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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 626 - 634 of 634
Gorham
Boreal and subarctic peatlands comprise a carbon pool of 455 Pg that has accumulated during the postglacial period at an average net rate of 0.096 Pg/yr (1 Pg = 10'5 g). Using Clymo's (1984) model, the current rate is estimated at 0.076 Pg/yr. Longterm drainage of these…
Year: 1991
Type: Document
Source: TTRS
Etiegni, Campbell
Chemical and physical properties are important in the development of processes for the disposal and utilization of wood ash. Ash yield was seen to decrease by approximately 45% as the combustion temperature increased from 538 to 1093 degrees C. Potassium, sodium, zinc and…
Year: 1991
Type: Document
Source: TTRS
Lewandrowski, Kim, Aillery
Economic studies have demonstrated that agricultural landowners could mitigate significant quantities of greenhouse gas (GHG) emissions through afforestation. The associated carbon, however, must remain stored in soils or biomass for several decades to achieve substantial…
Year: 2014
Type: Document
Source: FRAMES, TTRS
Ueyama, Ichii, Iwata, Euskirchen, Zona, Rocha, Harazono, Iwama, Nakai, Oechel
Warming in northern high latitudes has changed the energy balance between terrestrial ecosystems and the atmosphere. This study evaluated changes in regional surface energy exchange in Alaska from 2000 to 2011 when substantial declines in spring snow cover due to spring warming…
Year: 2014
Type: Document
Source: FRAMES, TTRS
Girardin, Guo, De Jong, Kinnard, Bernier, Raulier
The 20th century was a pivotal period at high northern latitudes as it marked the onset of rapid climatic warming brought on by major anthropogenic changes in global atmospheric composition. In parallel, Arctic sea ice extent has been decreasing over the period of available…
Year: 2014
Type: Document
Source: FRAMES
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
Frandsen
Smoldering ground fires can raise mineral soil temperatures above 300°C for several hours with peak temperatures near 600°C. Such temperatures can result in the decomposition of organic material and kill important soil organisms. The heat evolved per unit organic mass was…
Year: 1991
Type: Document
Source: TTRS