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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 35
Bond, van Wilgen
[no description entered]
Year: 1996
Type: Document
Source: TTRS
Gosz, Gosz
The desert/grassland biome transition zone in central New Mexico provides an important region for testing species differences to changing environmental conditions and various land management practices. Interactions of black grama (Bouteloua eripoda) and blue grama (Bouteloua…
Year: 1996
Type: Document
Source: TTRS
Vega-García, Lee, Woodard, Titus
Human-caused forest fires are a serious problem throughout the world. Believing that there are predictable characteristics common to all fires, we analyzed the historical human-caused fire occurrence data for the Whitecourt Provincial Forest of Alberta using artificial neural…
Year: 1996
Type: Document
Source: TTRS
Pojar
The western boreal forest of North America (Manitoba through Alaska) has a typical boreal climate, but the largely sedimentary Interior Plains and the northern Cordillera (part of which was ice-free in the Pleistocene) are physiographically and geologically very different from…
Year: 1996
Type: Document
Source: FRAMES
Hu, Brubaker, Anderson
Analyses of pollen, plant macrofossils, macroscopic charcoal, mollusks, magnetic susceptibility, and geochemical content of a sediment core from Farewell Lake yield a 11,000-yr record of terrestrial and aquatic ecosystem changes in the northwestern foothills of the Alaska Range…
Year: 1996
Type: Document
Source: FRAMES
Hansen, Ruedy, Sato, Reynolds
Global surface air temperature has increased about 0.5°C from the minimum of mid-1992, a year after the Mt. Pinatubo eruption. Both a land-based surface air temperature record and a land-marine temperature index place the meteorological year 1995 at approximately the same level…
Year: 1996
Type: Document
Source: FRAMES
Potter
Lower atmosphere moistures, temperatures, winds, and lapse rates are examined for the days of 339 fires over 400 ha in the United States from 1971 through 1984. These quantities are compared with a climatology dataset from the same 14-year period using 2-way unbalanced analysis…
Year: 1996
Type: Document
Source: FRAMES, TTRS
Harrington
Ecosystems are envisioned as integrated, complex systems with both living and non-living components, that are linked through processes of energy flow and nutrient cycling (Bowen, 1971; Ricklefs, 1979). The ecosystem approach seeks to describe the components of this system, the…
Year: 1996
Type: Document
Source: FRAMES
Neilson, Running
Chapter 23 in the book titled, Global change and terrestrial ecosystems.
Year: 1996
Type: Document
Source: FRAMES
Starfield, Chapin
One of the greatest challenges in global-change research is to predict the future distribution of vegetation. Most models of vegetation change predict either the response of a patch of present vegetation to climatic change or the future equilibrium distribution of vegetation…
Year: 1996
Type: Document
Source: FRAMES
Nash, Johnson
The coupling of synoptic scale weather conditions with local scale weather and fuel conditions was examined for 2551 fires and 1,537,624 lightning strikes for the May-August fire seasons in 1988, 1989, 1992, and 1993 in Alberta and Saskatchewan. The probability of lightning fire…
Year: 1996
Type: Document
Source: FRAMES
Bauer
The Atmospheric Boundary Layer (ABL) is the lowest portion of the Earth's atmosphere which is affected significantly by the properties of the Earth's (land or ocean) surface. The ABL may show a large daily variation in wind, temperature, and stability or turbulence. The ABL is…
Year: 1996
Type: Document
Source: FRAMES
McKenzie, Peterson, Alvarado
Models of vegetation change in response to global warming need to incorporate the effects of disturbance at broad spatial scales. Process-based predictive models, whether for fire behavior or fire effects on vegetation, assume homogeneity of crucial inputs over the spatial scale…
Year: 1996
Type: Document
Source: FRAMES, TTRS
Levine
The 1989 report of the National Research Council, Global Change and Our Common Future states: "Our planet and global environment are witnessing the most profound changes in the brief history of the human species. Human activity is the major agent of those changes - depletion of…
Year: 1996
Type: Document
Source: FRAMES
Wein, de Groot
Residents of Canada and other northern circumpolar countries are concerned with the scenarios of climate change since Global Circulation Models predict that global warming over the next 30-50 years will be most evident in the northern regions (Bolin et at. 1986; Roots 1989;…
Year: 1996
Type: Document
Source: FRAMES, TTRS
Volney
Insects are the most diverse group of terrestrial animals. Not surprisingly, they influence several ecosystem processes and thus have a profound influence in most terrestrial ecosystems by occupying a myriad o f niches. The reciprocal interaction of insects with forest plants…
Year: 1996
Type: Document
Source: FRAMES
Sykes, Prentice
Changes in the global carbon (C) cycle caused by human activities have focused the attention of environmental scientists on where and how C is distributed through the terrestrial biosphere. Forests are the largest land reservoir for C (e.g., see Kellomäki and Karjalainen,…
Year: 1996
Type: Document
Source: FRAMES
Swetnam
Siberian forests are shaped by complex interactions of climate, forest fires, insect outbreaks, and humans. Unravelling the linkages and mechanisms of these interactions will require long temporal and large spatial-scale perspectives. A full account of the past input of Siberian…
Year: 1996
Type: Document
Source: FRAMES
Stocks, Cahoon, Levine, Cofer, Lynham
From introduction: 'The boreal forest biome is a classic fire-dependent ecosystem, capable, during periods of extreme fire weather, of sustaining the large, high-intensity wildfires responsible for its existence. The natural fire cycle in the North American boreal forest…
Year: 1996
Type: Document
Source: FRAMES
Stocks, Lynham
The boreal forest, or taiga, predominates as a vegetation type in northern circumpolar countries, covering in excess of 12 million square kilometres, primarily in Russia and Canada, with lesser amounts in Scandinavia, China, and the United States (Alaska). Lying generally…
Year: 1996
Type: Document
Source: FRAMES
Shvidenko, Nilsson, Rojkov, Strakhov
The total land area of the Russian boreal zone is 1527.6 Mha, including 1143.0 Mha of Forest Fund areas and 735.8 Mha of forested areas. These estimates are based on Forest State Account data (Goscomles SSSR 1990, 1991). Forest Fund areas include forest land and nonforest land.…
Year: 1996
Type: Document
Source: FRAMES
Kurz, Apps
The Canadian boreal forest is comprised largely of even-aged stands that for millennia have undergone cycles of disturbance (i.e., fires or insect-induced stand mortality) and regrowth. Previous studies of regional-scale carbon (C) budgets have assumed that, when averaged over a…
Year: 1996
Type: Document
Source: FRAMES
Fosberg, Stocks, Lynham
Description not entered.
Year: 1996
Type: Document
Source: FRAMES
Cofer, Winstead, Stocks, Overbay, Goldammer, Cahoon, Levine
Description not entered.
Year: 1996
Type: Document
Source: FRAMES