2004 Alaska wildfires | |
---|---|
Statistics [1] | |
Total fires | 701 |
Total area | 6,600,000 acres (10,300 sq mi; 27,000 km2)+ |
The 2004 Alaska fire season was the worst wildfire season on record in the U.S. state of Alaska in terms of area burned. [2] Though the 1989 fire season recorded more fires, nearly 1,000, the 2004 season burned more than 6,600,000 acres (10,300 sq mi; 27,000 km2) in just 701 fires. [1] The largest of these fires was the Taylor Complex Fire. [3] This fire consumed over 1,700,000 acres (2,700 sq mi; 6,900 km2) and was the deemed to be the largest fire in the United States from at least 1997 to 2019. [3] Out of all 701 fires, 426 fires were started by humans and 215 by lightning. [1]
The general weather pattern for Interior Alaska is May is wet, June is hot and dry, July is transitional, and August is rainy. Beginning in May 2004, the summer was extremely warm and wet in comparison to typical Interior Alaska summer climate. The fire season was forecasted as average. Beginning in mid June, there was a drying trend, and was second warmest in 100 years. After the conclusion of the season, summer 2004 was described by a National Weather Service meteorologist as "three Junes." [4]
Much of the rain over the summer of 2004 came during thunderstorms, which resulted in record amounts of lightning triggering many of the original fires near Fairbanks, Alaska. [5] Wildfires are prone to develop in areas with frequent lightning strikes. [6] After months of lightning and increased temperatures, an uncharacteristically dry August resulted in fires continuing through September. [5]
Alaska has a climate that of the boreal zone, more commonly known as taiga. [7] The boreal zone, across the globe, makes up more than 25% of global forests, and when wildfires occur it is a top leader in carbon emissions. [7] Approximately 12% of the world's carbon is stored in top layer soil and this part is the first to burn in any wildfire. [8] These emissions have some of the greatest impacts on natural carbon balance, and Alaska gives its fair contribution. [8] Typically Alaskan forest fires make up 41% of the United States' carbon emissions from wildland fires, but more recently with warming conditions and more wildfire occurrences these figures have gone all the way to 89%. [8] Landscape is also changing as a result of wildfires. Less canopy is provided in the aftermath of a wildfire, hence soil temperatures may rise, rendering the area uninhabitable by certain species and allow new, non-native species to thrive. [8] When soil temperatures rise, permafrost is also revealed and begins to melt away, which can lead to landslides and erosion. [8]
The 2004 fire season of Alaska had large impacts on the air quality and safety of nearby populations. These impacts most significant in Fairbanks, Alaska. [1] For over 15 days, particulate matter measured 1,000 micrograms per cubic meter, well over the EPA thresholds for hazardous and unhealthy air quality. [1] To put it into perspective, an area deemed to be unhealthy typically has 65 micrograms of smoke particulate per cubic meter, while an area deemed to be hazardous has anymore than 250 micrograms per cubic meter. [1] Normal levels in Fairbanks, Alaska are typically 10 micrograms per cubic meter. [1] The main issue with smoke particulate is not the smoke itself but the matter that is mixed in. Wildfire smoke is usually made up of acids, chemicals, metals, soil/dust, and pollen/mold spores. [1]
Interior Alaska is the central region of Alaska's territory, roughly bounded by the Alaska Range to the south and the Brooks Range to the north. It is largely wilderness. Mountains include Denali in the Alaska Range, the Wrangell Mountains, and the Ray Mountains. The native people of the interior are Alaskan Athabaskans. The largest city in the interior is Fairbanks, Alaska's second-largest city, in the Tanana Valley. Other towns include North Pole, just southeast of Fairbanks, Eagle, Tok, Glennallen, Delta Junction, Nenana, Anderson, Healy and Cantwell. The interior region has an estimated population of 113,154.
Taiga or tayga, also known as boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces, and larches. The taiga or boreal forest is the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean, much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan.
A wildfire, forest fire, or a bushfire is an unplanned, uncontrolled and unpredictable fire in an area of combustible vegetation. Depending on the type of vegetation present, a wildfire may be more specifically identified as a bushfire, desert fire, grass fire, hill fire, peat fire, prairie fire, vegetation fire, or veld fire. Some natural forest ecosystems depend on wildfire. Wildfires are different from controlled or prescribed burning, which are carried out to provide a benefit for people. Modern forest management often engages in prescribed burns to mitigate fire risk and promote natural forest cycles. However, controlled burns can turn into wildfires by mistake.
