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A wildfire or wildland fire is a fire in an area of combustible vegetation that occurs in the countryside or rural area. Depending on the type of vegetation where it occurs, a wildfire can also be classified more specifically as a brush fire, bush fire, desert fire, forest fire, grass fire, hill fire, peat fire, vegetation fire, or veld fire. Fossil charcoal indicates that wildfires began soon after the appearance of terrestrial plants 420 million years ago. Wildfire’s occurrence throughout the history of terrestrial life invites conjecture that fire must have had pronounced evolutionary effects on most ecosystems' flora and fauna. Earth is an intrinsically flammable planet owing to its cover of carbon-rich vegetation, seasonally dry climates, atmospheric oxygen, and widespread lightning and volcano ignitions.
Wildfires can be characterized in terms of the cause of ignition, their physical properties, the combustible material present, and the effect of weather on the fire. Wildfires can cause damage to property and human life, but they have many beneficial effects on native vegetation, animals, and ecosystems that have evolved with fire. Many plant species depend on the effects of fire for growth and reproduction. However, wildfire in ecosystems where wildfire is uncommon or where non-native vegetation has encroached may have negative ecological effects. Wildfire behaviour and severity result from the combination of factors such as available fuels, physical setting, and weather. Analyses of historical meteorological data and national fire records in western North America show the primacy of climate in driving large regional fires via wet periods that create substantial fuels or drought and warming that extend conducive fire weather.
Strategies of wildfire prevention, detection, and suppression have varied over the years. One common and inexpensive technique is controlled burning: permitting or even igniting smaller fires to minimize the amount of flammable material available for a potential wildfire. Vegetation may be burned periodically to maintain high species diversity and frequent burning of surface fuels limits fuel accumulation. Wildland fire use is the cheapest and most ecologically appropriate policy for many forests. Fuels may also be removed by logging, but fuels treatments and thinning have no effect on severe fire behavior when under extreme weather conditions. Wildfire itself is reportedly "the most effective treatment for reducing a fire's rate of spread, fireline intensity, flame length, and heat per unit of area" according to Jan Van Wagtendonk, a biologist at the Yellowstone Field Station. Building codes in fire-prone areas typically require that structures be built of flame-resistant materials and a defensible space be maintained by clearing flammable materials within a prescribed distance from the structure.
- 1 Causes
- 2 Spread
- 3 Physical properties
- 4 Effect of weather
- 5 Ecology
- 6 History
- 7 Prevention
- 8 Detection
- 9 Suppression
- 10 Fire retardant
- 11 Human risk and exposure
- 12 Health effects
- 13 Notable wildfires
- 14 See also
- 15 References
- 16 Bibliography
- 17 External links
The most common direct human causes of wildfire ignition include arson, discarded cigarettes, power-line arcs (as detected by arc mapping), and sparks from equipment. Ignition of wildland fires via contact with hot rifle-bullet fragments is also possible under the right conditions. Wildfires can also be started in communities experiencing shifting cultivation, where land is cleared quickly and farmed until the soil loses fertility, and slash and burn clearing. Forested areas cleared by logging encourage the dominance of flammable grasses, and abandoned logging roads overgrown by vegetation may act as fire corridors. Annual grassland fires in southern Vietnam stem in part from the destruction of forested areas by US military herbicides, explosives, and mechanical land-clearing and -burning operations during the Vietnam War.
The most common cause of wildfires varies throughout the world. In Canada and northwest China, for example, lightning operates as the major source of ignition. In other parts of the world, human involvement is a major contributor. In Africa, Central America, Fiji, Mexico, New Zealand, South America, and Southeast Asia, wildfires can be attributed to human activities such as agriculture, animal husbandry, and land-conversion burning. In China and in the Mediterranean Basin, human carelessness is a major cause of wildfires. In the United States and Australia, the source of wildfires can be traced both to lightning strikes and to human activities (such as machinery sparks, cast-away cigarette butts, or arson)." Coal seam fires burn in the thousands around the world, such as those in Burning Mountain, New South Wales; Centralia, Pennsylvania; and several coal-sustained fires in China. They can also flare up unexpectedly and ignite nearby flammable material.
The spread of wildfires varies based on the flammable material present, its vertical arrangement and moisture content, and weather conditions. Fuel arrangement and density is governed in part by topography, as land shape determines factors such as available sunlight and water for plant growth. Overall, fire types can be generally characterized by their fuels as follows:
- Ground fires are fed by subterranean roots, duff and other buried organic matter. This fuel type is especially susceptible to ignition due to spotting. Ground fires typically burn by smoldering, and can burn slowly for days to months, such as peat fires in Kalimantan and Eastern Sumatra, Indonesia, which resulted from a riceland creation project that unintentionally drained and dried the peat.
- Crawling or surface fires are fueled by low-lying vegetation such as leaf and timber litter, debris, grass, and low-lying shrubbery.
- Ladder fires consume material between low-level vegetation and tree canopies, such as small trees, downed logs, and vines. Kudzu, Old World climbing fern, and other invasive plants that scale trees may also encourage ladder fires.
- Crown, canopy, or aerial fires burn suspended material at the canopy level, such as tall trees, vines, and mosses. The ignition of a crown fire, termed crowning, is dependent on the density of the suspended material, canopy height, canopy continuity, sufficient surface and ladder fires, vegetation moisture content, and weather conditions during the blaze. Stand-replacing fires lit by humans can spread into the Amazon rain forest, damaging ecosystems not particularly suited for heat or arid conditions.
Wildfires occur when all of the necessary elements of a fire triangle come together in a susceptible area: an ignition source is brought into contact with a combustible material such as vegetation, that is subjected to sufficient heat and has an adequate supply of oxygen from the ambient air. A high moisture content usually prevents ignition and slows propagation, because higher temperatures are required to evaporate any water within the material and heat the material to its fire point. Dense forests usually provide more shade, resulting in lower ambient temperatures and greater humidity, and are therefore less susceptible to wildfires. Less dense material such as grasses and leaves are easier to ignite because they contain less water than denser material such as branches and trunks. Plants continuously lose water by evapotranspiration, but water loss is usually balanced by water absorbed from the soil, humidity, or rain. When this balance is not maintained, plants dry out and are therefore more flammable, often a consequence of droughts.
A wildfire front is the portion sustaining continuous flaming combustion, where unburned material meets active flames, or the smoldering transition between unburned and burned material. As the front approaches, the fire heats both the surrounding air and woody material through convection and thermal radiation. First, wood is dried as water is vaporized at a temperature of 100 °C (212 °F). Next, the pyrolysis of wood at 230 °C (450 °F) releases flammable gases. Finally, wood can smoulder at 380 °C (720 °F) or, when heated sufficiently, ignite at 590 °C (1,000 °F). Even before the flames of a wildfire arrive at a particular location, heat transfer from the wildfire front warms the air to 800 °C (1,470 °F), which pre-heats and dries flammable materials, causing materials to ignite faster and allowing the fire to spread faster. High-temperature and long-duration surface wildfires may encourage flashover or torching: the drying of tree canopies and their subsequent ignition from below.
Wildfires have a rapid forward rate of spread (FROS) when burning through dense, uninterrupted fuels. They can move as fast as 10.8 kilometres per hour (6.7 mph) in forests and 22 kilometres per hour (14 mph) in grasslands. Wildfires can advance tangential to the main front to form a flanking front, or burn in the opposite direction of the main front by backing. They may also spread by jumping or spotting as winds and vertical convection columns carry firebrands (hot wood embers) and other burning materials through the air over roads, rivers, and other barriers that may otherwise act as firebreaks. Torching and fires in tree canopies encourage spotting, and dry ground fuels that surround a wildfire are especially vulnerable to ignition from firebrands. Spotting can create spot fires as hot embers and firebrands ignite fuels downwind from the fire. In Australian bushfires, spot fires are known to occur as far as 20 kilometres (12 mi) from the fire front.
Especially large wildfires may affect air currents in their immediate vicinities by the stack effect: air rises as it is heated, and large wildfires create powerful updrafts that will draw in new, cooler air from surrounding areas in thermal columns. Great vertical differences in temperature and humidity encourage pyrocumulus clouds, strong winds, and fire whirls with the force of tornadoes at speeds of more than 80 kilometres per hour (50 mph). Rapid rates of spread, prolific crowning or spotting, the presence of fire whirls, and strong convection columns signify extreme conditions.
Effect of weather
Heat waves, droughts, cyclical climate changes such as El Niño, and regional weather patterns such as high-pressure ridges can increase the risk and alter the behavior of wildfires dramatically. Years of precipitation followed by warm periods can encourage more widespread fires and longer fire seasons. Since the mid-1980s, earlier snowmelt and associated warming has also been associated with an increase in length and severity of the wildfire season in the Western United States. Global warming may increase the intensity and frequency of droughts in many areas, creating more intense and frequent wildfires. A 2015 study indicates that the increase in fire risk in California may be attributable to human-induced climate change. A study of alluvial sediment deposits going back over 8,000 years found warmer climate periods experienced severe droughts and stand-replacing fires and concluded climate was such a powerful influence on wildfire that trying to recreate presettlement forest structure is likely impossible in a warmer future.
Intensity also increases during daytime hours. Burn rates of smoldering logs are up to five times greater during the day due to lower humidity, increased temperatures, and increased wind speeds. Sunlight warms the ground during the day which creates air currents that travel uphill. At night the land cools, creating air currents that travel downhill. Wildfires are fanned by these winds and often follow the air currents over hills and through valleys. Fires in Europe occur frequently during the hours of 12:00 p.m. and 2:00 p.m. Wildfire suppression operations in the United States revolve around a 24-hour fire day that begins at 10:00 a.m. due to the predictable increase in intensity resulting from the daytime warmth.
Wildfire’s occurrence throughout the history of terrestrial life invites conjecture that fire must have had pronounced evolutionary effects on most ecosystems' flora and fauna. Wildfires are common in climates that are sufficiently moist to allow the growth of vegetation but feature extended dry, hot periods. Such places include the vegetated areas of Australia and Southeast Asia, the veld in southern Africa, the fynbos in the Western Cape of South Africa, the forested areas of the United States and Canada, and the Mediterranean Basin.
