Skip to main content

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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 40

Schroeder, Buck
[no description entered]
Year: 1970
Type: Document
Source: TTRS

Lee, Hellman
[no description entered]
Year: 1970
Type: Document
Source: TTRS

Balasubramanian, Victor, Chun
The results of chemical analyses of precipitation samples collected in Singapore between August 1997 and July 1998 are presented. Major inorganic and organic ions were determined in 169 rain samples collected using an automated wet-only sampler. The daily sample pH values ranged…
Year: 2001
Type: Document
Source: TTRS

Sorbel
The Kenai Lake Fire burned north of Kenai Lake on the Seward Ranger District of the Chugach National Forest from June 25 through July 8, 2001. The fire’s size was approximately 3260 acres. This assessment uses the FireFamily+ and RERAP (Rare Event Risk Assessment Process)…
Year: 2001
Type: Document
Source: FRAMES

Ferguson
From the Summary...'For many projects a simple model often provides as good information as a more complex model. Regulations, however, may dictate the level of modeling required for each project. Other times, community values will determine the level of effort needed to…
Year: 2001
Type: Document
Source: TTRS

Ferguson
From the Summary...'Managing smoke in ways that prevent serious impact to sensitive areas from single burns or multiple burns occurring simultaneously requires knowledge of the weather conditions that will affect smoke emissions, trajectories, and dispersion. Not only is it…
Year: 2001
Type: Document
Source: TTRS

McLin, Springer, Lane
[no description entered]
Year: 2001
Type: Document
Source: TTRS

Van Wagner
From the text: 'In 1959 Williams published a method of calculating the fire season severity rating, an integrated measure of fire weather over the whole season. Being based solely on the daily fire danger index (1956 type), it could be used as an objective yardstick for…
Year: 1970
Type: Document
Source: TTRS

Connaughton
From the text: 'We have established that fire in the Intermountain West is a well recognized and time honored natural orce as part of our dynamic evolution. We have had no trouble agreeing that fire preceded man and, until very recently at least, has been a far more potent force…
Year: 1970
Type: Document
Source: TTRS

Turner
The accumulated hours of bright sunshine provide a simple index of fire season severity for the southern coastal area of British Columbia. This index, based on the period May 1 to August 31, is highly correlated with the annual acreage burned over the Vancouver Forest District.…
Year: 1970
Type: Document
Source: TTRS

Hély, Flannigan, Bergeron, McRae
Spring and summer simulations were carried out using the Canadian Fire Behavior Prediction (FBP) and U.S. BEHAVE systems to study the role of vegetation and weather on fire behavior in the mixedwood boreal forest. Stands at Lake Duparquet (Quebec, Canada) were characterized as…
Year: 2001
Type: Document
Source: TTRS

Simard
Between 1931 and 1961 Canadian forest fire researchers gathered a vast quantity of data on weather, fuel moisture and test fire behavior. The original purpose of the data was primarily for the development of forest fire danger tables. The data was gathered at 11 field stations…
Year: 1970
Type: Document
Source: TTRS

Fosberg, Lancaster, Schroeder
Standard drying conditions in the laboratory have been related to the diurnal fluctuations of temperature and humidity to define a standard drying day for forest fuels. The mean equilibrium moisture content of a fuel on a standard drying day is slightly different from the…
Year: 1970
Type: Document
Source: TTRS

Byram, Martin
The fire whirlwind, an erratic and violent phenomenon associated with the behavior of intense fires, may generate velocities comparable to those reached in tornadoes. All the conditions essential to the formation of fire whirlwinds can be readily produced in the laboratory on a…
Year: 1970
Type: Document
Source: TTRS

Cargill
Fire perimeters can be quickly estimated using a 'rate of spread/elapsed time' table. This eliminates the need for plotting the fire acreage in order to determine the perimeter of the fire, and control force requirements based on fire perimeter can be determined quicker.
Year: 1970
Type: Document
Source: TTRS

Appleby
[no description entered]
Year: 1970
Type: Document
Source: TTRS

Papineau
Wintertime (November-March) surface air temperatures at 14 stations throughout the state of Alaska are correlated with the Southern Oscillation Index and the Pacific Decadal Oscillation index, for the years 1954-2000. On the seasonal and monthly timescales, the principal results…
Year: 2001
Type: Document
Source: FRAMES

Hess, Scott, Hufford, Fleming
Examining the relationship of El Niño to weather patterns in Alaska shows wide climate variances that depend on the teleconnection between the tropics and the northern latitudes. However, the weather patterns exhibited in Alaska during and just after moderate to strong El Niño…
Year: 2001
Type: Document
Source: FRAMES, TTRS

Conard, Hartzell, Hilbruner, Zimmerman
Attitudes and policies concerning wildland fire, fire use, and fire management have changed greatly since early European settlers arrived in North America. Active suppression of wildfires accelerated early in the 20th Century, and areas burned dropped dramatically. In recent…
Year: 2001
Type: Document
Source: FRAMES, TTRS

Jenkins, Clark, Coen
This chapter attempts to describe a fairly recent and major advance in the modeling of wildfires: the coupling of a cloud-resolving numerical prediction model with a simple fire-spread and wildfire behavior model, so that the atmosphere-fire is treated as a single, dynamical…
Year: 2001
Type: Document
Source: FRAMES

Schroeder, Buck
Weather is never static. It is always dynamic. Its interpretation is an art. The art of applying complex information about weather to the equally complex task of wildland fire control cannot be acquired easily especially not by the mere reading of a book. The environment is in…
Year: 1970
Type: Document
Source: FRAMES

Fernando, Smith, IV
An intriguing variety of vortex structures arise during buoyant convection, especially in the presence of background stratification and rotation. These vortices play an important role in environmental fluid motions, bearing upon small-scale turbulence to planetary-scale…
Year: 2001
Type: Document
Source: FRAMES

Schroeder, Buck
[Excerpt from text] The fire weather occurring on a particular day is a dominant factor in the fire potential for that day. Fire climate well may be thought of as the synthesis of daily fire weather over a long period of time, is a dominant factor in fire control planning.…
Year: 1970
Type: Document
Source: FRAMES, TTRS

Ferguson, Rorig
Lightning causes most wildfires in the western United States, and is a major cause of fire elsewhere in the U.S. Because most lightning occurs with significant precipitation, however, simple predictions of Lightning Activity Level (LAL) do not accurately determine fire ignition…
Year: 2001
Type: Document
Source: FRAMES

Dale, Joyce, McNulty, Neilson, Ayres, Flannigan, Hanson, Irland, Lugo, Peterson, Simberloff, Swanson, Stocks, Wotton
This article examines how eight disturbances influence forest structure, composition, and function, and how climate change may influence the severity, frequency, and magnitude of disturbances to forests. We focus on examples from the United States, although these influences…
Year: 2001
Type: Document
Source: FRAMES, TTRS