scholarly journals Fire scars reveal source of New England's 1780 Dark Day

2007 ◽  
Vol 16 (3) ◽  
pp. 266 ◽  
Author(s):  
Erin R. McMurry ◽  
Michael C. Stambaugh ◽  
Richard P. Guyette ◽  
Daniel C. Dey
Keyword(s):  
New England ◽  
Direct Evidence ◽  
Atmospheric Conditions ◽  
Historical Evidence ◽  
Fire Scars ◽  
Fire Scar ◽  
Lake States

Historical evidence suggests that great wildfires burning in the Lake States and Canada can affect atmospheric conditions several hundred miles away (Smith 1950; Wexler 1950). Several ‘dark’ or ‘yellow’ days, as such events are commonly called, have been recorded, often with anecdotal or direct evidence pointing to wildfires as the source (Plummer 1912; Ludlum 1972). One such ‘dark day’ occurred across New England in 1780, a year in which people were technologically unable to confirm the source of such a phenomenon. Here we combine written accounts and fire scar evidence to document wildfire as the likely source of the infamous Dark Day of 1780.

Fire histories in ponderosa pine forests of Grand Canyon are well supported: reply to Baker

2006 ◽  
Vol 15 (3) ◽  
pp. 439 ◽  
Author(s):  
Peter Z. Fulé ◽  
Thomas A. Heinlein ◽  
W. Wallace Covington
Keyword(s):  
Ponderosa Pine ◽  
Grand Canyon ◽  
Pine Forests ◽  
Fire Scars ◽  
Surface Fire ◽  
Ponderosa Pine Forests ◽  
Fire Scar ◽  
Study Sites ◽  
Fire Intervals ◽  
Old Trees

Fire scars and other paleoecological methods are imperfect proxies for detecting past patterns of fire events. However, calculations of long fire rotations in Grand Canyon ponderosa pine forests by Baker are not convincing in methodology or assumptions compared with fire-scar evidence of frequent surface fires. Patches of severe disturbance are a possible hypothesis to explain the relatively short age structure at the park, where ~12% fewer trees were older than 300 years compared with another unharvested northern Arizona site. However, mapped patterns of old trees as well as the evidence for frequent surface fire from fire scars, charcoal deposition studies, and evolutionary history are more consistent with the dominance of surface fire prior to c. 1880. The most relevant available evidence of fire recurrence at a given point, mean point fire intervals, had median values <16 years at all five study sites, close to filtered composite fire interval statistics (~6–10 years), but much lower than Baker’s calculated fire rotation values (55–110 years). The composite fire interval is not a uniquely important statistic or a numerical guideline for management, but one of many lines of evidence underscoring the ecological role of frequent surface fire in ponderosa pine forests.

scholarly journals Fire-scarred fossil tree from the Late Triassic shows a pre-fire drought signal

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Bruce A. Byers ◽  
Lucía DeSoto ◽  
Dan Chaney ◽  
Sidney R. Ash ◽  
Anya B. Byers ◽  
...  
Keyword(s):  
National Park ◽  
Wood Anatomy ◽  
Recovery Period ◽  
Late Triassic ◽  
Fire Scars ◽  
Ecological Processes ◽  
Fire Scar ◽  
Evolutionary Force ◽  
Ancient Forests

AbstractExploring features of wood anatomy associated with fire scars found on fossil tree trunks is likely to increase our knowledge of the environmental and ecological processes that occurred in ancient forests and of the role of fire as an evolutionary force. In Petrified Forest National Park, Arizona, where Late Triassic fossil trees are exposed, we found 13 examples of fossil logs with external features resembling modern fire scars. One specimen with the unambiguous external features of a fire scar was collected for analysis of its fossilized wood. A light-colored band composed of compressed and distorted tracheids was associated with the scarring event. Cell lumen diameter and cell wall thickness in the pre-scarring fossilized wood show a response similar to that described in modern trees experiencing drought conditions. Tracheids in the post-scarring wood are initially smaller, and then become larger than average following a recovery period, as is often observed in modern conifers following fire. The responses in external morphology and wood anatomy to drought and fire were similar to those of some modern trees and support the view that some forests may have experienced conditions favoring the evolution of fire-adapted traits for more than 200 million years.