High-severity wildfire creates complex early seral forest habitat (also called “snag forest habitat”), which often has higher species richness and diversity than unburned old forest. Plant and animal species in most types of North American forests evolved with fire, and many of these species depend on wildfires, and particularly high-severity fires, to reproduce and grow. Fire helps to return nutrients from plant matter back to soil, the heat from fire is necessary to the germination of certain types of seeds, and the snags (dead trees) and early successional forests created by high-severity fire create habitat conditions that are beneficial to wildlife. Early successional forests created by high-severity fire support some of the highest levels of native biodiversity found in temperate conifer forests. Post-fire logging has no ecological benefits and many negative impacts; the same is often true for post-fire seeding.
Although some ecosystems rely on naturally occurring fires to regulate growth, some ecosystems suffer from too much fire, such as the chaparral in southern California and lower elevation deserts in the American Southwest. The increased fire frequency in these ordinarily fire-dependent areas has upset natural cycles, damaged native plant communities, and encouraged the growth of non-native weeds. Invasive species, such as Lygodium microphyllum and Bromus tectorum, can grow rapidly in areas that were damaged by fires. Because they are highly flammable, they can increase the future risk of fire, creating a positive feedback loop that increases fire frequency and further alters native vegetation communities.
In the Amazon Rainforest, drought, logging, cattle ranching practices, and slash-and-burn agriculture damage fire-resistant forests and promote the growth of flammable brush, creating a cycle that encourages more burning. Fires in the rainforest threaten its collection of diverse species and produce large amounts of CO2. Also, fires in the rainforest, along with drought and human involvement, could damage or destroy more than half of the Amazon rainforest by the year 2030. Wildfires generate ash, destroy available organic nutrients, and cause an increase in water runoff, eroding away other nutrients and creating flash flood conditions. A 2003 wildfire in the North Yorkshire Moors destroyed 2.5 square kilometers (600 acres) of heather and the underlying peat layers. Afterwards, wind erosion stripped the ash and the exposed soil, revealing archaeological remains dating back to 10,000 BC. Wildfires can also have an effect on climate change, increasing the amount of carbon released into the atmosphere and inhibiting vegetation growth, which affects overall carbon uptake by plants.
In tundra there is a natural pattern of accumulation of fuel and wildfire which varies depending on the nature of vegetation and terrain. Research in Alaska has shown fire-event return intervals, (FRIs) that typically vary from 150 to 200 years with dryer lowland areas burning more frequently than wetter upland areas.
Plants in wildfire-prone ecosystems often survive through adaptations to their local fire regime. Such adaptations include physical protection against heat, increased growth after a fire event, and flammable materials that encourage fire and may eliminate competition. For example, plants of the genus Eucalyptus contain flammable oils that encourage fire and hard sclerophyll leaves to resist heat and drought, ensuring their dominance over less fire-tolerant species. Dense bark, shedding lower branches, and high water content in external structures may also protect trees from rising temperatures. Fire-resistant seeds and reserve shoots that sprout after a fire encourage species preservation, as embodied by pioneer species. Smoke, charred wood, and heat can stimulate the germination of seeds in a process called serotiny. Exposure to smoke from burning plants promotes germination in other types of plants by inducing the production of the orange butenolide.
Grasslands in Western Sabah, Malaysian pine forests, and Indonesian Casuarina forests are believed to have resulted from previous periods of fire. Chamise deadwood litter is low in water content and flammable, and the shrub quickly sprouts after a fire. Cape lilies lie dormant until flames brush away the covering, then blossom almost overnight. Sequoia rely on periodic fires to reduce competition, release seeds from their cones, and clear the soil and canopy for new growth. Caribbean Pine in Bahamian pineyards have adapted to and rely on low-intensity, surface fires for survival and growth. An optimum fire frequency for growth is every 3 to 10 years. Too frequent fires favor herbaceous plants, and infrequent fires favor species typical of Bahamian dry forests.
Most of the Earth's weather and air pollution resides in the troposphere, the part of the atmosphere that extends from the surface of the planet to a height of about 10 kilometers (6 mi). The vertical lift of a severe thunderstorm or pyrocumulonimbus can be enhanced in the area of a large wildfire, which can propel smoke, soot, and other particulate matter as high as the lower stratosphere. Previously, prevailing scientific theory held that most particles in the stratosphere came from volcanoes, but smoke and other wildfire emissions have been detected from the lower stratosphere. Pyrocumulus clouds can reach 6,100 meters (20,000 ft) over wildfires. Satellite observation of smoke plumes from wildfires revealed that the plumes could be traced intact for distances exceeding 1,600 kilometers (1,000 mi). Computer-aided models such as CALPUFF may help predict the size and direction of wildfire-generated smoke plumes by using atmospheric dispersion modeling.
Wildfires can affect local atmospheric pollution, and release carbon in the form of carbon dioxide. Wildfire emissions contain fine particulate matter which can cause cardiovascular and respiratory problems. Increased fire byproducts in the troposphere can increase ozone concentration beyond safe levels. Forest fires in Indonesia in 1997 were estimated to have released between 0.81 and 2.57 gigatonnes (0.89 and 2.83 billion short tons) of CO2 into the atmosphere, which is between 13%–40% of the annual global carbon dioxide emissions from burning fossil fuels. Atmospheric models suggest that these concentrations of sooty particles could increase absorption of incoming solar radiation during winter months by as much as 15%.
In the Welsh Borders, the first evidence of wildfire is rhyniophytoid plant fossils preserved as charcoal, dating to the Silurian period (about ). Smoldering surface fires started to occur sometime before the Early Devonian period . Low atmospheric oxygen during the Middle and Late Devonian was accompanied by a decrease in charcoal abundance. Additional charcoal evidence suggests that fires continued through the Carboniferous period. Later, the overall increase of atmospheric oxygen from 13% in the Late Devonian to 30-31% by the Late Permian was accompanied by a more widespread distribution of wildfires. Later, a decrease in wildfire-related charcoal deposits from the late Permian to the Triassic periods is explained by a decrease in oxygen levels.
Wildfires during the Paleozoic and Mesozoic periods followed patterns similar to fires that occur in modern times. Surface fires driven by dry seasons[clarification needed] are evident in Devonian and Carboniferous progymnosperm forests. Lepidodendron forests dating to the Carboniferous period have charred peaks, evidence of crown fires. In Jurassic gymnosperm forests, there is evidence of high frequency, light surface fires. The increase of fire activity in the late Tertiary is possibly due to the increase of C4-type grasses. As these grasses shifted to more mesic habitats, their high flammability increased fire frequency, promoting grasslands over woodlands. However, fire-prone habitats may have contributed to the prominence of trees such as those of the genera Eucalyptus, Pinus and Sequoia, which have thick bark to withstand fires and employ serotiny.
The human use of fire for agricultural and hunting purposes during the Paleolithic and Mesolithic ages altered the preexisting landscapes and fire regimes. Woodlands were gradually replaced by smaller vegetation that facilitated travel, hunting, seed-gathering and planting. In recorded human history, minor allusions to wildfires were mentioned in the Bible and by classical writers such as Homer. However, while ancient Hebrew, Greek, and Roman writers were aware of fires, they were not very interested in the uncultivated lands where wildfires occurred. Wildfires were used in battles throughout human history as early thermal weapons. From the Middle ages, accounts were written of occupational burning as well as customs and laws that governed the use of fire. In Germany, regular burning was documented in 1290 in the Odenwald and in 1344 in the Black Forest. In the 14th century Sardinia, firebreaks were used for wildfire protection. In Spain during the 1550s, sheep husbandry was discouraged in certain provinces by Philip II due to the harmful effects of fires used in transhumance. As early as the 17th century, Native Americans were observed using fire for many purposes including cultivation, signaling, and warfare. Scottish botanist David Douglas noted the native use of fire for tobacco cultivation, to encourage deer into smaller areas for hunting purposes, and to improve foraging for honey and grasshoppers. Charcoal found in sedimentary deposits off the Pacific coast of Central America suggests that more burning occurred in the 50 years before the Spanish colonization of the Americas than after the colonization. In the post-World War II Baltic region, socio-economic changes led more stringent air quality standards and bans on fires that eliminated traditional burning practices. In the mid-19th century, explorers from the HMS Beagle observed Australian Aborigines using fire for ground clearing, hunting, and regeneration of plant food in a method later named fire-stick farming. Such careful use of fire has been employed for centuries in the lands protected by Kakadu National Park to encourage biodiversity.
Wildfires typically occurred during periods of increased temperature and drought. An increase in fire-related debris flow in alluvial fans of northeastern Yellowstone National Park was linked to the period between AD 1050 and 1200, coinciding with the Medieval Warm Period. However, human influence caused an increase in fire frequency. Dendrochronological fire scar data and charcoal layer data in Finland suggests that, while many fires occurred during severe drought conditions, an increase in the number of fires during 850 BC and 1660 AD can be attributed to human influence. Charcoal evidence from the Americas suggested a general decrease in wildfires between 1 AD and 1750 compared to previous years. However, a period of increased fire frequency between 1750 and 1870 was suggested by charcoal data from North America and Asia, attributed to human population growth and influences such as land clearing practices. This period was followed by an overall decrease in burning in the 20th century, linked to the expansion of agriculture, increased livestock grazing, and fire prevention efforts. A meta-analysis found that 17 times more land burned annually in California before 1800 compared to recent decades (1,800,000 hectares/year compared to 102,000 hectares/year).
According to a paper published in Science, the number of natural and human-caused fires decreased by 24.3% between 1998 and 2015. Researchers explain this a transition from nomadism to settled lifestyle and intensification of agriculture that lead to a drop in the use of fire for land clearing.
Wildfire prevention refers to the preemptive methods aimed at reducing the risk of fires as well as lessening its severity and spread. Prevention techniques aim to manage air quality, maintain ecological balances, protect resources, and to affect future fires. North American firefighting policies permit naturally caused fires to burn to maintain their ecological role, so long as the risks of escape into high-value areas are mitigated. However, prevention policies must consider the role that humans play in wildfires, since, for example, 95% of forest fires in Europe are related to human involvement. Sources of human-caused fire may include arson, accidental ignition, or the uncontrolled use of fire in land-clearing and agriculture such as the slash-and-burn farming in Southeast Asia.
