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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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.

Displaying 14801 - 14825 of 14919

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

Jones, Booth, Yu, Ferry
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

Manies, Harden, Ottmar
This report describes the sample collection and processing for U.S. Geological Survey efforts at FROSTFIRE, an experimental burn that occurred in Alaska in 1999. Data regarding carbon, water, and energy dynamics pre-fire, during, and post-fire were obtained in this landscape-…
Year: 2011
Type: Document
Source: FRAMES

Yi, McGuire, Kasischke, Harden, Manies, Mack, Turetsky
Ecosystem models have not comprehensively considered how interactions among fire disturbance, soil environmental conditions, and biogeochemical processes affect ecosystem dynamics in boreal forest ecosystems. In this study, we implemented a dynamic organic soil structure in the…
Year: 2010
Type: Document
Source: FRAMES, TTRS

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

Nelson
Eighteen experimental fires were used to compare measured and calculated values for emission factors and fuel consumption to evaluate the carbon balance technique. The technique is based on a model for the emission factor of carbon dioxide, corrected for the production of other…
Year: 1982
Type: Document
Source: FRAMES, TTRS

McMahon
Forest fires can be divided into two broad classes-wildfires and prescribed fires. Wildfires, whether caused by nature (lightning, etc.) or by the accidental or malicious acts of man, are not planned by forest managers and do not occur under controlled conditions. They can be…
Year: 1983
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

Rocha, Shaver
Burned landscapes present several challenges to quantifying landscape carbon balance. Fire scars are composed of a mosaic of patches that differ in burn severity, which may influence postfire carbon budgets through damage to vegetation and carbon stocks. We deployed three eddy…
Year: 2011
Type: Document
Source: FRAMES, TTRS

Bond, Scott
We suggest that the spread of angiosperms in the Cretaceous was facilitated by novel fire regimes. Angiosperms were capable of high productivity and therefore accumulated flammable biomass ('fuel') more rapidly than their predecessors. They were capable of rapid reproduction,…
Year: 2010
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

de Groot, Pritchard, Lynham
In many forest types, over half of the total stand biomass is located in the forest floor. Carbon emissions during wildland fire are directly related to biomass (fuel) consumption. Consumption of forest floor fuel varies widely and is the greatest source of uncertainty in…
Year: 2009
Type: Document
Source: FRAMES, TTRS

Smith, Wooster
The classification of savanna fires into headfire and backfire types can in theory help in assessing pollutant emissions to the atmosphere via relative apportionment of the amounts of smouldering and flaming combustion occurring, and is also important when assessing a fire's…
Year: 2005
Type: Document
Source: FRAMES

Boby, Schuur, Mack, Verbyla, Johnstone
The boreal region stores a large proportion of the world's terrestrial carbon (C) and is subject to high-intensity, stand-replacing wildfires that release C and nitrogen (N) stored in biomass and soils through combustion. While severity and extent of fires drives overall…
Year: 2010
Type: Document
Source: FRAMES

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

Countryman
Carbon monoxide (CO) is a highly toxic, nonirritating gas. One of the products of combustion, it is invisible, odorless, tasteless, and slightly lighter than air. But smoke, another combustion product, is visible. And when smoke is present, it is highly likely that CO and other…
Year: 1971
Type: Document
Source: FRAMES, TTRS

Blackard, Finco, Helmer, Holden, Hoppus, Jacobs, Lister, Moisen, Nelson, Riemann, Ruefenacht, Salajanu, Weyermann, Winterberger, Brandeis, Czaplewski, McRoberts, Patterson, Tycio
Annotation: This paper presents a spatially explicit dataset of aboveground live forest biomass made from ground measured inventory plots for the conterminous U.S., Alaska and Puerto Rico. The plot data are from the USDA Forest Service Forest Inventory and Analysis (FIA) program…
Year: 2008
Type: Document
Source: FRAMES

Boerner, Huang, Hart
The Fire and Fire Surrogates (FFS) network is composed of 12 forest sites that span the continental United States, all of which historically had frequent low-severity fire. The goal of the FFS study was to assess the efficacy of three management treatments (prescribed fire,…
Year: 2008
Type: Document
Source: FRAMES

The Fire and Fuels Extension (FFE) to the Forest Vegetation Simulator (FVS) simulates fuel dynamics and potential fire behavior over time, in the context of stand development and management. Existing models of fire behavior and fire effects were added to FVS to form the FFE…
Year: 2010
Type: Document
Source: FRAMES