Draft:Chisholm fire
 | Review waiting, please be patient.
This may take 6 weeks or more, since drafts are reviewed in no specific order. There are 1,213 pending submissions waiting for review.
Where to get help
How to improve a draft
You can also browse Wikipedia:Featured articles and Wikipedia:Good articles to find examples of Wikipedia's best writing on topics similar to your proposed article. Improving your odds of a speedy review To improve your odds of a faster review, tag your draft with relevant WikiProject tags using the button below. This will let reviewers know a new draft has been submitted in their area of interest. For instance, if you wrote about a female astronomer, you would want to add the Biography, Astronomy, and Women scientists tags. Editor resources
Reviewer tools
|
Comment: I don't really see a lot of WP:SECONDARY sources that discuss the event, particularly after the event. Bobby Cohn (talk) 19:46, 21 October 2024 (UTC)
 | This article relies largely or entirely on a single source. (October 2024) |
| Chisholm Fire | |
|---|---|
| Date(s) | May 23, 2001 – June 4, 2001 |
| Location | Alberta, Canada |
| Statistics | |
| Total area | 116,000 hectares (290,000 acres) |
| Impacts | |
| Structures destroyed | >=61 |
The Chisholm fire was a forest fire in the Canadian province of Alberta that burned in the late spring of 2001. It is known for its exceptional intensity and fire behavior. In fact, at the time, it had the highest head fire intensity ever recorded.[1] The fire was declared under control on June 4, 2001,[2] with a total burned area of 116,000 hectares (290,000 acres).[3] It was notable for its record-setting intensity and several research papers were conducted regarding this fire and its unique pyrocumulonimbus cloud.[4][5][6][7]It was one of the first fires to have known to penetrate the tropopause in recorded history.[8]
Background
[edit]Northern Alberta is largely boreal forest, with a mix of deciduous and highly flammable conifer species, such as white and black spruce, balsam fir, and jack pine. This is a forest type adapted to fire that burns in 50- to 200-year cycles.[9] In 2001, fire season started on March 1st, a month earlier than all previous years except 2000. This was the result of precipitation deficits from the winters of 1997-2000 which led to unprecedented fuel consumption by the fire. Over 300 fires have burned in Alberta in the few weeks prior to this fire,[10] and 6 fires were burning simultaneously with this fire.[9] Similarities have been drawn with the 1968 Vega Fire, in particular regarding the weather conditions, extreme fire intensity, rapid rates of spread, and the location where it burned.[1]
Ignition
[edit]The fire was initially discovered at 9:19 PM local time on May 23, 2001 by the public, who alerted fire officials. The Alberta government faulted a malfunctioning train wheel on a Canadian National Railway train as the source of the fire.[11] The fire rapidly spread through the night and by 9 A.M the following day, it covered 4,000 hectares (9,900 acres) of land.[1]
Progression
[edit]Unusually intense fire behavior was observed on the first night, with crowning occurring late into the night.[12] On the second day, extremely active fire behavior was recorded, including spots 1km ahead of the fire, and occasional torching. In the morning, the fire jumped the Athabasca River. By noon, it had spread further, with an infrared mapping putting it at 4,310 hectares (10,700 acres). The next day, the fire made its first run toward the hamlet of Chisholm, Alberta. At 19:00 local time, it crossed the dozer line, and then proceeded to spread extremely rapidly, covering approximately 1 mile (1.6 km) in just 5 minutes.[1] Fire activity moderated on the 26th due to a small amount of rain. However, this lull in activity would not last long, as the next day, the fire made a large run to the northwest, away from Chisholm. The day after that(the 28th), winds were strong(30-50 km/h sustained), along with high fuel densities, so the day was dominated by extreme fire behavior. A spot fire was observed at 1:30 PM. Due to the strong winds, intense fire behavior, and smoke, the spot fire could not be brought under control, and the spot fire later burned some structures within the next couple hours. The fire soon developed a 45,000 foot convection column.[1] Just after 4 P.M, another fire started NE of Chisholm, Alberta and rapidly spread, making a 12 kilometer run and chewing through 3,063 hectares (7,570 acres) of land by 8 P.M. Weather conditions moderated the next day, and from then on, no significant fire activity was observed.[1]
Effects
[edit]Firefighting efforts cost the Albertan government CA$10,000,000 (equivalent to $16,063,395 in 2023).[9] The town of Chisholm suffered significant losses from the fire, with 10 homes, 51 outbuildings, and several vehicles destroyed. At that time, Chisholm only had a total of 19 houses. In addition, there were other losses, such as forest resource losses and oil and gas shutdowns.[1]There was some controversy about firefighting methods used against the fire, with some people blaming the government for the loss of their homes.[neutrality is disputed] Suggestions pertaining to firefighting methods have been adopted by local officials.[13]In 2004, CN agreed to pay CA$18.8 million as settlement, with some of those funds going toward wildfire reduction programs.[11]
References
[edit]- ^ a b c d e f g "Final documentation report Chisholm fire (LWF-063) - Open Government". open.alberta.ca. Retrieved 2024-08-21.
- ^ "Massive Alberta forest fire contained". CBC News. June 4, 2001.
- ^ Benscoter, Brian W; Wieder, R Kelman (2003-12-01). "Variability in organic matter lost by combustion in a boreal bog during the 2001 Chisholm fire". Canadian Journal of Forest Research. 33 (12): 2509–2513. doi:10.1139/x03-162. ISSN 0045-5067.
- ^ Fromm, M.; Torres, O.; Diner, D.; Lindsey, D.; Vant Hull, B.; Servranckx, R.; Shettle, E. P.; Li, Z. (2008-04-27). "Stratospheric impact of the Chisholm pyrocumulonimbus eruption: 1. Earth‐viewing satellite perspective". Journal of Geophysical Research: Atmospheres. 113 (D8). doi:10.1029/2007JD009153. ISSN 0148-0227.
- ^ Rosenfeld, Daniel (February 9, 2007). "The Chisholm firestorm: observed microstructure, precipitation and lightning activity of a pyro-cumulonimbus" (PDF). ACP Copernicus.
- ^ Tory, K. J.; Kepert, J. D. (2021-04-01). "Pyrocumulonimbus Firepower Threshold: Assessing the Atmospheric Potential for pyroCb". Weather and Forecasting. 36 (2): 439–456. doi:10.1175/WAF-D-20-0027.1. ISSN 1520-0434.
- ^ Fromm, Michael D.; Servranckx, René (2003-05-15). "Transport of forest fire smoke above the tropopause by supercell convection". Geophysical Research Letters. 30 (10). doi:10.1029/2002GL016820. ISSN 0094-8276.
- ^ "Smoke Soars to Stratospheric Heights". NASA Jet Propulsion Laboratory (JPL). Retrieved 2024-10-19.
- ^ a b c Chisholm fire Review Committee (2001-10-01). Chisholm Fire Review Committee final report (PDF). Edmonton, Alberta: Sustainable Resource Development, Government of Alberta. p. 7.
- ^ "Light rain dampens huge Alberta fire - UPI Archives". UPI. Retrieved 2024-10-21.
- ^ a b "CN settles Alberta wildfire claims". CBC. January 13, 2006. Retrieved October 21, 2024.
- ^ "The World's First Wildfire Tornado Blazed a Path of Destruction Through Australia". Smithsonian Magazine. 2023-06-06. Retrieved 2024-09-12.
- ^ "Memories return on anniversary of one of Alberta's most destructive fires". CBC. May 24, 2002. Retrieved October 21, 2024.