Forest-fire-scar aging using SPOT-VEGETATION for Canadian ecoregions

2003 ◽  
Vol 33 (6) ◽  
pp. 1116-1125 ◽  
Author(s):  
Brian D Amiro ◽  
Jing M Chen
Keyword(s):  
Near Infrared ◽  
Forest Succession ◽  
Short Wave ◽  
Federal Agencies ◽  
Infrared Band ◽  
Fire Scars ◽  
Fire Scar ◽  
Remote Sensing Techniques ◽  
Large Effort ◽  
Nominal Resolution

The mapping of Canadian fires is a large effort supported by provincial, territorial, and federal agencies. Remote sensing techniques can aid in mapping, especially in remote areas and during busy fire seasons. The SPOT-VEGETATION (SPOT-VGT) sensor has previously shown promise at distinguishing fire scars on the landscape. The usefulness of SPOT-VGT to age fires in 18 Canadian ecoregions was evaluated for a period up to 50 years since fire, analysing more than 250 000 pixels (nominal resolution about 1 km2). The SPOT-VGT reflectances were evaluated using the ratio of the short-wave infrared band (1.58–1.75 µm) to near-infrared band (0.78–0.89 µm), compared with the Canadian large-fire database (fires greater than 200 ha in size). Nonlinear regressions were significant for all ecoregions with r2 values being greater than 0.57 for 16 of them. Five ecoregions groupings had similar relationships, consistent with their contiguous pattern on the landscape. The prediction of fire-scar age depends on ecoregion and can be successful over periods as short as 6 years to as long as 30 years. The root mean square error for all ecoregions ranged from 5 years for recent burns to about 12 years for three decades following fire. This tool is useful to get approximate fire-scar ages, but the accuracy is limited because of the variation in forest succession on the landscape, and it cannot replace more detailed mapping done currently by fire agencies.

Fire history in a Sequoiasempervirens forest at Salt Point State Park, California

1989 ◽  
Vol 19 (11) ◽  
pp. 1451-1457 ◽  
Author(s):  
Mark A. Finney ◽  
Robert E. Martin
Keyword(s):  
Fire History ◽  
Moving Average ◽  
Fire Scars ◽  
Coast Redwood ◽  
Fire Scar ◽  
Point Data ◽  
Substantial Bias ◽  
Fire Intervals ◽  
Redwood Forest ◽  
Composite Data

Fire occurrence data between the 12th and 20th centuries were obtained from analysis of fire scars on coast redwood (Sequoiasempervirens (D. Don.) Endl.) and bishop pine (Pinusmuricata D. Don.). Mean fire intervals were calculated for settlement and presettlement periods from fire scar samples individually (point data) and from composites of samples aggregated within three approximately 200-ha study areas. Mean fire intervals from point data (20.5 to 29.0 years) were more than three times greater than mean intervals from composite data (6.1 to 9.3 years). Mean fire intervals derived from point data compared well with values previously reported, although substantial bias ascribed to point data suggests that these values for mean fire intervals in redwood forest communities are too large. A period of significantly longer fire intervals during the 17th century was suggested by analysis of fire intervals by century and using a moving average.

Comparison of fire scars, fire atlases, and satellite data in the northwestern United States

2007 ◽  
Vol 37 (10) ◽  
pp. 1933-1943 ◽  
Author(s):  
Lauren B. Shapiro-Miller ◽  
Emily K. Heyerdahl ◽  
Penelope Morgan
Keyword(s):  
20Th Century ◽  
Regional Scale ◽  
Early 20Th Century ◽  
Fire Scars ◽  
Late 20Th Century ◽  
Fire Scar ◽  
Fire Atlas ◽  
Normalized Burn Ratio ◽  
Source Of Information ◽  
Fire Extent

We evaluated agreement in the location and occurrence of 20th century fires recorded in digital fire atlases with those inferred from fire scars that we collected systematically at one site in Idaho and from existing fire-scar reconstructions at four sites in Washington. Fire perimeters were similar for two of three 20th century fires in Idaho (1924 and 1986). Overall spatial agreement was best in 1924 (producer’s accuracy = 94% and 68% and user’s accuracy = 90% and 70% for the 1924 and 1986 fires, respectively). In 1924, fire extent from the atlas was greater than for fire scars, but the reverse was true for 1986. In 1986, fire extent interpreted from the delta normalized burn ratio derived from pre- and post-fire satellite imagery was similar to that inferred from the fire-scar record (producer’s accuracy = 92%, user’s accuracy = 88%). In contrast, agreement between fire-scar and fire-atlas records was poor at the Washington sites. Fire atlases are the most readily available source of information on the extent of late 20th century fires and the only source for the early 20th century. While fire atlases capture broad patterns useful at the regional scale, they should be field validated and used with caution at the local scale.