In 1937, U.S. President Franklin D. Roosevelt initiated a nationwide fire prevention campaign, highlighting the role of human carelessness in forest fires. Later posters of the program featured Uncle Sam, leaders of the Axis powers of World War II, characters from the Disney movie Bambi, and the official mascot of the U.S. Forest Service, Smokey Bear. Reducing human-caused ignitions may be the most effective means of reducing unwanted wildfire. Alteration of fuels is commonly undertaken when attempting to affect future fire risk and behavior. Wildfire prevention programs around the world may employ techniques such as wildland fire use and prescribed or controlled burns. Wildland fire use refers to any fire of natural causes that is monitored but allowed to burn. Controlled burns are fires ignited by government agencies under less dangerous weather conditions.
Vegetation may be burned periodically to maintain high species diversity and frequent burning of surface fuels limits fuel accumulation. Wildland fire use is the cheapest and most ecologically appropriate policy for many forests. Fuels may also be removed by logging, but fuels treatments and thinning have no effect on severe fire behavior Wildfire models are often used to predict and compare the benefits of different fuel treatments on future wildfire spread, but their accuracy is low.
Wildfire itself is reportedly "the most effective treatment for reducing a fire's rate of spread, fireline intensity, flame length, and heat per unit of area" according to Jan van Wagtendonk, a biologist at the Yellowstone Field Station.
Building codes in fire-prone areas typically require that structures be built of flame-resistant materials and a defensible space be maintained by clearing flammable materials within a prescribed distance from the structure. Communities in the Philippines also maintain fire lines 5 to 10 meters (16 to 33 ft) wide between the forest and their village, and patrol these lines during summer months or seasons of dry weather. Continued residential development in fire-prone areas and rebuilding structures destroyed by fires has been met with criticism. The ecological benefits of fire are often overridden by the economic and safety benefits of protecting structures and human life.
Fast and effective detection is a key factor in wildfire fighting. Early detection efforts were focused on early response, accurate results in both daytime and nighttime, and the ability to prioritize fire danger. Fire lookout towers were used in the United States in the early 20th century and fires were reported using telephones, carrier pigeons, and heliographs. Aerial and land photography using instant cameras were used in the 1950s until infrared scanning was developed for fire detection in the 1960s. However, information analysis and delivery was often delayed by limitations in communication technology. Early satellite-derived fire analyses were hand-drawn on maps at a remote site and sent via overnight mail to the fire manager. During the Yellowstone fires of 1988, a data station was established in West Yellowstone, permitting the delivery of satellite-based fire information in approximately four hours.
Currently, public hotlines, fire lookouts in towers, and ground and aerial patrols can be used as a means of early detection of forest fires. However, accurate human observation may be limited by operator fatigue, time of day, time of year, and geographic location. Electronic systems have gained popularity in recent years as a possible resolution to human operator error. A government report on a recent trial of three automated camera fire detection systems in Australia did, however, conclude "...detection by the camera systems was slower and less reliable than by a trained human observer". These systems may be semi- or fully automated and employ systems based on the risk area and degree of human presence, as suggested by GIS data analyses. An integrated approach of multiple systems can be used to merge satellite data, aerial imagery, and personnel position via Global Positioning System (GPS) into a collective whole for near-realtime use by wireless Incident Command Centers.
A small, high risk area that features thick vegetation, a strong human presence, or is close to a critical urban area can be monitored using a local sensor network. Detection systems may include wireless sensor networks that act as automated weather systems: detecting temperature, humidity, and smoke. These may be battery-powered, solar-powered, or tree-rechargeable: able to recharge their battery systems using the small electrical currents in plant material. Larger, medium-risk areas can be monitored by scanning towers that incorporate fixed cameras and sensors to detect smoke or additional factors such as the infrared signature of carbon dioxide produced by fires. Additional capabilities such as night vision, brightness detection, and color change detection may also be incorporated into sensor arrays.
Satellite and aerial monitoring through the use of planes, helicopter, or UAVs can provide a wider view and may be sufficient to monitor very large, low risk areas. These more sophisticated systems employ GPS and aircraft-mounted infrared or high-resolution visible cameras to identify and target wildfires. Satellite-mounted sensors such as Envisat's Advanced Along Track Scanning Radiometer and European Remote-Sensing Satellite's Along-Track Scanning Radiometer can measure infrared radiation emitted by fires, identifying hot spots greater than 39 °C (102 °F). The National Oceanic and Atmospheric Administration's Hazard Mapping System combines remote-sensing data from satellite sources such as Geostationary Operational Environmental Satellite (GOES), Moderate-Resolution Imaging Spectroradiometer (MODIS), and Advanced Very High Resolution Radiometer (AVHRR) for detection of fire and smoke plume locations. However, satellite detection is prone to offset errors, anywhere from 2 to 3 kilometers (1 to 2 mi) for MODIS and AVHRR data and up to 12 kilometers (7.5 mi) for GOES data. Satellites in geostationary orbits may become disabled, and satellites in polar orbits are often limited by their short window of observation time. Cloud cover and image resolution and may also limit the effectiveness of satellite imagery.
in 2015 a new fire detection tool is in operation at the U.S. Department of Agriculture (USDA) Forest Service (USFS) which uses data from the Suomi National Polar-orbiting Partnership (NPP) satellite to detect smaller fires in more detail than previous space-based products. The high-resolution data is used with a computer model to predict how a fire will change direction based on weather and land conditions. The active fire detection product using data from Suomi NPP's Visible Infrared Imaging Radiometer Suite (VIIRS) increases the resolution of fire observations to 1,230 feet (375 meters). Previous NASA satellite data products available since the early 2000s observed fires at 3,280 foot (1 kilometer) resolution. The data is one of the intelligence tools used by the USFS and Department of Interior agencies across the United States to guide resource allocation and strategic fire management decisions. The enhanced VIIRS fire product enables detection every 12 hours or less of much smaller fires and provides more detail and consistent tracking of fire lines during long duration wildfires – capabilities critical for early warning systems and support of routine mapping of fire progression. Active fire locations are available to users within minutes from the satellite overpass through data processing facilities at the USFS Remote Sensing Applications Center, which uses technologies developed by the NASA Goddard Space Flight Center Direct Readout Laboratory in Greenbelt, Maryland. The model uses data on weather conditions and the land surrounding an active fire to predict 12–18 hours in advance whether a blaze will shift direction. The state of Colorado decided to incorporate the weather-fire model in its firefighting efforts beginning with the 2016 fire season.
In 2014, an international campaign was organized in South Africa's Kruger National Park to validate fire detection products including the new VIIRS active fire data. In advance of that campaign, the Meraka Institute of the Council for Scientific and Industrial Research in Pretoria, South Africa, an early adopter of the VIIRS 375m fire product, put it to use during several large wildfires in Kruger.
The demand for timely, high-quality fire information has increased in recent years. Wildfires in the United States burn an average of 7 million acres of land each year. For the last 10 years, the USFS and Department of Interior have spent a combined average of about $2–4 billion annually on wildfire suppression.
Wildfire suppression depends on the technologies available in the area in which the wildfire occurs. In less developed nations the techniques used can be as simple as throwing sand or beating the fire with sticks or palm fronds. In more advanced nations, the suppression methods vary due to increased technological capacity. Silver iodide can be used to encourage snow fall, while fire retardants and water can be dropped onto fires by unmanned aerial vehicles, planes, and helicopters. Complete fire suppression is no longer an expectation, but the majority of wildfires are often extinguished before they grow out of control. While more than 99% of the 10,000 new wildfires each year are contained, escaped wildfires under extreme weather conditions are difficult to suppress without a change in the weather. Wildfires in Canada and the US burn an average of 54,500 square kilometers (13,000,000 acres) per year.
Above all, fighting wildfires can become deadly. A wildfire's burning front may also change direction unexpectedly and jump across fire breaks. Intense heat and smoke can lead to disorientation and loss of appreciation of the direction of the fire, which can make fires particularly dangerous. For example, during the 1949 Mann Gulch fire in Montana, USA, thirteen smokejumpers died when they lost their communication links, became disoriented, and were overtaken by the fire. In the Australian February 2009 Victorian bushfires, at least 173 people died and over 2,029 homes and 3,500 structures were lost when they became engulfed by wildfire.
Costs of wildfire suppression
In California, the U.S. Forest Service spends about $200 million per year to suppress 98% of wildfires and up to $1 billion to suppress the other 2% of fires that escape initial attack and become large.
Wildland firefighting safety
Wildland fire fighters face several life-threatening hazards including heat stress, fatigue, smoke and dust, as well as the risk of other injuries such as burns, cuts and scrapes, animal bites, and even rhabdomyolysis.
Especially in hot weather condition, fires present the risk of heat stress, which can entail feeling heat, fatigue, weakness, vertigo, headache, or nausea. Heat stress can progress into heat strain, which entails physiological changes such as increased heart rate and core body temperature. This can lead to heat-related illnesses, such as heat rash, cramps, exhaustion or heat stroke. Various factors can contribute to the risks posed by heat stress, including strenuous work, personal risk factors such as age and fitness, dehydration, sleep deprivation, and burdensome personal protective equipment. Rest, cool water, and occasional breaks are crucial to mitigating the effects of heat stress.
Smoke, ash, and debris can also pose serious respiratory hazards to wildland fire fighters. The smoke and dust from wildfires can contain gases such as carbon monoxide, sulfur dioxide and formaldehyde, as well as particulates such as ash and silica. To reduce smoke exposure, wildfire fighting crews should, whenever possible, rotate firefighters through areas of heavy smoke, avoid downwind firefighting, use equipment rather than people in holding areas, and minimize mop-up. Camps and command posts should also be located upwind of wildfires. Protective clothing and equipment can also help minimize exposure to smoke and ash.
Firefighters are also at risk of cardiac events including strokes and heart attacks. Fire fighters should maintain good physical fitness. Fitness programs, medical screening and examination programs which include stress tests can minimize the risks of firefighting cardiac problems. Other injury hazards wildland fire fighters face include slips, trips and falls, burns, scrapes and cuts from tools and equipment, being struck by trees, vehicles, or other objects, plant hazards such as thorns and poison ivy, snake and animal bites, vehicle crashes, electrocution from power lines or lightning storms, and unstable building structures.
