Matches in SemOpenAlex for { <https://semopenalex.org/work/W2436692536> ?p ?o ?g. }
- W2436692536 abstract "Abstract Forest fires are an important disturbance factor of boreal forests, annually burning about 0.5% of the forested area in Canada. Wildfire regimes are influenced by climate and a number of studies project an increase in wildfire activity with climate change. Another factor influencing wildfires is human intervention (fire suppression), and one factor that has rarely been assessed is fuel fragmentation. Studies evaluating the effect of forest fire suppression concluded that in areas with strong suppression effort the burned area as well as the fire size decreased. Here we evaluate wildfire distributions over the last three decades for two areas that differ mainly in their level of forest management and fire suppression: the Boreal Shield (unmanaged) and the Boreal Plain regions (intensively managed) in the Canadian Province of Saskatchewan. We calculate a fuel fragmentation index and relate fire sizes and burned areas to fire weather. We use the concept of the characteristic fire size (CFS); hence we analyze how much burned area is contributed to the total burned area per fire size class. Both areas show a uni-modal distribution of the CFS, indicating that the majority of burned area was contributed by medium sized fires (Boreal Shield 6.39 · 104 ha, the Boreal Plain 8.79 · 104 ha). Burned area as well as fuel fragmentation is lower in the managed forest compared to the unmanaged area. The fuel fragmentation index constantly increased since the 1980s in both regions. Despite the large efforts of fire suppression in the Boreal Plains, the CFS is slightly larger in this managed region. Neither the burned area nor the fire size could be linked statistically to the weather conditions, at the time of the fire (using the Canadian Fire Weather Index). We argue that the high fragmentation over the last decades have decreased the burned area. The slightly higher characteristic fire size in the managed area might be explained by the considerably lower fragmentation, counteracting fire suppression efforts. Fuel fragmentation is likely to decrease over the next decades due re-growth. Though a strong link between fire weather and burned area at the fine scale of this study could not be detected we expect that a decrease in fragmentation in combination with an increase in fire prone weather conditions (as expected for the future) might increase the risk of large fires in both areas. We suggest that future fire risk analysis should include an assessment of the effect of fuel fragmentation." @default.
- W2436692536 created "2016-06-24" @default.
- W2436692536 creator A5067386175 @default.
- W2436692536 creator A5069408220 @default.
- W2436692536 creator A5078913441 @default.
- W2436692536 date "2016-09-01" @default.
- W2436692536 modified "2023-09-24" @default.
- W2436692536 title "Fuel fragmentation and fire size distributions in managed and unmanaged boreal forests in the province of Saskatchewan, Canada" @default.
- W2436692536 cites W1882556349 @default.
- W2436692536 cites W1976902084 @default.
- W2436692536 cites W1982800299 @default.
- W2436692536 cites W1985769566 @default.
- W2436692536 cites W1988183644 @default.
- W2436692536 cites W1988559119 @default.
- W2436692536 cites W1989364707 @default.
- W2436692536 cites W1992550673 @default.
- W2436692536 cites W2014229429 @default.
- W2436692536 cites W2017724555 @default.
- W2436692536 cites W2021576258 @default.
- W2436692536 cites W2022974530 @default.
- W2436692536 cites W2044934292 @default.
- W2436692536 cites W2047212340 @default.
- W2436692536 cites W2047656004 @default.
- W2436692536 cites W2056091222 @default.
- W2436692536 cites W2065227035 @default.
- W2436692536 cites W2083309207 @default.
- W2436692536 cites W2122134723 @default.
- W2436692536 cites W2125408438 @default.
- W2436692536 cites W2127725134 @default.
- W2436692536 cites W2132481553 @default.
- W2436692536 cites W2144743642 @default.
- W2436692536 cites W2156302207 @default.
- W2436692536 cites W2157820541 @default.
- W2436692536 cites W2165977355 @default.
- W2436692536 cites W2166229287 @default.
