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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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 1 - 25 of 160

De Grandpre, Gagnon
The changes observed in the composition and abundance of shrubs, herbs and mosses were investigated following fire in the southern boreal forest of the Abitibi region, Quebec. Ten plots of 100m2 were sampled at each of eight sites varying in age from 26 to 230 years after fire (…
Year: 1991
Type: Document
Source: TTRS

Anderson
[no description entered]
Year: 1991
Type: Document
Source: TTRS

Roads, Ueyoshi, Chen, Alpert, Fujioka
The forecast skill of the National Meteorological Center's medium range forecast (MRF) numerical forecasts of fire weather variables is assessed for the period June 1, 1988 to May 31, 1990. Near-surface virtual temperature, relative humidity, wind speed and a derived fire…
Year: 1991
Type: Document
Source: TTRS

From the text ... 'The Wildfire Act is supported by the Fire Suppression Funding Solutions Partner Caucus and has been deemed especially critical in the face of global climate change. The Forest Service states that as a result of a changing climate, forest conditions are more…
Year: 2014
Type: Document
Source: TTRS

Zhang, Kondragunta, Roy
The ratio of key elements such as nitrogen, phosphorus, and silica determines nutrient limitations that are important to regulating primary productivity and species composition in aquatic ecosystems. The flux of these nutrients in streams, as dissolved constituents or as…
Year: 2014
Type: Document
Source: TTRS

Wheeler
From the text lll 'Several types of firebreaks exist, and often more than one type of firebreak is used during a prescribed fire. Different types of firebreaks offer different levels of performance and permanence and have varying levels of installation costs. the firebreaks that…
Year: 2014
Type: Document
Source: TTRS

Stephens, Burrows, Buyantuyev, Gray, Keane, Kubian, Liu, Seijo, Shu, Tolhurst, van Wagtendonk
Mega-fires are often defined according to their size and intensity but are more accurately described by their socioeconomic impacts. Three factors -- climate change, fire exclusion, and antecedent disturbance, collectively referred to as the 'mega-fire triangle' -- likely…
Year: 2014
Type: Document
Source: TTRS

Oliveira, Lopes, Baliga, Almeida, Viegas
Mathematical models and numerical solution procedures for predicting the trajectory, oscillation, possible rotation, and mass and size time-evolution of cylindrical wind-driven firebrands are described and discussed. Two test problems and the results, used for validating the…
Year: 2014
Type: Document
Source: FRAMES, TTRS

Keane, Dillon, Drury, Innes, Morgan, Lutes, Prichard, Smith, Strand
From the introduction ... 'Announcing the release of new software packages for application in wildland fire science and management, two fields that are already fully saturated with computer technology, may seem a bit too much to many managers. However, there have been some…
Year: 2014
Type: Document
Source: TTRS

Harbour
From the text ... 'Wildfires can be caused by an accumulation of dead matter (leaves, twigs, and trees) that can create enough heat in some instances to spontaneously combust and ignite the surrounding area.'
Year: 2014
Type: Document
Source: TTRS

Cruz, Alexander
From the text ... 'Operational guides for predicting various aspects of wildland fire behavior, including crowning, are generally dependent on mathematical models that can take a variety of forms. The degree of accuracy in predictions of crown fire behavior is dependent on the…
Year: 2014
Type: Document
Source: TTRS

Zimmerman, Lasko, Kaufmann
Significant changes occurring in the wildland fire environment of the United States are generatinguncharacteristic shifts in the complexity, behavior, extent, and effects of wildfires. Increases in wildfire numbers, temporal and spatial scales, and ecological, social, and…
Year: 2014
Type: Document
Source: FRAMES

The following list of fire research topics and questions were generated by personnel from agencies and organizations within AWFCG during 2014 Fall Fire Review and through other solicitations. The topics were initially ranked by the AWFCG Fire Research, Development and…
Year: 2014
Type: Document
Source: FRAMES

Barnes, Ziel
What factors may influence new fires burning into or being slowed by previous fire scars? How long can we consider fire scars a fuel barrier? More and more area in Alaska seems to be burning in close succession, or "repeat burns."
Year: 2014
Type: Media
Source: FRAMES

Pyne, Ziel
Presented at 2014 Fall Alaska Fire Science Workshop.
Year: 2014
Type: Media
Source: FRAMES

Saperstein
The Funny River Fire (AK-KKS-403140) was ignited by humans on May 19, 2014, and burned almost 200,000 acres on the Kenai Peninsula, Alaska, by early June. Most of the fire was within the Kenai National Wildlife Refuge, but it threatened adjacent communities. Four recreational…
Year: 2014
Type: Media
Source: FRAMES

Ziel
A brief refresher of CFFDRS from the 3-day Summit, held October 28-30 in Fairbanks.
Year: 2014
Type: Media
Source: FRAMES

Ramsey, Higgins
The tables presented here contain forest fire statistics for the calendar year 1984, 1985, 1986, and 1987 as reported by all Canadian forest fire control agencies. The statistical data are presented separately for each province or other major jurisdiction, and for Canada as a…
Year: 1991
Type: Document
Source: TTRS

Kourtz, Todd
Lightning causes one third of the 9000 wildfires that occur in Canada. Annually, these lightning-caused fires account for 90% of the area burned and cost Canadians at least 150 million dollars in suppression costs and values destroyed. Unlike the fires caused by human negligence…
Year: 1991
Type: Document
Source: TTRS

Weber
This is a review of the essential ingredients needed to make a mathematical model of fire spread through a fuel bed. The physical problem is outlined in general terms. Previous models are classified as statistical, empirical, or physical in accordance with the methods used in…
Year: 1991
Type: Document
Source: TTRS

Brown, Reinhardt
Equations for predicting duff and large woody fuel (7.6+ cm) consumption are summarized. Dependent variables are duff depth reduction, percentage duff depth reduction, percentage mineral soil, large fuel diameter reduction, and percentage large fuel reduction. Opportunities to…
Year: 1991
Type: Document
Source: TTRS

Hungerford, Campbell
Predictions of soil heating for two models were compared with temperatures and moisture contents measured in laboratory experiments. Columns packed with soil of different water contents and bulk densities were placed under a radiant gas heater. Temperature and water content were…
Year: 1991
Type: Document
Source: TTRS

Viney, Hatton, Dawes
The moisture content of the litter is one of the most important environmental factors affecting the ignition and propogation of a forest fire. The concept of equilibrium moisture content has proven utility in making a meaningful connection between weather and litter moisture.…
Year: 1991
Type: Document
Source: TTRS

Todd, Kourtz
People are responsible for starting two out of every three forest fires in Canada. To efficiently suppress these fires while they are still small, a modern forest fire control organization must be able to predict their numbers and locations one day in advance. Contrary to…
Year: 1991
Type: Document
Source: TTRS

Latham
A prescribed fire was ignited near Chapleau, western Ontario, Canada, on the afternoon of August 10, 1989. The fire, covering approximately 400 ha, burned vigorously over a period of 3 hours, from 1400 to 1700 EDT, generating a plume cloud structure including a portion…
Year: 1991
Type: Document
Source: TTRS