Fire retardants are used to help slow wildfires, coat fuels, and lessen oxygen availability as required by various firefighting situations. They are composed of nitrates, ammonia, phosphates and sulfates, as well as other chemicals and thickening agents. The choice of whether to apply retardant depends on the magnitude, location and intensity of the wildfire. Fire retardants are used to reach inaccessible geographical regions where ground firefighting crews are unable to reach a wildfire or in any occasion where human safety and structures are endangered. In certain instances, fire retardant may also be applied ahead of wildfires for protection of structures and vegetation as a precautionary fire defense measure.
The application of aerial fire retardants creates an atypical appearance on land and water surfaces and has the potential to change soil chemistry. Fire retardant can decrease the availability of plant nutrients in the soil by increasing the acidity of the soil. Fire retardant may also affect water quality through leaching, eutrophication, or misapplication. Fire retardant's effects on drinking water remain inconclusive. Dilution factors, including water body size, rainfall, and water flow rates lessen the concentration and potency of fire retardant. Wildfire debris (ash and sediment) clog rivers and reservoirs increasing the risk for floods and erosion that ultimately slow and/or damage water treatment systems. There is continued concern of fire retardant effects on land, water, wildlife habitats, and watershed quality, additional research is needed. However, on the positive side, fire retardant (specifically its nitrogen and phosphorus components) has been shown to have a fertilizing effect on nutrient-deprived soils and thus creates a temporary increase in vegetation.
Current USDA procedure maintains that the aerial application of fire retardant in the United States must clear waterways by a minimum of 300 feet in order to safeguard effects of retardant runoff. Aerial uses of fire retardant are required to avoid application near waterways and endangered species (plant and animal habitats). After any incident of fire retardant misapplication, the U.S. Forest Service requires reporting and assessment impacts be made in order to determine mitigation, remediation, and/or restrictions on future retardant uses in that area.
Wildfire modeling is concerned with numerical simulation of wildfires in order to comprehend and predict fire behavior. Wildfire modeling aims to aid wildfire suppression, increase the safety of firefighters and the public, and minimize damage. Using computational science, wildfire modeling involves the statistical analysis of past fire events to predict spotting risks and front behavior. Various wildfire propagation models have been proposed in the past, including simple ellipses and egg- and fan-shaped models. Early attempts to determine wildfire behavior assumed terrain and vegetation uniformity. However, the exact behavior of a wildfire's front is dependent on a variety of factors, including windspeed and slope steepness. Modern growth models utilize a combination of past ellipsoidal descriptions and Huygens' Principle to simulate fire growth as a continuously expanding polygon. Extreme value theory may also be used to predict the size of large wildfires. However, large fires that exceed suppression capabilities are often regarded as statistical outliers in standard analyses, even though fire policies are more influenced by large wildfires than by small fires.
Human risk and exposure
Wildfire risk is the chance that a wildfire will start in or reach a particular area and the potential loss of human values if it does. Risk is dependent on variable factors such as human activities, weather patterns, availability of wildfire fuels, and the availability or lack of resources to suppress a fire. Wildfires have continually been a threat to human populations. However, human induced geographical and climatic changes are exposing populations more frequently to wildfires and increasing wildfire risk. It is speculated that the increase in wildfires arises from a century of wildfire suppression coupled with the rapid expansion of human developments into fire-prone wildlands. Wildfires are naturally occurring events that aid in promoting forest health. Global warming and climate changes are causing an increase in temperatures and more droughts nationwide which contributes to an increase in wildfire risk.
The most noticeable adverse effect of wildfires is the destruction of property. However, the release of hazardous chemicals from the burning of wildland fuels also significantly impacts health in humans.
Wildfire smoke is composed primarily of carbon dioxide and water vapor. Other common smoke components present in lower concentrations are carbon monoxide, formaldehyde, acrolein, polyaromatic hydrocarbons, and benzene. Small particulates suspended in air which come in solid form or in liquid droplets are also present in smoke. 80 -90% of wildfire smoke, by mass, is within the fine particle size class of 2.5 micrometers in diameter or smaller.
Despite carbon dioxide's high concentration in smoke, it poses a low health risk due to its low toxicity. Rather, carbon monoxide and fine particulate matter, particularly 2.5 µm in diameter and smaller, have been identified as the major health threats. Other chemicals are considered to be significant hazards but are found in concentrations that are too low to cause detectable health effects.
The degree of wildfire smoke exposure to an individual is dependent on the length, severity, duration, and proximity of the fire. People are exposed directly to smoke via the respiratory tract though inhalation of air pollutants. Indirectly, communities are exposed to wildfire debris that can contaminate soil and water supplies.
The U.S. Environmental Protection Agency (EPA) developed the Air Quality Index (AQI), a public resource that provides national air quality standard concentrations for common air pollutants. The public can use this index as a tool to determine their exposure to hazardous air pollutants based on visibility range.
Groups at risk
Firefighters are at the greatest risk for acute and chronic health effects resulting from wildfire smoke exposure. Due to firefighters' occupational duties, they are frequently exposed to hazardous chemicals at a close proximity for longer periods of time. A case study on the exposure of wildfire smoke among wildland firefighters shows that firefighters are exposed to significant levels of carbon monoxide and respiratory irritants above OSHA-permissible exposure limits (PEL) and ACGIH threshold limit values (TLV). 5–10% are overexposed. The study obtained exposure concentrations for one wildland firefighter over a 10-hour shift spent holding down a fireline. The firefighter was exposed to a wide range of carbon monoxide and respiratory irritant (combination of particulate matter 3.5 µm and smaller, acrolein, and formaldehype) levels. Carbon monoxide levels reached up to 160ppm and the TLV irritant index value reached a high of 10. In contrast, the OSHA PEL for carbon monoxide is 30ppm and for the TLV respiratory irritant index, the calculated threshold limit value is 1; any value above 1 exceeds exposure limits.
Between 2001 and 2012, over 200 fatalities occurred among wildland firefighters. In addition to heat and chemical hazards, firefighters are also at risk for electrocution from power lines; injuries from equipment; slips, trips, and falls; injuries from vehicle rollovers; heat-related illness; insect bites and stings; stress; and rhabdomyolysis.
Residents in communities surrounding wildfires are exposed to lower concentrations of chemicals, but they are at a greater risk for indirect exposure through water or soil contamination. Exposure to residents is greatly dependent on individual susceptibility. Vulnerable persons such as children (ages 0–4), the elderly (ages 65 and older), smokers, and pregnant women are at an increased risk due to their already compromised body systems, even when the exposures are present at low chemical concentrations and for relatively short exposure periods.
Additionally, there is evidence of an increase in material stress, as documented by researchers M.H. O'Donnell and A.M. Behie, thus affecting birth outcomes. In Australia, studies show that male infants born with drastically higher average birth weights were born in mostly severely fire-affected areas. This is attributed to the fact that maternal signals directly affect fetal growth patterns.
Inhalation of smoke from a wildfire can be a health hazard. Wildfire smoke is composed of carbon dioxide, water vapor, particulate matter, organic chemicals, nitrogen oxides and other compounds. The principal health concern is the inhalation of particulate matter and carbon monoxide.
Particulate matter (PM) is a type of air pollution made up of particles of dust and liquid droplets. They are characterized into two categories based on the diameter of the particle. Coarse particles are between 2.5 micrometers and 10 micrometers and fine particles measure 2.5 micrometers and less. Both sizes can be inhaled. Coarse particles are filtered by the upper airways and can cause eye and sinus irritation as well as sore throat and coughing. The fine particles are more problematic because, when inhaled, they can be deposited deep into the lungs, where they are absorbed into the bloodstream. This is particularly hazardous to the very young, elderly and those with chronic conditions such as asthma, chronic obstructive pulmonary disease (COPD), cystic fibrosis and cardiovascular conditions. The illnesses most commonly with exposure to fine particle from wildfire smoke are bronchitis, exacerbation of asthma or COPD, and pneumonia. Symptoms of these complications include wheezing and shortness of breath and cardiovascular symptoms include chest pain, rapid heart rate and fatigue.
Carbon monoxide (CO) is a colorless, odorless gas that can be found at the highest concentration at close proximity to a smoldering fire. For this reason, carbon monoxide inhalation is a serious threat to the health of wildfire firefighters. CO in smoke can be inhaled into the lungs where it is absorbed into the bloodstream and reduces oxygen delivery to the body's vital organs. At high concentrations, it can cause headache, weakness, dizziness, confusion, nausea, disorientation, visual impairment, coma and even death. However, even at lower concentrations, such as those found at wildfires, individuals with cardiovascular disease may experience chest pain and cardiac arrhythmia. A recent study tracking the number and cause of wildfire firefighter deaths from 1990–2006 found that 21.9% of the deaths occurred from heart attacks.
Another important and somewhat less obvious health effect of wildfires is psychiatric diseases and disorders. Both adults and children from countries ranging from the United States and Canada to Greece and Australia who were directly and indirectly affected by wildfires were found by researchers to demonstrate several different mental conditions linked to their experience with the wildfires. These include post-traumatic stress disorder (PTSD), depression, anxiety, and phobias.
In a new twist to wildfire health effects, former uranium mining sites were burned over in the summer of 2012 near North Fork, Idaho. This prompted concern from area residents and Idaho State Department of Environmental Quality officials over the potential spread of radiation in the resultant smoke, since those sites had never been completely cleaned up from radioactive remains.
The EPA has defined acceptable concentrations of particulate matter in the air, through the National Ambient Air Quality Standards and monitoring of ambient air quality has been mandated. Due to these monitoring programs and the incidence of several large wildfires near populated areas, epidemiological studies have been conducted and demonstrate an association between human health effects and an increase in fine particulate matter due to wildfire smoke.
An increase in PM emitted from the Hayman fire in Colorado in June 2002, was associated with an increase in respiratory symptoms in patients with COPD. Looking at the wildfires in Southern California in October 2003 in a similar manner, investigators have shown an increase in hospital admissions due to asthma during peak concentrations of PM. Children participating in the Children's Health Study were also found to have an increase in eye and respiratory symptoms, medication use and physician visits. Recently, it was demonstrated that mothers who were pregnant during the fires gave birth to babies with a slightly reduced average birth weight compared to those who were not exposed to wildfire during birth. Suggesting that pregnant women may also be at greater risk to adverse effects from wildfire. Worldwide it is estimated that 339,000 people die due to the effects of wildfire smoke each year.
