ライフサイエンスコーパス: forest fire

1 d in-situ immediately after a typical boreal forest fire.

2 ere determined from the subtropical eucalypt forest fire.

3 ge-scale disturbances such as clear cuts and forest fires.

4 Neither were egg Hg trends related to recent forest fires.

5 and of a similar magnitude as emissions from forest fires.

6 3 PAHs) were determined from the subtropical forest fire (7,000 +/- 170) compared to the tropical sav

7 rallels debates involving abstract models of forest fires, a central metaphor in complex systems theo

8 Increased forest fire activity across the western continental Unit

9 change has emerged as a driver of increased forest fire activity and should continue to do so while

10 For example, avalanches, earthquakes, and forest fires all propagate in systems organized into a c

11 ng) within the Athabasca watershed, however, forest fires and erosion of fossil fuel deposits within

12 etle outbreaks fuel more ecologically severe forest fires and impair postfire resilience.

13 ied greatly since 1788 as a result of boreal forest fires and industrial activities.

14 ency-size statistics of two natural hazards, forest fires and landslides.

15 onths and in southern California (related to forest fires and secondary OC).

16 observed behavior, the forest fire model for forest fires and the sand pile model for landslides.

17 chanism of feedback particularly relevant to forest fires), and it presents evidence that characteris

18 olcanism, biogenic activity, windblown dust, forest fires, and pollution-induced acid rain.

19 nce Arctic temperatures and the frequency of forest fires are both expected to rise with climate chan

20 Forest fires are growing in size and frequency across th

21 increases in eight fuel aridity metrics and forest fire area across the western United States.

22 ntributed to an additional 4.2 million ha of forest fire area during 1984-2015, nearly doubling the f

23 e area during 1984-2015, nearly doubling the forest fire area expected in its absence.

24 ring the droughts of 2007 and 2010, regional forest fires burned 12 and 5% of southeastern Amazon for

25 ng of medicinal plants, pasturing cattle and forest fires can induce environmental modifications, esp

26 Our work also suggests that forest fires cause greater ALTs by simultaneously decrea

27 s often lead to more common and more intense forest fires, causing dramatic changes in the nutrient s

28 es in its watershed during the study period (forest fire; changes in shoreline inundation due to beav

29 ocessed AOS bitumen, upgrader residual coke, forest fires, coal, gasoline and diesel soot).

30 Along a transect (10-150-350 m) from the forest fire, concentration decrease for PCBs during flam

31 Forest fires create positive feedbacks in future fire su

32 Consequently, there is now a forest "fire deficit" in the western United States attri

33 The forest fire dynamics in two regions of the eastern Amazo

34 Affecting the health of millions, net forest fire emissions may have released carbon equivalen

35 se results suggest that the impact of boreal forest fire emissions on air quality in the mid-latitude

36 However, a forest fire episode during April to July 2011 resulted i

37 concerning their initiation and propagation, forest fires exhibit power-law frequency-area statistics

38 atural petrogenic source (93% petrogenic, 7% forest fire) for alkylated PAHs during the past approxim

39 how that these episodes were caused by large forest fires in Canada.

40 Smoke from forest fires in southern Mexico was advected into the U.

41 Forest fires include biogenic emissions that produce SOA

42 ombustion, suggests that its use as a unique forest fire indicator may not be suitable in PAD sedimen

43 report measurements and analysis of a boreal forest fire, integrating the effects of greenhouse gases

44 d as analogs for this observed behavior, the forest fire model for forest fires and the sand pile mod

45 For the forest fire model the cascade consists of the coalescenc

46 A simple forest fire model, which is an example of self-organized

47 Application of a recently developed forest-fire model indicates that epidemic cholera dynami

48 Forest fires occur with increasing frequency and severit

49 Prominent peaks in forest fires occurred during the Medieval Climate Anomal

50 e are well documented in North America, with forest fire occurrence and area clearly increasing in re

51 assessments from destructive events such as forest fires or clear felling of forests.

52 d PAHs and DBTs were not elevated during the forest fire period, supporting their association with pe

53 Within the forest fire plumes, there were also high concentrations

54 ck carbon sediments from Northern Hemisphere forest fires reduced albedo below a critical threshold i

55 en drought and fire regimes in United States forests, fire-related drought metrics and expected chang

56 sults suggest that warming may also increase forest fire severity (the number of trees killed) indepe

57 Forest fire suppression has reduced habitat and disrupte

58 ecover from catastrophic disturbances (e.g., forest fires, traffic jams, orphaned children, and refug

59 EF data for many PAHs from the eucalypt forest fire were comparable with those previously report

60 l stacks, vehicles, residential heating, and forest fires, whereas the PAH concentrations at AMS 14 (

61 dies have found that conditions conducive to forest fires, which generate harmful air pollutants and

62 e severe during El Nino events, pan-tropical forest fires will increase as more damaged, less fire-re