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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 The database provides a listing of fire research publications relevant to Alaska and a venue for sharing unpublished agency reports and works in progress that are not normally found in the published literature.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 376 - 400 of 410

Soja, Al-Saadi, Pouliot, Kittaka, Zhang, Raffuse, Wiedinmyer
Area burned is one of four primary parameters necessary for estimating biomass burning emissions, and it is a parameter than remains illusive, particularly if we include all area burned. In this report, we compare the intensive 2002 ground-based data for the western United…
Year: 2009
Type: Document
Source: TTRS

Barker, Amiro, Kwon, Ewers, Angstmann
The Canadian boreal forest consists of a mosaic of landscapes of varying soil drainage and forest age driven by wildfire. The hydrological consequences are complicated by plant responses to soil moisture and forest age, both potentially influencing evapotranspiration.…
Year: 2009
Type: Document
Source: TTRS

Marchand, Prairie, Del Giorgio
Natural fires annually decimate up to 1% of the forested area in the boreal region of Quebec, and represent a major structuring force in the region, creating a mosaic of watersheds characterized by large variations in vegetation structure and composition. Here, we investigate…
Year: 2009
Type: Document
Source: TTRS

Magnussen
A simulation of regional and national forest carbon balance in Canada requires, due to regional correlations, a joint simulation of areas burned (BA) in regional fires. Regional correlations of BA are largely determined by concurrent years of relatively large (LF) and small…
Year: 2009
Type: Document
Source: TTRS

Girardin, Ali, Carcaillet, Mudelsee, Drobyshev, Hély, Bergeron
We investigated changes in wildfire risk over the 1901-2002 (AD) period with an analysis of broad-scale patterns of July monthly drought code (MDC) variability on 28 forested ecoregions of the North American and Eurasian continents. The MDC is an estimate of the net effect of…
Year: 2009
Type: Document
Source: TTRS

Frolking, Palace, Clark, Chambers, Shugart, Hurtt
Abrupt forest disturbances generating gaps >0.001 km2 impact roughly 0.4-0.7 million km2 a-1. Fire, windstorms, logging, and shifting cultivation are dominant disturbances; minor contributors are land conversion, flooding, landslides, and avalanches. All can have substantial…
Year: 2009
Type: Document
Source: TTRS

Doerr, Woods, Martin, Casimiro
Soils under a wide range of vegetation types exhibit water repellency following the passage of a fire. This is viewed by many as one of the main causes for accelerated post-fire runoff and soil erosion and it has often been assumed that strong soil water repellency present after…
Year: 2009
Type: Document
Source: TTRS

Bryant, Clausen, Swihart, Landhausser, Stevens, Hawkins, Carrière, Kirilenko, Veitch, Popko, Cleland, Williams, Jakubas, Carlson, Bodony, Cebrian, Paragi, Picone, Moore, Packee, Malone
Fire has been the dominant disturbance in boreal America since the Pleistocene, resulting in a spatial mosaic in which the most fire occurs in the continental northwest. Spatial variation in snowshoe hare (Lepus americanus) density reflects the fire mosaic. Because fire…
Year: 2009
Type: Document
Source: TTRS

Balshi, McGuire, Duffy, Flannigan, Kicklighter, Melillo
The boreal forest contains large reserves of carbon. Across this region, wildfires influence the temporal and spatial dynamics of carbon storage. In this study, we estimate fire emissions and changes in carbon storage for boreal North America over the 21st century. We use a…
Year: 2009
Type: Document
Source: TTRS

Wells
From the text ... 'Removing hazardous fuels to reduce the risk of wildfire has become a priority for land managers across the United States. Utilizing biomass taken from forests to cover the cost of fuel reduction is an attractive ideal. Effective utilization could also address…
Year: 2009
Type: Document
Source: TTRS

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: TTRS

Wieder, Scott, Kamminga, Vile, Vitt, Bone, Xu, Benscoter, Bhatti
Boreal peatland ecosystems occupy about 3.5 million km2 of the earth's land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and…
Year: 2009
Type: Document
Source: TTRS

van der Kamp, Yassir, Buurman
Soil carbon changes upon secondary succession in Imperata grasslands are important both for their effect on potential production and for possible implications of forest degradation and regeneration on global climate change. We studied the effect of forest regeneration after fire…
Year: 2009
Type: Document
Source: TTRS