- Peshtigo Fire, 1871; most loss of life in a US wildfire.
- Great Fire of 1910 in the US; shaped 20th-century wildfire policy
- Landes Forest 1949 wildfire in South West France; 50,000 hectares (500 km2; 190 sq mi) of forest land were burnt and 82 people were killed.
- 1988 Yellowstone wildfires
- 2003 Portuguese wildfires
- 2009 SE Australia bushfires
- 2010 Bolivian forest fires
- 2010 Russian wildfires
- 2011 Texas wildfires
- 2013 Beaver Creek Fire in Idaho.
- 2015 Southeast Asian haze caused by a wildfire in Riau
- 2016 Fort McMurray wildfire in Canada
- 2016 Nevada wildfire
- 2017 Portugal wildfires
- Bushfires in Australia
- Dry thunderstorm
- Fire-adapted communities
- Fire ecology
- Floods and landslides after wildfires
- Forest fire weather index
- Haines Index
- Keetch-Byram Drought Index
- National Fire Danger Rating System
- Remote Automated Weather Station
- Smoke inhalation
- Weather forecasting
- Wildfires in the United States
- Women in firefighting
- Cambridge Advanced Learner's Dictionary (Third ed.). Cambridge University Press. 2008. ISBN 978-0-521-85804-5.
- "BBC Earth – Forest fire videos – See how fire started on Earth". Retrieved 2016-02-13.
- Scott, Andrew C.; Glasspool, Ian J. (2006-07-18). "The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration". Proceedings of the National Academy of Sciences. 103 (29): 10861–10865. Bibcode:2006PNAS..10310861S. ISSN 0027-8424. PMC . PMID 16832054. doi:10.1073/pnas.0604090103.
- Bowman, David M. J. S.; Balch, Jennifer K.; Artaxo, Paulo; Bond, William J.; Carlson, Jean M.; Cochrane, Mark A.; D’Antonio, Carla M.; DeFries, Ruth S.; Doyle, John C. (2009-04-24). "Fire in the Earth System". Science. 324 (5926): 481–484. Bibcode:2009Sci...324..481B. ISSN 0036-8075. PMID 19390038. doi:10.1126/science.1163886.
- Flannigan, M.D.; B.D. Amiro; K.A. Logan; B.J. Stocks & B.M. Wotton (2005). "Forest Fires and Climate Change in the 21st century" (PDF). Mitigation and Adaptation Strategies for Global Change. 11 (4): 847–859. doi:10.1007/s11027-005-9020-7. Retrieved 26 June 2009.
- "The Ecological Importance of Mixed-Severity Fires – ScienceDirect". www.sciencedirect.com. Retrieved 2016-08-22.
- Hutto, Richard L. (2008-12-01). "The Ecological Importance of Severe Wildfires: Some Like It Hot". Ecological Applications. 18 (8): 1827–1834. ISSN 1939-5582. doi:10.1890/08-0895.1.
- Stephen J. Pyne. "How Plants Use Fire (And Are Used By It)". NOVA online. Retrieved 30 June 2009.
- Graham, et al., 12, 36
- National Wildfire Coordinating Group Communicator's Guide For Wildland Fire Management, 4–6.
- "National Wildfire Coordinating Group Fireline Handbook, Appendix B: Fire Behavior" (PDF). National Wildfire Coordinating Group. April 2006. Retrieved 11 December 2008.
- Westerling, A. L.; Hidalgo, H. G.; Cayan, D. R.; Swetnam, T. W. (2006-08-18). "Warming and Earlier Spring Increase Western U.S. Forest Wildfire Activity". Science. 313 (5789): 940–943. Bibcode:2006Sci...313..940W. ISSN 0036-8075. PMID 16825536. doi:10.1126/science.1128834.
- "International Experts Study Ways to Fight Wildfires". Voice of America (VOA) News. 24 June 2009. Retrieved 9 July 2009.
- Interagency Strategy for the Implementation of the Federal Wildland Fire Policy, entire text
- National Wildfire Coordinating Group Communicator's Guide For Wildland Fire Management, entire text
- Fire. The Australian Experience, 5–6.
- Graham, et al., 15.
- Noss, Reed F.; Franklin, Jerry F.; Baker, William L.; Schoennagel, Tania; Moyle, Peter B. (2006-11-01). "Managing fire-prone forests in the western United States". Frontiers in Ecology and the Environment. 4 (9): 481–487. ISSN 1540-9309. doi:10.1890/1540-9295(2006)4[481:MFFITW]2.0.CO;2.
- Lydersen, Jamie M.; North, Malcolm P.; Collins, Brandon M. (2014-09-15). "Severity of an uncharacteristically large wildfire, the Rim Fire, in forests with relatively restored frequent fire regimes". Forest Ecology and Management. 328: 326–334. doi:10.1016/j.foreco.2014.06.005.
- van Wagtendonk (1996), 1164
- "California's Fire Hazard Severity Zone Update and Building Standards Revision" (PDF). CAL FIRE. May 2007. Retrieved 18 December 2008.
- "California Senate Bill No. 1595, Chapter 366" (PDF). State of California. 27 September 2008. Retrieved 18 December 2008.
- "Wildfire Prevention Strategies" (PDF). National Wildfire Coordinating Group. March 1998. p. 17. Retrieved 3 December 2008.
- Scott, A (2000). "The Pre-Quaternary history of fire". Palaeogeography, Palaeoclimatology, Palaeoecology. 164: 281–329. Bibcode:2000PPP...164..281S. doi:10.1016/S0031-0182(00)00192-9.
- Pyne, Stephen J.; Andrews, Patricia L.; Laven, Richard D. (1996). Introduction to wildland fire (2nd ed.). John Wiley and Sons. p. 65. ISBN 978-0-471-54913-0. Retrieved 26 January 2010.
- "News 8 Investigation: SDG&E Could Be Liable For Power Line Wildfires". UCAN News. 5 November 2007. Retrieved 20 July 2009.
- Finney, Mark A.; Maynard, Trevor B.; McAllister, Sara S.; Grob, Ian J. (2013). A Study of Ignition by Rifle Bullets. Fort Collins, CO: United States Forest Service. Retrieved 15 June 2014.
- The Associated Press (16 November 2006). "Orangutans in losing battle with slash-and-burn Indonesian farmers". TheStar online. Retrieved 1 December 2008.
- Karki, 4.
- Krock, Lexi (June 2002). "The World on Fire". NOVA online – Public Broadcasting System (PBS). Retrieved 13 July 2009.
- Krajick, Kevin (May 2005). "Fire in the hole". Smithsonian Magazine. Retrieved 30 July 2009.
- Graham, et al., iv.
- Graham, et al., 9, 13
- Rincon, Paul (9 March 2005). "Asian peat fires add to warming". British Broadcasting Corporation (BBC) News. Retrieved 9 December 2008.
- Graham, et al ., iv, 10, 14
- "Global Fire Initiative: Fire and Invasives". The Nature Conservancy. Retrieved 3 December 2008.
- Graham, et al., iv, 8, 11, 15.
- Butler, Rhett (19 June 2008). "Global Commodities Boom Fuels New Assault on Amazon". Yale School of Forestry & Environmental Studies. Retrieved 9 July 2009.
- "The Science of Wildland fire". National Interagency Fire Center. Retrieved 21 November 2008.
- Graham, et al., 12.
- National Wildfire Coordinating Group Communicator's Guide For Wildland Fire Management, 3.
- "Ashes cover areas hit by Southern Calif. fires". MSNBC. Associated Press. 15 November 2008. Retrieved 4 December 2008.
- "Influence of Forest Structure on Wildfire Behavior and the Severity of Its Effects" (PDF). US Forest Service. November 2003. Retrieved 19 November 2008.
- "Prepare for a Wildfire". Federal Emergency Management Agency (FEMA). Retrieved 1 December 2008.
- Glossary of Wildland Fire Terminology, 74.
- de Sousa Costa and Sandberg, 229–230.
- "Archimedes Death Ray: Idea Feasibility Testing". Massachusetts Institute of Technology (MIT). October 2005. Retrieved 1 February 2009.
- "Satellites are tracing Europe's forest fire scars". European Space Agency. 27 July 2004. Retrieved 12 January 2009.
- Graham, et al., 10–11.
- "Protecting Your Home From Wildfire Damage" (PDF). Florida Alliance for Safe Homes (FLASH). p. 5. Retrieved 3 March 2010.
- Billing, 5–6
- Graham, et al., 12
- Shea, Neil (July 2008). "Under Fire". National Geographic. Retrieved 8 December 2008.
- Graham, et al., 16.
- Graham, et al., 9, 16.
- Volume 1: The Kilmore East Fire. 2009 Victorian Bushfires Royal Commission. Victorian Bushfires Royal Commission, Australia. July 2010. ISBN 978-0-9807408-2-0. Retrieved 26 October 2013.
- National Wildfire Coordinating Group Communicator's Guide For Wildland Fire Management, 4.
- Graham, et al., 16–17.
- Olson, et al., 2
- "The New Generation Fire Shelter" (PDF). National Wildfire Coordinating Group. March 2003. p. 19. Retrieved 16 January 2009.
- Glossary of Wildland Fire Terminology, 69.
- "Chronological List of U.S. Billion Dollar Events". National Oceanic and Atmospheric Administration (NOAA) Satellite and Information Service. Retrieved 4 February 2009.
- McKenzie, et al., 893
- Graham, et al., 2
- Westerling, Al; Hidalgo, Hg; Cayan, Dr; Swetnam, Tw (August 2006). "Warming and earlier spring increase western U.S. Forest wildfire activity". Science. 313 (5789): 940–3. Bibcode:2006Sci...313..940W. ISSN 0036-8075. PMID 16825536. doi:10.1126/science.1128834.
- Bill Gabbert (November 9, 2015). "Was the 2014 wildfire season in California affected by climate change?". Wildfire Today. Retrieved May 17, 2016.
- Yoon; et al. (2015). "Extreme Fire Season in California: A Glimpse Into the Future?". Bulletin of the American Meteorological Society. 96 (11): S5–S9. Bibcode:2015BAMS...96S...5Y. doi:10.1175/BAMS-D-15-00114.1.