A controlled or prescribed (Rx) burn is the practice of intentionally setting a fire to change the assemblage of vegetation and decaying material in a landscape. The purpose could be for forest management, ecological restoration, land clearing or wildfire fuel management. A controlled burn may also refer to the intentional burning of slash and fuels through burn piles. Controlled burns may also be referred to as hazard reduction burning, backfire, swailing or a burn-off. In industrialized countries, controlled burning regulations and permits are usually overseen by fire control authorities.
Fire ecology is a scientific discipline concerned with the effects of fire on natural ecosystems. Many ecosystems, particularly prairie, savanna, chaparral and coniferous forests, have evolved with fire as an essential contributor to habitat vitality and renewal. Many plant species in fire-affected environments use fire to germinate, establish, or to reproduce. Wildfire suppression not only endangers these species, but also the animals that depend upon them.
Smouldering or smoldering is the slow, flameless form of combustion, sustained by the heat evolved when oxygen directly attacks the surface of a condensed-phase fuel. Many solid materials can sustain a smouldering reaction, including coal, cellulose, wood, cotton, tobacco, cannabis, peat, plant litter, humus, synthetic foams, charring polymers including polyurethane foam and some types of dust. Common examples of smouldering phenomena are the initiation of residential fires on upholstered furniture by weak heat sources, and the persistent combustion of biomass behind the flaming front of wildfires.
Wildfire suppression is a range of firefighting tactics used to suppress wildfires. Firefighting efforts depend on many factors such as the available fuel, the local atmospheric conditions, the features of the terrain, and the size of the wildfire. Because of this wildfire suppression in wild land areas usually requires different techniques, equipment, and training from the more familiar structure fire fighting found in populated areas. Working in conjunction with specially designed aerial firefighting aircraft, fire engines, tools, firefighting foams, fire retardants, and using various firefighting techniques, wildfire-trained crews work to suppress flames, construct fire lines, and extinguish flames and areas of heat in order to protect resources and natural wilderness. Wildfire suppression also addresses the issues of the wildland–urban interface, where populated areas border with wild land areas.
The Yellowstone fires of 1988 collectively formed the largest wildfire in the recorded history of Yellowstone National Park in the United States. Starting as many smaller individual fires, the flames quickly spread out of control due to drought conditions and increasing winds, combining into several large conflagrations which burned for several months. The fires almost destroyed two major visitor destinations and, on September 8, 1988, the entire park was closed to all non-emergency personnel for the first time in its history. Only the arrival of cool and moist weather in the late autumn brought the fires to an end. A total of 793,880 acres (3,213 km2), or 36 percent of the park, burned at varying levels of severity.
A boreal ecosystem is an ecosystem with a subarctic climate located in the Northern Hemisphere, approximately between 50° and 70°N latitude. These ecosystems are commonly known as taiga and are located in parts of North America, Europe, and Asia. The ecosystems that lie immediately to the south of boreal zones are often called hemiboreal. There are a variety of processes and species that occur in these areas as well.
The 2008 California wildfire season was one of the most devastating in the state of the 21st century. While 6,255 fires occurred, about two-thirds as many as in 2007, the total area burned— 1,593,690 acres —far exceeded that of previous years.
A dry thunderstorm is a thunderstorm that produces thunder and lightning, but where all or most of its precipitation evaporates before reaching the ground. Dry lightning refers to lightning strikes occurring in this situation. Both are so common in the American West that they are sometimes used interchangeably.
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Wildfires are outdoor fires that occur in the wilderness or other vast spaces. Other common names associated with wildfires are brushfire and forest fire. Since wildfires can occur anywhere on the planet, except for Antarctica, they pose a threat to civilizations and wildlife alike. In terms of emergency management, wildfires can be particularly devastating. Given their ability to destroy large areas of entire ecosystems, there must be a contingency plan in effect to be as prepared as possible in case of a wildfire and to be adequately prepared to handle the aftermath of one as well.
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Terrestrial ecosystems found in the boreal regions of North America and Eurasia cover 17% of the Earth's land surface, and contain more than 30% of all carbon present in the terrestrial biome. In terms of carbon storage, the boreal region consists of three ecosystems: boreal forest, peatland, and tundra. Vast areas of the globe and are contributing greatly to atmospheric carbon release due to increased temperature and fire hazard. High northern latitudes will experience the most significant increase in warming on the planet as a result of increased atmospheric greenhouse gases thus placing in jeopardy the carbon sink in these areas. In addition to the release of carbon through the melting of permafrost, high intensity wildfires will become more common and thus contribute to the release of stored carbon. This means that the boreal forest and its fire regime is becoming an increasingly more significant factor in determining the global carbon budget.
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