Langner, Siegert
South-east Asia's tropical rainforests are experiencing the highest rate of deforestation worldwide and fire is one of the most important drivers of forest loss and subsequent carbon dioxide emissions. In this study, we analyzed all fire events in Borneo recorded by satellites…
Year: 2009
Type: Document
Source: TTRS

Langmann, Duncan, Textor, Trentmann, Van der Werf
Gaseous and particulate emissions from vegetation fires substantially modify the atmospheric chemical composition, degrade air quality and can alter weather and climate. The impact of vegetation fire emissions on air pollution and climate has been recognised in the late 1970s.…
Year: 2009
Type: Document
Source: TTRS

Kane, Vogel
To understand how carbon (C) pools in boreal ecosystems may change with warming, we measured above- and belowground C pools and C increment along a soil temperature gradient across 16 mature upland black spruce (Picea mariana Mill. [B·S.P]) forests in interior Alaska. Total…
Year: 2009
Type: Document
Source: TTRS

Flannigan, Stocks, Turetsky, Wotton
Forest fires are a significant and natural element of the circumboreal forest. Fire activity is strongly linked to weather, and increased fire activity due to climate change is anticipated or arguably has already occurred. Recent studies suggest a doubling of area burned along…
Year: 2009
Type: Document
Source: TTRS

Norris, Quideau, Bhatti, Wasylishen, MacKenzie
Boreal forest soils represent a considerable reservoir of carbon on a global basis. The objective of this study was to compare the response of soil organic carbon (OC) to disturbance along two jack pine (Pinus banksiana Lamb.) chronosequences of either fire or harvest origin.…
Year: 2009
Type: Document
Source: TTRS

The Forest Health Monitoring Program's annual national technical report presents results of forest health analyses from a national perspective using data from a variety of sources. The report is organized according to the Criteria and Indicators for the Conservation and…
Year: 2009
Type: Document
Source: TTRS

Betts, Jones
With climatic warming, wildfire occurrence is increasing in the boreal forest of interior Alaska. Loss of catchment vegetation during fire can impact streams directly through altered solute and debris inputs and changed light and temperature regimes. Over longer time scales,…
Year: 2009
Type: Document
Source: TTRS

Styger, Fernandes, Rakotondramasy, Rajaobelinirina
Soil fertility restoration depends on natural fallows in the slash-and-burn system of eastern Madagascar. In the Beforona-Vohidrazana study zone, none of the fallow species are able to withstand the slashing, burning and cropping frequencies of 3-5 years. Eventually soils are…
Year: 2009
Type: Document
Source: TTRS

Duran, Rodriguez, Fernandez-Palacios, Gallardo
The concern that climate change may increase fire frequency and intensity has recently heightened the interest in the effects of wildfires on ecosystem functioning. Although short-term fire effects on forest soils are well known, less information can be found on the long-term…
Year: 2009
Type: Document
Source: TTRS

Smithwick, Ryan, Kashian, Romme, Tinker, Turner
The interaction between disturbance and climate change and resultant effects on ecosystem carbon (C) and nitrogen (N) fluxes are poorly understood. Here, we model (using CENTURY version 4.5) how climate change may affect C and N fluxes among mature and regenerating lodgepole…
Year: 2009
Type: Document
Source: TTRS

Okin, Parsons, Herrick, Bestelmeyer, Peters, Fredrickson
Arid and semiarid regions cover more than 40% of Earths land surface. Desertification, or broadscale land degradation in drylands, is a major environmental hazard facing inhabitants of the world's deserts as well as an important component of global change. There is no unifying…
Year: 2009
Type: Document
Source: TTRS

O'Donnell, Turetsky, Harden, Manies, Pruett, Shetler, Neff
Fire is an important control on the carbon (C) balance of the boreal forest region. Here, we present findings from two complementary studies that examine how fire modifies soil organic matter properties, and how these modifications influence rates of decomposition and C exchange…
Year: 2009
Type: Document
Source: TTRS