- Pierce, Jennifer L.; Meyer, Grant A.; Timothy Jull, A. J. (2004-11-04). "Fire-induced erosion and millennial-scale climate change in northern ponderosa pine forests". Nature. 432 (7013): 87–90. Bibcode:2004Natur.432...87P. ISSN 0028-0836. PMID 15525985. doi:10.1038/nature03058.
- de Souza Costa and Sandberg, 228
- National Wildfire Coordinating Group Communicator's Guide For Wildland Fire Management, 5.
- San-Miguel-Ayanz, et al., 364.
- Glossary of Wildland Fire Terminology, 73.
- Donato, Daniel C.; Fontaine, Joseph B.; Robinson, W. Douglas; Kauffman, J. Boone; Law, Beverly E. (2009-01-01). "Vegetation response to a short interval between high-severity wildfires in a mixed-evergreen forest". Journal of Ecology. 97 (1): 142–154. ISSN 1365-2745. doi:10.1111/j.1365-2745.2008.01456.x.
- Interagency Strategy for the Implementation of the Federal Wildland Fire Policy, 3, 37.
- Graham, et al., 3.
- Keeley, J.E. (1995). "Future of California floristics and systematics: wildfire threats to the California flora" (PDF). Madrono. US Geological Survey. 42: 175–179. Retrieved 26 June 2009.
- Zedler, P.H. (1995). "Fire frequency in southern California shrublands: biological effects and management options". In Keeley, J.E.; Scott, T. Brushfires in California wildlands: ecology and resource management. Fairfield, WA: International Association of Wildland Fire. pp. 101–112.
- van Wagtendonk (2007), 14.
- Nepstad, 4, 8–11
- Lindsey, Rebecca (5 March 2008). "Amazon fires on the rise". Earth Observatory (NASA). Retrieved 9 July 2009.
- Nepstad, 4
- "Bushfire and Catchments: Effects of Fire on Soils and Erosion". eWater Cooperative Research Center's. Retrieved 8 January 2009.
- Refern, Neil; Vyner, Blaise. "Fylingdales Moor a lost landscape rises from the ashes". Current Archaeology. Current Publishing. XIX (226): 20–27. ISSN 0011-3212.
- Running, S.W. (2008). "Ecosystem Disturbance, Carbon and Climate". Science. 321 (5889): 652–653. PMID 18669853. doi:10.1126/science.1159607.
- Higuera, Philip E.; Chipman, Melissa L.; Barnes, Jennifer L.; Urban, Michael A.; Hu, Feng Sheng (2011). "Variability of tundra fire regimes in Arctic Alaska: Millennial-scale patterns and ecological implications". Ecological Applications. 21 (8): 3211–3226. doi:10.1890/11-0387.1.
- Santos, Robert L. (1997). "Section Three: Problems, Cares, Economics, and Species". The Eucalyptus of California. California State University. Retrieved 26 June 2009.
- Fire. The Australian Experience, 5.
- Keeley, J.E. & C.J. Fotheringham (1997). "Trace gas emission in smoke-induced germination" (PDF). Science. 276: 1248–1250. doi:10.1126/science.276.5316.1248. Retrieved 26 June 2009.
- Flematti GR; Ghisalberti EL; Dixon KW; Trengove RD (2004). "A compound from smoke that promotes seed germination". Science. 305 (5686): 977. PMID 15247439. doi:10.1126/science.1099944.
- Karki, 3.
- Pyne, Stephen. "How Plants Use Fire (And How They Are Used By It)". Nova. Retrieved 26 September 2013.
- "Giant Sequoias and Fire". US National Park Service. Retrieved 30 June 2009.
- "Fire Management Assessment of the Caribbean Pine (Pinus caribea) Forest Ecosystems on Andros and Abaco Islands, Bahamas" (PDF). TNC Global Fire Initiative. The Nature Conservancy. September 2004. Retrieved 27 August 2009.
- Wang, P.K. (2003). The physical mechanism of injecting biomass burning materials into the stratosphere during fire-induced thunderstorms. San Francisco, California: American Geophysical Union fall meeting.
- Fromm, M.; Stocks, B.; Servranckx, R.; Lindsey, D. Smoke in the Stratosphere: What Wildfires have Taught Us About Nuclear Winter; abstract #U14A-04. American Geophysical Union, Fall Meeting 2006. Bibcode:2006AGUFM.U14A..04F. Retrieved 4 February 2009.
- Graham, et al., 17
- John R. Scala; et al. "Meteorological Conditions Associated with the Rapid Transport of Canadian Wildfire Products into the Northeast during 5–8 July 2002" (PDF). American Meteorological Society. Retrieved 4 February 2009.
- Breyfogle, Steve; Sue A., Ferguson (December 1996). "User Assessment of Smoke-Dispersion Models for Wildland Biomass Burning" (PDF). US Forest Service. Retrieved 6 February 2009.
- Bravo, A.H.; E. R. Sosa; A. P. Sánchez; P. M. Jaimes & R. M. I. Saavedra (2002). "Impact of wildfires on the air quality of Mexico City, 1992–1999". Environmental Pollution. 117 (2): 243–253. PMID 11924549. doi:10.1016/S0269-7491(01)00277-9.
- Dore, S.; Kolb, T. E.; Montes-Helu, M.; Eckert, S. E.; Sullivan, B. W.; Hungate, B. A.; Kaye, J. P.; Hart, S. C.; Koch, G. W. (2010-04-01). "Carbon and water fluxes from ponderosa pine forests disturbed by wildfire and thinning". Ecological Applications. 20 (3): 663–683. ISSN 1939-5582. doi:10.1890/09-0934.1.
- Douglass, R. (2008). "Quantification of the health impacts associated with fine particulate matter due to wildfires. MS Thesis" (PDF). Nicholas School of the Environment and Earth Sciences of Duke University.
- National Center for Atmospheric Research (13 October 2008). "Wildfires Cause Ozone Pollution to Violate Health Standards". Geophysical Research Letters. Retrieved 4 February 2009.
- Page, Susan E.; Florian Siegert; John O. Rieley; Hans-Dieter V. Boehm; Adi Jaya & Suwido Limin (11 July 2002). "The amount of carbon released from peat and forest fires in Indonesia during 1997". Nature. 420 (6911): 61–65. Bibcode:2002Natur.420...61P. PMID 12422213. doi:10.1038/nature01131.
- Tacconi, Luca (February 2003). "Fires in Indonesia: Causes, Costs, and Policy Implications (CIFOR Occasional Paper No. 38)" (PDF). Bogor, Indonesia: Center for International Forestry Research. ISSN 0854-9818. Retrieved 6 February 2009.
- Baumgardner, D.; et al. (2003). "Warming of the Arctic lower stratosphere by light absorbing particles". American Geophysical Union fall meeting. San Francisco, California.
- Glasspool Ij, E. D.; Edwards, D.; Axe, L. (2004). "Charcoal in the Silurian as evidence for the earliest wildfire". Geology. 32 (5): 381–383. Bibcode:2004Geo....32..381G. doi:10.1130/G20363.1.
- Edwards, D.; Axe, L. (April 2004). "Anatomical Evidence in the Detection of the Earliest Wildfires". PALAIOS. 19 (2): 113–128. ISSN 0883-1351. doi:10.1669/0883-1351(2004)019<0113:AEITDO>2.0.CO;2.
- Scott, C.; Glasspool, J. (Jul 2006). "The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration" (Free full text). Proceedings of the National Academy of Sciences of the United States of America. 103 (29): 10861–10865. Bibcode:2006PNAS..10310861S. ISSN 0027-8424. PMC . PMID 16832054. doi:10.1073/pnas.0604090103.
- Pausas and Keeley, 594
- Historically, the Cenozoic has been divided up into the Quaternary and Tertiary sub-eras, as well as the Neogene and Paleogene periods. The 2009 version of the ICS time chart recognizes a slightly extended Quaternary as well as the Paleogene and a truncated Neogene, the Tertiary having been demoted to informal status.
- Pausas and Keeley, 595
- Pausas and Keeley, 596
- "Redwood Trees".
- Pausas and Keeley, 597
- Rackham, Oliver (November–December 2003). "Fire in the European Mediterranean: History". AridLands Newsletter. University of Arizona College of Agriculture & Life Sciences. 54. Retrieved 17 July 2009.
- Rackham, 229–230
- Goldammer, Johann G. (5–9 May 1998). "History of Fire in Land-Use Systems of the Baltic Region: Implications on the Use of Prescribed Fire in Forestry, Nature Conservation and Landscape Management". First Baltic Conference on Forest Fires. Radom-Katowice, Poland: Global Fire Monitoring Center (GFMC).
- * "Wildland fire – An American legacy|" (PDF). Fire Management Today. USDA Forest Service. 60 (3): 4, 5, 9, 11. Summer 2000. Retrieved 31 July 2009.
- Fire. The Australian Experience, 7.
- Karki, 27.
- Meyer, G.A.; Wells, S.G.; Jull, A.J.T. (1995). "Fire and alluvial chronology in Yellowstone National Park: Climatic and intrinsic controls on Holocene geomorphic processes". GSA Bulletin. 107 (10): 1211–1230. Bibcode:1995GSAB..107.1211M. doi:10.1130/0016-7606(1995)107<1211:FAACIY>2.3.CO;2.
- Pitkänen, et al., 15–16 and 27–30
- J. R. Marlon; P. J. Bartlein; C. Carcaillet; D. G. Gavin; S. P. Harrison; P. E. Higuera; F. Joos; M. J. Power; I. C. Prentice (2008). "Climate and human influences on global biomass burning over the past two millennia". Nature Geoscience. 1 (10): 697–702. Bibcode:2008NatGe...1..697M. doi:10.1038/ngeo313. University of Oregon Summary, accessed 2 February 2010 Archived 27 September 2008 at the Wayback Machine.
- Stephens, Scott L.; Martin, Robert E.; Clinton, Nicholas E. (2007). "Prehistoric fire area and emissions from California's forests, woodlands, shrublands, and grasslands". Forest Ecology and Management. 251: 205–216. doi:10.1016/j.foreco.2007.06.005. Retrieved 4 May 2015.
- "Researchers Detect a Global Drop in Fires". NASA Earth Observatory. June 30, 2017. Retrieved July 4, 2017.
- Andela, N.; Morton, D.C.; et al. (June 30, 2017). "A human-driven decline in global burned area". Science. Bibcode:2017Sci...356.1356A. doi:10.1126/science.aal4108. Retrieved July 4, 2017.
