forest Sector (CBM-CFS2) is a national-scale model of forest sector carbon (C) pools and fluxes. This model has been applied to conduct a retrospective analysis of the C budget of the forests of British Columbia for the period 1920- 1989.…
Year: 1996
Type: Document
Source: FRAMES
Kurz, Apps, Webb, McNamee
An assessment of the contribution of Canadian forest ecosystems and forestry activities to the global carbon budget was undertaken. The first phase of this study consisted of the development of a computer modeling framework and the use of published information to establish the…
Year: 1992
Type: Document
Source: FRAMES
Zimov, Schuur, Chapin
Climate warming will thaw permafrost, releasing trapped carbon from this high-latitude reservoir and further exacerbating global warming.
Year: 2006
Type: Document
Source: FRAMES
Vogel, Valentine, Ruess
Climate warming at high latitudes is expected to increase root and microbial respiration and thus cause an increase in soil respiration. We measured the root and microbial components of soil respiration near Fairbanks, Alaska, in 2000 and 2001, in three black spruce (Picea…
Year: 2005
Type: Document
Source: FRAMES
Swanson
Some soils with permafrost thawed deeply and become drier after forest fires, while others changed little. Soils with permafrost on the coldest and wettest landscape positions (concave to plane, lower slope positions, and north-facing midslopes) usually failed to thaw deeply…
Year: 1996
Type: Document
Source: FRAMES