- W2436692536 cites W2168084509 @default.
- W2436692536 cites W2170474871 @default.
- W2436692536 cites W2255133319 @default.
- W2436692536 cites W2279888815 @default.
- W2436692536 cites W4248183608 @default.
- W2436692536 doi "https://doi.org/10.1016/j.foreco.2016.06.014" @default.
- W2436692536 hasPublicationYear "2016" @default.
- W2436692536 type Work @default.
- W2436692536 sameAs 2436692536 @default.
- W2436692536 citedByCount "5" @default.
- W2436692536 countsByYear W24366925362016 @default.
- W2436692536 countsByYear W24366925362017 @default.
- W2436692536 countsByYear W24366925362019 @default.
- W2436692536 countsByYear W24366925362020 @default.
- W2436692536 countsByYear W24366925362021 @default.
- W2436692536 crossrefType "journal-article" @default.
- W2436692536 hasAuthorship W2436692536A5067386175 @default.
- W2436692536 hasAuthorship W2436692536A5069408220 @default.
- W2436692536 hasAuthorship W2436692536A5078913441 @default.
- W2436692536 hasConcept C100537666 @default.
- W2436692536 hasConcept C100970517 @default.
- W2436692536 hasConcept C110872660 @default.
- W2436692536 hasConcept C127313418 @default.
- W2436692536 hasConcept C132651083 @default.
- W2436692536 hasConcept C151730666 @default.
- W2436692536 hasConcept C166957645 @default.
- W2436692536 hasConcept C18903297 @default.
- W2436692536 hasConcept C191015642 @default.
- W2436692536 hasConcept C195330766 @default.
- W2436692536 hasConcept C205649164 @default.
- W2436692536 hasConcept C2777601987 @default.
- W2436692536 hasConcept C39432304 @default.
- W2436692536 hasConcept C54286561 @default.
- W2436692536 hasConcept C86803240 @default.
- W2436692536 hasConcept C87621631 @default.
- W2436692536 hasConcept C89736061 @default.
- W2436692536 hasConcept C97137747 @default.
- W2436692536 hasConceptScore W2436692536C100537666 @default.
- W2436692536 hasConceptScore W2436692536C100970517 @default.
- W2436692536 hasConceptScore W2436692536C110872660 @default.
- W2436692536 hasConceptScore W2436692536C127313418 @default.
- W2436692536 hasConceptScore W2436692536C132651083 @default.
- W2436692536 hasConceptScore W2436692536C151730666 @default.
- W2436692536 hasConceptScore W2436692536C166957645 @default.
- W2436692536 hasConceptScore W2436692536C18903297 @default.
- W2436692536 hasConceptScore W2436692536C191015642 @default.
- W2436692536 hasConceptScore W2436692536C195330766 @default.
- W2436692536 hasConceptScore W2436692536C205649164 @default.
- W2436692536 hasConceptScore W2436692536C2777601987 @default.
- W2436692536 hasConceptScore W2436692536C39432304 @default.
- W2436692536 hasConceptScore W2436692536C54286561 @default.
- W2436692536 hasConceptScore W2436692536C86803240 @default.
- W2436692536 hasConceptScore W2436692536C87621631 @default.
- W2436692536 hasConceptScore W2436692536C89736061 @default.
- W2436692536 hasConceptScore W2436692536C97137747 @default.
- W2436692536 hasLocation W24366925361 @default.
- W2436692536 hasOpenAccess W2436692536 @default.
- W2436692536 hasPrimaryLocation W24366925361 @default.
- W2436692536 hasRelatedWork W1485823330 @default.
- W2436692536 hasRelatedWork W1975910192 @default.
- W2436692536 hasRelatedWork W1976823336 @default.
- W2436692536 hasRelatedWork W2047656004 @default.
- W2436692536 hasRelatedWork W2073965784 @default.
- W2436692536 hasRelatedWork W2075167675 @default.
- W2436692536 hasRelatedWork W2075802165 @default.