Anatomical changes induced by fire-damaged cambium in two native tree species of the Chaco Region, Argentina

IAWA Journal ◽  
2010 ◽  
Vol 31 (3) ◽  
pp. 283-292 ◽  
Author(s):  
Sandra Bravo
Keyword(s):  
Cross Sections ◽  
Wood Quality ◽  
Cambial Activity ◽  
Wood Formation ◽  
Vessel Diameter ◽  
Fire Damage ◽  
Fire Scars ◽  
Fire Scar ◽  
Chaco Region ◽  
Altered Zone

This study examined anatomical responses to fire damage of the cambium in Schinopsis lorentzii and Aspidosperma quebracho-blanco. Bole cross sections were extracted from specimens with external signs of fire damage. Samples were taken from zones designated normal, discoloured and wound altered. The vessel, fibre, axial and ray parenchyma percentages, tangential vessel diameter, vessels per mm2, rays per mm, and ray width and height of these zones were compared. Fire scars and fire marks were identified on cross sections of S. lorentzii and A. quebracho-blanco. The fire marks reflect minor wounds that did not affect wood formation. The fire scars, on the other hand, are the result of wounds that interrupted cambial activity thus affecting the shape of the bole and causing discolouration of pre-existing wood adjacent to wounds. The wood formed after fire damage included callus, barrier zones at fire scar edges and the formation of ribs of wound wood. The wound altered zone was characterised by a decrease in the percentage of vessels and fibres, an increase in the percentage of axial parenchyma, the formation of grouped rays, a decrease in vessel tangential diameter, and occurrence of fibres with atypical structure. Disorientation in the axial xylem system was observed in the barrier zone. The anatomical responses to cambium damage and formation of discoloured wood and woundwood ribs suggest that wood quality and utilisable volume of bole in the studied species is affected by fire.

scholarly journals Integrating fire-scar, charcoal and fungal spore data to study fire events in the boreal forest of northern Europe

The Holocene ◽  
2019 ◽  
Vol 29 (9) ◽  
pp. 1480-1490 ◽  
Author(s):  
Normunds Stivrins ◽  
Tuomas Aakala ◽  
Liisa Ilvonen ◽  
Leena Pasanen ◽  
Timo Kuuluvainen ◽  
...  
Keyword(s):  
Boreal Forest ◽  
Tree Rings ◽  
Fire History ◽  
Statistical Tests ◽  
Sediment Cores ◽  
Fungal Spores ◽  
Fire Dynamics ◽  
Fire Scars ◽  
Fire Event ◽  
Fire Scar

Fire is a major disturbance agent in the boreal forest, influencing many current and future ecosystem conditions and services. Surprisingly few studies have attempted to improve the accuracy of fire-event reconstructions even though the estimates of the occurrence of past fires may be biased, influencing the reliability of the models employing those data (e.g. C stock, cycle). This study aimed to demonstrate how three types of fire proxies – fire scars from tree rings, sedimentary charcoal and, for the first time in this context, fungal spores of Neurospora – can be integrated to achieve a better understanding of past fire dynamics. By studying charcoal and Neurospora from sediment cores from forest hollows, and the fire scars from tree rings in their surroundings in the southern Fennoscandian and western Russian boreal forest, we produced composite fire-event data sets and fire-event frequencies, and estimated fire return intervals. Our estimates show that the fire return interval varied between 126 and 237 years during the last 11,000 years. The highest fire frequency during the 18th–19th century can be associated with the anthropogenic influence. Importantly, statistical tests revealed a positive relationship between other fire event indicators and Neurospora occurrence allowing us to pinpoint past fire events at times when the sedimentary charcoal was absent, but Neurospora were abundant. We demonstrated how fire proxies with different temporal resolution can be linked, providing potential improvements in the reliability of fire history reconstructions from multiple proxies.

Fire History and Tree Recruitment in an Uncut New England Forest

1994 ◽  
Vol 42 (2) ◽  
pp. 206-215 ◽  
Author(s):  
Daniel H. Mann ◽  
F.Brett Engstrom ◽  
Jill L. Bubier
Keyword(s):  
New England ◽  
Fire History ◽  
Fire Frequency ◽  
Tree Age ◽  
Fuel Load ◽  
Summer Drought ◽  
Climate History ◽  
Fire Scar ◽  
15Th Century ◽  
Dead Trees

AbstractFire and forest histories in a hemlock-pine forest in Vermont have been reconstructed by dating fire scars and reconstructing the age distributions of living and dead trees. The ages of living red pines, white pines, and hemlocks show that most of the present forest germinated after a series of spatially overlapping fires between A.D. 1790 and 1850. The ages of cross-dated, dead red pines indicate that this was the third major recruitment interval for pines in this forest since ca. A.D. 1450. We interpret the fire scar and tree age data as recording ca. 50-yr intervals of increased fire frequency recurring every 100-200 yr in response to accumulating fuel loads that coincide with summer drought. The historical records of fires and tree ages, together with the present fuel load, suggest that the next interval of stand-regenerating fires is now overdue. Our success in cross-dating the remnants of dead red pines as old as the 15th century A.D. holds promise for extending reconstructions of fire, forest, and climate history in other parts of this tree's range.

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