- Karki, 6.
- van Wagtendonk (1996), 1156.
- Interagency Strategy for the Implementation of the Federal Wildland Fire Policy, 42.
- San-Miguel-Ayanz, et al., 361.
- Karki, 7, 11–19.
- "Smokey's Journey". Smokeybear.com. Retrieved 26 January 2010.
- "Backburn". MSN Encarta. Retrieved 9 July 2009.
- "UK: The Role of Fire in the Ecology of Heathland in Southern Britain". International Forest Fire News. 18: 80–81. January 1998.
- "Prescribed Fires". SmokeyBear.com. Retrieved 21 November 2008.
- Karki, 14.
- Manning, Richard (1 December 2007). "Our Trial by Fire". onearth.org. Retrieved 7 January 2009.
- "Extreme Events: Wild & Forest Fire". National Oceanic and Atmospheric Administration (NOAA). Retrieved 7 January 2009.
- San-Miguel-Ayanz, et al., 362.
- "An Integration of Remote Sensing, GIS, and Information Distribution for Wildfire Detection and Management" (PDF). Photogrammetric Engineering and Remote Sensing. Western Disaster Center. 64 (10): 977–985. October 1998. Retrieved 26 June 2009.
- "Radio communication keeps rangers in touch". Canadian Broadcasting Corporation (CBC) Digital Archives. 21 August 1957. Retrieved 6 February 2009.
- "Wildfire Detection and Control". Alabama Forestry Commission. Retrieved 12 January 2009.
- "Evaluation of three wildfire smoke detection systems", 4
- Fok, Chien-Liang; Roman, Gruia-Catalin & Lu, Chenyang (29 November 2004). "Mobile Agent Middleware for Sensor Networks: An Application Case Study". Washington University in St. Louis. Archived from the original (PDF) on 3 January 2007. Retrieved 15 January 2009.
- Chaczko, Z.; Ahmad, F. (July 2005). "Wireless Sensor Network Based System for Fire Endangered Areas". Third International Conference on Information Technology and Applications. 2 (4–7): 203–207. ISBN 0-7695-2316-1. doi:10.1109/ICITA.2005.313. Retrieved 15 January 2009.
- "Wireless Weather Sensor Networks for Fire Management". University of Montana – Missoula. Retrieved 19 January 2009.
- Solobera, Javier (9 April 2010). "Detecting Forest Fires using Wireless Sensor Networks with Waspmote". Libelium Comunicaciones Distribuidas S.L.
- Thomson, Elizabeth A. (23 September 2008). "Preventing forest fires with tree power". Massachusetts Institute of Technology (MIT) News. Retrieved 15 January 2009.
- "Evaluation of three wildfire smoke detection systems", 6
- "SDSU Tests New Wildfire-Detection Technology". San Diego, CA: San Diego State University. 23 June 2005. Archived from the original on 1 September 2006. Retrieved 12 January 2009.
- San-Miguel-Ayanz, et al., 366–369, 373–375.
- Rochester Institute of Technology (4 October 2003). "New Wildfire-detection Research Will Pinpoint Small Fires From 10,000 feet". ScienceDaily. Retrieved 12 January 2009.
- "Airborne campaign tests new instrumentation for wildfire detection". European Space Agency. 11 October 2006. Retrieved 12 January 2009.
- "World fire maps now available online in near-real time". European Space Agency. 24 May 2006. Retrieved 12 January 2009.
- "Earth from Space: California's 'Esperanza' fire". European Space Agency. 11 March 2006. Retrieved 12 January 2009.
- "Hazard Mapping System Fire and Smoke Product". National Oceanic and Atmospheric Administration (NOAA) Satellite and Information Service. Retrieved 15 January 2009.
- Ramachandran, Chandrasekar; Misra, Sudip & Obaidat, Mohammad S. (9 June 2008). "A probabilistic zonal approach for swarm-inspired wildfire detection using sensor networks". Int. J. Commun. Syst. 21 (10): 1047–1073. doi:10.1002/dac.937.
- Miller, Jerry; Borne, Kirk; Thomas, Brian; Huang Zhenping & Chi, Yuechen. "Automated Wildfire Detection Through Artificial Neural Networks" (PDF). NASA. Retrieved 15 January 2009.
- Zhang, Junguo; Li, Wenbin; Han, Ning & Kan, Jiangming (September 2008). "Forest fire detection system based on a ZigBee wireless sensor network" (PDF). Frontiers of Forestry in China. Higher Education Press, co-published with Springer-Verlag GmbH. 3 (3): 369–374. doi:10.1007/s11461-008-0054-3. Retrieved 26 June 2009.
- Karki, 16
- "China Makes Snow to Extinguish Forest Fire". FOXNews.com. 18 May 2006. Retrieved 10 July 2009.
- Ambrosia, Vincent G. (2003). "Disaster Management Applications – Fire" (PDF). NASA-Ames Research Center. Retrieved 21 July 2009.
- Plucinski, et al., 6
- "Fighting fire in the forest". CBS News. 17 June 2009. Archived from the original on 19 June 2009. Retrieved 26 June 2009.
- "Climate of 2008 Wildfire Season Summary". National Climatic Data Center. 11 December 2008. Retrieved 7 January 2009.
- Rothermel, Richard C. (May 1993). "General Technical Report INT-GTR-299 – Mann Gulch Fire: A Race That Couldn't Be Won". United States Department of Agriculture, Forest Service, Intermountain Research Station. Retrieved 26 June 2009.
- "Victorian Bushfires". Parliament of New South Wales. New South Wales Government. 13 March 2009. Retrieved 26 January 2010.
- "Region 5 – Land & Resource Management". www.fs.usda.gov. Retrieved 2016-08-22.
- Campbell, Corey; Liz Dalsey. "Wildland Fire Fighting Safety and Health". NIOSH Science Blog. National Institute of Occupational Safety and Health. Retrieved 6 August 2012.
- "Wildland Fire Fighting: Hot Tips to Stay Safe and Healthy" (PDF). National Institute for Occupational Safety and Health. Retrieved 21 March 2014.
- United States Department of Agriculture (USDA), Forest Service (2012). "Nation wide application of fire retardant on national forest system land: Record of Decision" (PDF).
- Kaladokidis, K.D. (2000). "Effects of wildfire suppression chemicals on people and the environment-a review" (PDF). Global Nest: the International Journal. 2 (2): 129–137.
- Magill, B. "Officials: Fire slurry poses little threat". Coloradoan.com.
- Boerner, C., Coday B., Noble, J., Roa, P., Roux V., Rucker K., & Wing, A. (2012). "Impact of wildfire in Clear Creek Watershed of the city of Golden's drinking water supply" (PDF). Colorado School of Mines.
- Eichenseher, T. (2012). "Colorado Wildfires Threaten Water Supplies". National Geographic Daily News.
- "Prometheus". Tymstra, C.; Bryce, R.W.; Wotton, B.M.; Armitage, O.B. 2009. Development and structure of Prometheus: the Canadian wildland fire growth simulation Model. Inf. Rep. NOR-X-417. Nat. Resour. Can., Can. For. Serv., North. For. Cent., Edmonton, AB. Retrieved 1 January 2009.
- "FARSITE". FireModels.org – Fire Behavior and Danger Software, Missoula Fire Sciences Laboratory. Archived from the original on 15 February 2008. Retrieved 1 July 2009.
- G.D. Richards, "An Elliptical Growth Model of Forest Fire Fronts and Its Numerical Solution", Int. J. Numer. Meth. Eng.. 30:1163–1179, 1990.
- Finney, 1–3.
- Alvarado, et al., 66–68
- "About Oregon wildfire risk". Oregon State University. Retrieved 9 July 2012.
- "The National Wildfire Mitigation Programs Database: State, County, and Local Efforts to Reduce Wildfire Risk" (PDF). US Forest Service. Retrieved 19 January 2014.
- "Extreme wildfires may be fueled by climate change". Michigan State University. 1 August 2013. Retrieved 1 August 2013.
- Rajamanickam Antonimuthu (August 5, 2014). White House explains the link between Climate Change and Wild Fires. YouTube.
- Office of Environmental Health Hazard Assessment (2008). "Wildfire smoke: A guide for public health officials" (PDF). Retrieved 9 July 2012.
- National Wildlife Coordination Group (2001). "Smoke management guide for prescribed and wildland fire" (PDF). Boise, ID: National Interagency Fire Center.
- U.S. Environmental Protection Agency (2009). "Air quality index: A guide to air quality and health" (PDF). Retrieved 9 July 2012.
- Booze, T.F.; Reinhardt, T.E.; Quiring, S.J.; Ottmar, R.D. (2004). "A screening-level assessment of the health risks of chronic smoke exposure for wildland firefighters". Journal Occupational and Environmental Hygiene. 1 (5): 296–305. doi:10.1080/15459620490442500.
- "CDC – NIOSH Publications and Products – Wildland Fire Fighting: Hot Tips to Stay Safe and Healthy (2013–158)". www.cdc.gov. Retrieved 2016-11-22.
- O'Donnell, M H; Behie, A M (November 15, 2015). "Effects of wildfire disaster exposure on male birth weight in an Australian population.". Evolution, medicine, and public health. England. 2015 (1): 344–354. ISSN 2050-6201. doi:10.1093/emph/eov027. Retrieved January 27, 2016.
- "1 Wildfire Smoke A Guide for Public Health Officials" (PDF). US Environmental Protection Agency. Retrieved 19 January 2014.
- Forsberg, Nicole T.; Longo, Bernadette M.; Baxter, Kimberly; Boutté, Marie (2012). "Wildfire Smoke Exposure: A Guide for the Nurse Practitioner". The Journal for Nurse Practitioners. 8 (2): 98–106. doi:10.1016/j.nurpra.2011.07.001.
- National Wildfire Coordinating Group (June 2007). "Wildland firefighter fatalities in the United States 1990–2006" (PDF). NWCG Safety and Health Working Team.
- Papanikolaou, V; Adamis, D; Mellon, RC; Prodromitis, G (2011). "Psychological distress following wildfires disaster in a rural part of Greece: A case-control population-based study". International journal of emergency mental health. 13 (1): 11–26. PMID 21957753.
