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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 1 - 25 of 126
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
North, Stephens, Collins, Agee, Aplet, Franklin, Fulé
From the text ... 'Management reform in the United States has failed, not because of policy, but owing to lack of coordinated pressure sufficient to overcome entrenched agency disincentive to working with fire. Responding to established research, official agency policy now…
Year: 2015
Type: Document
Source: TTRS
North, Stephens, Collins, Agee, Aplet, Franklin, Fulé
Year: 2015
Type: Document
Source: TTRS
Liu, Hussaini, Okten
Rothermel's wildland surface fire spread model is widely used in North America. The model outputs depend on a number of input parameters, which can be broadly categorized as fuel model, fuel moisture, terrain, and wind parameters. Due to the inevitable presence of uncertainty in…
Year: 2015
Type: Document
Source: TTRS
Katurji, Nikolic, Zhong, Pratt, Yu, Heilman
We have demonstrated the use of an advanced Gaussian-Process (GP) emulator to estimate wildland fire emissions over a wide range of fuel and atmospheric conditions. The Fire Emission Production Simulator, or FEPS, is used to produce an initial set of emissions data that…
Year: 2015
Type: Document
Source: TTRS
Finney, Cohen, Forthofer, McAllister, Gollner, Gorham, Saito, Akafuah, Adam, English
Large wildfires of increasing frequency and severity threaten local populations and natural resources and contribute carbon emissions into the earth-climate system. Although wildfires have been researched and modeled for decades, no verifiable physical theory of spread is…
Year: 2015
Type: Document
Source: TTRS
Boer, Price, Bradstock
From the text...'Studies in Australia and the United States show that weather is a stronger determinant of fire severity than is fuel...Fuel treatment whether by managed fires or other means, may be most cost-effective when strategically targeted in close proximity to assets at…
Year: 2015
Type: Document
Source: TTRS
Appenzeller
From the text ... 'The trees of the boreal, after all, are used to fire. The dominant species in Alaska and much of Canada, black spruce, maintains an aerial storehouse of seeds, locked in cones that form a distinctive tuft at the treetop. When a fire singes the cones and melts…
Year: 2015
Type: Document
Source: TTRS
Wang, Thompson, Marshall, Tymstra, Carr, Flannigan
In Canadian forests, the majority of burned area occurs on a small number of days of extreme fire weather. These days lie within the tail end of the distribution of fire weather, and are often the periods when fire suppression capacity is most challenged. We examined the…
Year: 2015
Type: Document
Source: TTRS
Liu, Jimenez, Hussaini, Okten, Goodrick
Rothermel's wildland surface fire model is a popular model used in wildland fire management. The original model has a large number of parameters, making uncertainty quantification challenging. In this paper, we use variance-based global sensitivity analysis to reduce the number…
Year: 2015
Type: Document
Source: FRAMES, TTRS
Smurthwaite
From the text ... 'What does the future of rangelands and wildfire look like? The easy answer to the question is that rangelands will look different in the future and so will wildfire occurrence and behavior.'
Year: 2015
Type: Document
Source: TTRS
Lowell, Parrent, Deering, Bihn, Becker
The Community Biomass Handbook. Volume 2: Alaska, Where Woody Biomass Can Work, is a companion volume to the Community Biomass Handbook. Volume 1: Thermal Wood Energy, published in April 2014 (Becker et al. 2014). Why an Alaska volume? The original handbook contains information…
Year: 2015
Type: Document
Source: FRAMES
Based primarily on the Canadian Forest Fire Danger Rating System (CFFDRS) component parts, the Fire Weather Index (FWI) System and the Fire Behavior Prediction (FBP) System, this document can be used to guide learning users through the fire behavior assessment process from the…
Year: 2015
Type: Document
Source: FRAMES
This guide is intended as a reference for US users who may have reason to work with the system in the United States, where English units are primarily used. Keep in mind that the Canadian Forest Service has produced the definitive selection of reference publications and tools…
Year: 2015
Type: Document
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