Historical high-severity fire patches in mixed-conifer forests

被引:25
作者
Yocom-Kent, Larissa L. [1 ]
Fule, Peter Z. [1 ]
Bunn, Windy A. [2 ]
Gdula, Eric G. [2 ]
机构
[1] No Arizona Univ, Sch Forestry, Flagstaff, AZ 86011 USA
[2] Grand Canyon Natl Pk, Natl Pk Serv, Grand Canyon, AZ 86023 USA
关键词
dendrochronology; fire history; Grand Canyon; Kaibab Plateau; mixed conifer; quaking aspen; CANYON-NATIONAL-PARK; PONDEROSA PINE FORESTS; UPPER MONTANE FORESTS; STAND-REPLACING FIRE; COLORADO FRONT RANGE; GRAND-CANYON; NORTH RIM; TREE RECRUITMENT; MOUNTAIN-RANGE; AGE STRUCTURE;
D O I
10.1139/cjfr-2015-0128
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Two ends of the fire regime spectrum are a frequent low-intensity fire regime and an infrequent high-intensity fire regime, but intermediate fire regimes combine high-and low-severity fire over space and time. We used fire-scar and tree-age data to reconstruct fire regime attributes of mixed-conifer and aspen forests in the North Rim area of Grand Canyon National Park, with a goal of estimating patch sizes of historical high-severity fire and comparing them with modern patch sizes. We used three methods based on (i) aspen groves, (ii) even-aged stands, and (iii) inverse distance weighting, to estimate occurrence and patch sizes of historical high-severity fire. Evidence of high-severity fire was common in the 1800s, and high-severity fire years were associated with drought. High-severity fire patch sizes likely ranged from 10(-1) to 10(2) ha. However, the forest is quite young, and we cannot rule out a historical large high-severity fire that could have reinitiated much of the 1400 ha study area. Fire scars, which are indicative of low-severity fire, were also common. Historical fire was likely heterogeneous across the landscape. Maintaining heterogeneity of fire severity, size, and frequency would promote heterogeneity of forest structure and composition and resilience to future disturbances.
引用
收藏
页码:1587 / 1596
页数:10
相关论文
共 51 条
[41]   Spatial and temporal variation in historic fire regimes in subalpine forests across the Colorado Front Range in Rocky Mountain National Park, Colorado, USA [J].
Sibold, JS ;
Veblen, TT ;
González, ME .
JOURNAL OF BIOGEOGRAPHY, 2006, 33 (04) :631-647
[42]  
Stokes M.A., 1968, Tree-Ring Dating, DOI DOI 10.1038/268402B0
[43]  
Swetnam TW, 1999, ECOL APPL, V9, P1189, DOI 10.1890/1051-0761(1999)009[1189:AHEUTP]2.0.CO
[44]  
2
[45]  
Touchan R., 1996, General Technical Report - Rocky Mountain Forest and Range Experiment Station, USDA Forest Service, P33
[46]   EFFECTS OF FIRE ON LANDSCAPE HETEROGENEITY IN YELLOWSTONE-NATIONAL-PARK, WYOMING [J].
TURNER, MG ;
HARGROVE, WW ;
GARDNER, RH ;
ROMME, WH .
JOURNAL OF VEGETATION SCIENCE, 1994, 5 (05) :731-742
[47]   Post-1935 changes in forest vegetation of Grand Canyon National Park, Arizona, USA: Part 1-ponderosa pine forest [J].
Vankat, John L. .
FOREST ECOLOGY AND MANAGEMENT, 2011, 261 (03) :309-325
[48]   Late Glacial and Holocene vegetation history and paleoclimate of the Kaibab Plateau, Arizona [J].
Weng, CY ;
Jackson, ST .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 1999, 153 (1-4) :179-201
[49]   PRESETTLEMENT REGENERATION PATTERNS IN A SOUTHWESTERN PONDEROSA PINE STAND [J].
WHITE, AS .
ECOLOGY, 1985, 66 (02) :589-594
[50]   MIDDLE AND HIGH-ELEVATION CONIFEROUS FOREST COMMUNITIES OF THE NORTH RIM REGION OF GRAND-CANYON NATIONAL-PARK, ARIZONA, USA [J].
WHITE, MA ;
VANKAT, JL .
VEGETATIO, 1993, 109 (02) :161-174