- Mellon, Robert C.; Papanikolau, Vasiliki; Prodromitis, Gerasimos (2009). "Locus of control and psychopathology in relation to levels of trauma and loss: Self-reports of Peloponnesian wildfire survivors". Journal of Traumatic Stress. 22 (3): 189–96. PMID 19452533. doi:10.1002/jts.20411.
- Marshall, G. N.; Schell, T. L.; Elliott, M. N.; Rayburn, N. R.; Jaycox, L. H. (2007). "Psychiatric Disorders Among Adults Seeking Emergency Disaster Assistance After a Wildland-Urban Interface Fire". Psychiatric Services. 58 (4): 509–14. PMID 17412853. doi:10.1176/appi.ps.58.4.509.
- McDermott, BM; Lee, EM; Judd, M; Gibbon, P (2005). "Posttraumatic stress disorder and general psychopathology in children and adolescents following a wildfire disaster". Canadian Journal of Psychiatry. 50 (3): 137–43. PMID 15830823.
- Jones, RT; Ribbe, DP; Cunningham, PB; Weddle, JD; Langley, AK (2002). "Psychological impact of fire disaster on children and their parents". Behavior modification. 26 (2): 163–86. PMID 11961911. doi:10.1177/0145445502026002003.
- Leader, Jessica (21 September 2012). "Idaho Wildfire: Radiation Raises Slight Concern As Blaze Hits Former Uranium, Gold Mines". Huffington Post.
- "Particulate Matter (PM) Standards". EPA. April 24, 2016.
- Sutherland, E. Rand; Make, Barry J.; Vedal, Sverre; Zhang, Lening; Dutton, Steven J.; Murphy, James R.; Silkoff, Philip E. (2005). "Wildfire smoke and respiratory symptoms in patients with chronic obstructive pulmonary disease". Journal of Allergy and Clinical Immunology. 115 (2): 420–2. PMID 15696107. doi:10.1016/j.jaci.2004.11.030.
- Delfino, R J; Brummel, S; Wu, J; Stern, H; Ostro, B; Lipsett, M; Winer, A; Street, D H; Zhang, L; Tjoa, T; Gillen, D L (2009). "The relationship of respiratory and cardiovascular hospital admissions to the southern California wildfires of 2003". Occupational and Environmental Medicine. 66 (3): 189–97. PMID 19017694. doi:10.1136/oem.2008.041376.
- Kunzli, N.; Avol, E.; Wu, J.; Gauderman, W. J.; Rappaport, E.; Millstein, J.; Bennion, J.; McConnell, R.; Gilliland, F. D.; Berhane, Kiros; Lurmann, Fred; Winer, Arthur; Peters, John M. (2006). "Health Effects of the 2003 Southern California Wildfires on Children". American Journal of Respiratory and Critical Care Medicine. 174 (11): 1221–8. PMC . PMID 16946126. doi:10.1164/rccm.200604-519OC.
- Holstius, David M.; Reid, Colleen E.; Jesdale, Bill M.; Morello-Frosch, Rachel (2012). "Birth Weight Following Pregnancy During the 2003 Southern California Wildfires". Environmental Health Perspectives. 120 (9): 1340–5. PMC . PMID 22645279. doi:10.1289/ehp.1104515.
- Bowman, David M.J.S. et al. (May 2012). "Estimated global mortality attributable to smoke from landscape fires" (PDF). Environmental Health Perspectives. 120 (5): 695–701. PMC . PMID 22456494. doi:10.1289/ehp.1104422.
- Christophe Neff (13 July 2009). "The Fatal Forest Fire – remembering the "1949 Mega fire" in the "Forêt des Landes" (South West France)". Blogs le Monde on LeMonde.fr.
- Alvarado, Ernesto; Sandberg, David V; Pickford, Stewart G (Special Issue 1998). "Modeling Large Forest Fires as Extreme Events" (PDF). Northwest Science. 72: 66–75. Retrieved 6 February 2009.
- "Are Big Fires Inevitable? A Report on the National Bushfire Forum" (PDF). Parliament House, Canberra: Bushfire CRC. 27 February 2007. Retrieved 9 January 2009.
- "Automatic remote surveillance system for the prevention of forest fires" (PDF). Council of Australian Governments (COAG) Inquiry on Bushfire Mitigation and Management. Retrieved 10 July 2009.
- Billing, P (June 1983). "Otways Fire No. 22 – 1982/83 Aspects of fire behaviour. Research Report No.20" (PDF). Victoria Department of Sustainability and Environment. Retrieved 26 June 2009.
- de Souza Costa, Fernando; Sandberg, David (2004). "Mathematical model of a smoldering log" (PDF). Combustion and Flame (139): 227–238. Retrieved 6 February 2009.
- "Evaluation of three wildfire smoke detection systems" (PDF). Advantage. Forest Engineering Research Institute of Canada (FERIC). 5 (4). June 2004. Retrieved 13 January 2009.
- "Federal Fire and Aviation Operations Action Plan" (PDF). National Interagency Fire Center. 18 April 2005. Retrieved 26 June 2009.
- Finney, Mark A (March 1998). "FARSITE: Fire Area Simulator—Model Development and Evaluation" (PDF). US Forest Service. Retrieved 5 February 2009.
- "Fire. The Australian Experience" (PDF). NSW Rural Fire Service. Retrieved 4 February 2009.
- "Glossary of Wildland Fire Terminology" (PDF). National Wildfire Coordinating Group. November 2008. Retrieved 18 December 2008. (HTML version)
- Graham, Russell; McCaffrey, Sarah; Jain, Theresa B (April 2004). "Science Basis for Changing Forest Structure to Modify Wildfire Behavior and Severity" (2.79 MB PDF). General Technical Report RMRS-GTR-120. Fort Collins, CO: United States Department of Agriculture, Forest Service, Rocky Mountain Research Station: US Forest Service. Retrieved 6 February 2009.
- Grove, A T; Rackham, Oliver (2001). The Nature of Mediterranean Europe: An Ecological History. New Haven, CT: Yale University Press. ISBN 0300100558. Retrieved 17 July 2009.
- Karki, Sameer (2002). "Community Involvement in and Management of Forest Fires in South East Asia" (PDF). Project FireFight South East Asia. Archived from the original (PDF) on 30 July 2007. Retrieved 13 February 2009.
- Fire intensity, fire severity and burn severity: a brief review and suggested usage [PDF]. International Journal of Wildland Fire. 2009;18(1):116–26. doi:10.1071/WF07049.
- "Interagency Strategy for the Implementation of Federal Wildland Fire Management Policy" (PDF). National Interagency Fire Council. 20 June 2003. Archived from the original (PDF) on 14 May 2009. Retrieved 21 December 2008.
- Lyons, John W (6 January 1971). The Chemistry and Uses of Fire Retardants. United States of America: John Wiley & Sons, Inc. ISBN 0-471-55740-4.
- Martell, David L; Sun, Hua (2008). "The impact of fire suppression, vegetation, and weather on the area burned by lightning-caused forest fires in Ontario" (PDF). Canadian Journal of Forest Research. 38 (6): 1547–1563. doi:10.1139/X07-210. Retrieved 26 June 2009.
- Climatic change, wildfire, and conservation [PDF]. Conservation Biology. 2004;18(4):890–902. doi:10.1111/j.1523-1739.2004.00492.x.
- "National Wildfire Coordinating Group Communicator's Guide for Wildland Fire Management: Fire Education, Prevention, and Mitigation Practices, Wildland Fire Overview" (PDF). National Wildfire Coordinating Group. Retrieved 11 December 2008.
- Nepstad, Daniel C (2007). "The Amazon's Vicious Cycles: Drought and Fire in the Greenhouse" (PDF). World Wide Fund for Nature (WWF International). Retrieved 9 July 2009.
- Olson, Richard Stuart; Gawronski, Vincent T (2005). "The 2003 Southern California Wildfires: Constructing Their Cause(s)" (PDF). Quick Response Research Report. University of Colorado at Boulder Natural Hazards Center. 173. Retrieved 15 July 2009. (HTML version)
- Pausas, Juli G; Keeley, Jon E (July–August 2009). "A Burning Story: The Role of Fire in the History of Life" (PDF). BioScience. American Institute of Biological Sciences. 59 (7): 593–601. ISSN 0006-3568. doi:10.1525/bio.2009.59.7.10.
- Peuch, Eric (26–28 April 2005). "Firefighting Safety in France" (PDF). In Butler, B W; Alexander, M E. Eighth International Wildland Firefighter Safety Summit – Human Factors – 10 Years Later (PDF). Missoula, Montana: The International Association of Wildland Fire, Hot Springs, South Dakota.
- Pitkänen, Aki; Huttunen, Pertti; Jungner, Högne; Meriläinen, Jouko; Tolonen, Kimmo (28 February 2003). "Holocene fire history of middle boreal pine forest sites in eastern Finland" (PDF). Annales Botanici Fennici. 40: 15–33. ISSN 0003-3847.
- Plucinski, M; Gould, J; McCarthy, G; Hollis, J (June 2007). The Effectiveness and Efficiency of Aerial Firefighting in Australia: Part 1 (PDF) (Report). Bushfire Cooperative Research Centre. ISBN 0-643-06534-2. Retrieved 4 March 2009.
- San-Miguel-Ayanz, Jesus; Ravail, Nicolas; Kelha, Vaino; Ollero, Anibal (2005). "Active Fire Detection for Fire Emergency Management: Potential and Limitations for the Operational Use of Remote Sensing" (PDF). Natural Hazards. Springer. 35 (3): 361–376. doi:10.1007/s11069-004-1797-2. Retrieved 5 March 2009.
- van Wagtendonk, Jan W (1996). "Use of a Deterministic Fire Growth Model to Test Fuel Treatments" (PDF). Sierra Nevada Ecosystem Project: Final report to Congress, vol. II, Assessments and scientific basis for management options. Davis: University of California, Centers for Water and Wildland Resources: 1155–1166. Retrieved 5 February 2009.
- van Wagtendonk, Jan W (2007). "The History and Evolution of Wildland Fire Use" (PDF). Fire Ecology. Association for Fire Ecology. 3 (2): 3–17. doi:10.4996/fireecology.0302003. Retrieved 24 August 2008. (U.S. Government public domain material published in Association journal. See WERC Highlights – April 2008)
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