ライフサイエンスコーパス: forest fire

1 ere determined from the subtropical eucalypt forest fire.

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

3 dissipated due to the influence of a nearby forest fire.

4 tion on the toxicity of particulate ROC from forest fires.

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

6 inal Tasmanians, despite episodic widespread forest fires.

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

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

9 d drying has led to more severe and frequent forest fires(5-7), which threaten to shift the carbon ba

10 3 PAHs) were determined from the subtropical forest fire (7,000 +/- 170) compared to the tropical sav

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

12 Increased forest fire activity across the western continental Unit

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

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

15 nd total losses of biomass in land clearing, forest fires and clear cuts are easy to measure.

16 dium spp, predominantly), impacted or not by forest fires and collected at different times, were stud

17 electric tissues and chemical oscillators to forest fires and competing populations, are nonlinear, s

18 e Amazon where recent records show increased forest fires and deforestation.

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

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

21 further underestimates emissions from Arctic forest fires and inadequately represents long-range poll

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

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

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

25 of complex phenomena including earthquakes, forest fires and solar flares.

26 that has resulted in increased frequency of forest fires and subsequent alteration of watershed carb

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

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

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

30 ces of brown carbon include biomass burning, forest fires, and residential burning of biofuels, and a

31 Forest fires, Arctic air masses, and road salt also impa

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

33 Forest fires are growing in size and frequency across th

34 Forest fires are increasing across the American West due

35 Forest fires are larger carbon dioxide sources per unit

36 Forest fires are usually viewed within the context of a

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

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

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

40 he western United States (WUS), where annual forest fire area increased by more than 1,100% during 19

41 We found that forest fires avoided ownerships with a concentration of

42 n, as well as the risk of biotic attacks and forest fire behaviour.

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

44 carbon emissions from the Amazon, with many forest fires burning uncontrolled for weeks.

45 Destruction was more likely in forest fires, but they burned less WUI.

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

47 This contributed to a 60% increase in forest fire carbon emissions from forest ecoregions glob

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

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

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

51 Furthermore, we show that Forest Fire Clustering can make robust, inductive infere

52 Overall, Forest Fire Clustering is a useful tool for rare cell ty

53 Forest Fire Clustering makes minimal prior assumptions a

54 Here, we introduce Forest Fire Clustering, an efficient and interpretable m

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

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

57 Forest fires create positive feedbacks in future fire su

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

59 hifts in ambient temperature, air pollution, forest fires, desert (dust and sand) storms and extreme

60 nds that influence regional hydroclimate and forest fire during the following warm season.

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

62 with recently estimated increases in global forest fire emissions and active fire detections.

63 function of pyrogenic carbon in neutralizing forest fire emissions and call for its consideration in

64 delineation revealed that rapidly increasing forest fire emissions in extratropical pyromes, linked t

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

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

67 Boreal forest fires emit large amounts of carbon into the atmos

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

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

70 he influence of NPJ behavior on moisture and forest fire extremes in California before and during the

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

72 Forest fires generate a large amount of carbon that rema

73 Record-breaking summer forest fires have become a regular occurrence in Califor

74 The 2023 Canadian forest fires have been extreme in scale and intensity wi

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

76 oisture content (FMC) is a crucial driver of forest fires in many regions world-wide.

77 we focus on the elevational distribution of forest fires in mountainous ecoregions of the western Un

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

79 yed by grassland and shrubland fires than by forest fires in the United States.

80 collected on unmanned aircraft systems over forest fires in Utah, USA, we determine bacterial emissi

81 Forest fires include biogenic emissions that produce SOA

82 Forest fire increases surface temperature by 0.15 K (0.1

83 sitive to vegetation changes associated with forest fires, increasing by 94% in burned vs. unburned f

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

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

86 rmer world would likely increase the risk of forest fires, leading to potentially substantial release

87 s in models, our results suggest that boreal forest fires may be more sensitive to future aerosol mit

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

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

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

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

92 paredness, enhancing their ability to manage forest fires more efficiently.

93 Forest fires occur with increasing frequency and severit

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

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

96 by the carbon dioxide emission increase from forest fires offsetting the decreasing emissions from gr

97 The biophysical feedbacks of forest fire on Earth's surface radiative budget remain u

98 n extreme El Nino (EN) drought and extensive forest fires on plant mortality and carbon loss in undis

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

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

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

102 imilar to previous observations of temperate forest fire plumes.

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

104 In contrast, the health risk from forest fire-related PAH emissions may play an increasing

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

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

107 nic compounds (ROC) in western U.S. wildland forest fire smoke using a combination of observations fr

108 Forest fire suppression has reduced habitat and disrupte

109 ern migrant tactic emerged following a large forest fire that enhanced forage in an area with lower p

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

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

112 The forest fires were only completely under control at the b

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

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

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

116 on prenatal exposure to the 1997 Indonesian forest fires with child nutritional outcomes and find th