scholarly journals Fine-Scale Patchiness in Fuel Load Can Influence Initial Post-Fire Understory Composition in a Mixed Conifer Forest, Sequoia National Park, California

2009 ◽  
Vol 29 (2) ◽  
pp. 126-132 ◽  
Author(s):  
Monique E. Rocca
2015 ◽  
Vol 24 (4) ◽  
pp. 484 ◽  
Author(s):  
Jamie M. Lydersen ◽  
Brandon M. Collins ◽  
Eric E. Knapp ◽  
Gary B. Roller ◽  
Scott Stephens

Although knowledge of surface fuel loads is critical for evaluating potential fire behaviour and effects, their inherent variability makes these difficult to quantify. Several studies relate fuel loads to vegetation type, topography and spectral imaging, but little work has been done examining relationships between forest overstorey variables and surface fuel characteristics on a small scale (<0.05 ha). Within-stand differences in structure and composition would be expected to influence fuel bed characteristics, and thus affect fire behaviour and effects. We used intensive tree and fuel measurements in a fire-excluded Sierra Nevada mixed conifer forest to assess relationships and build predictive models for loads of duff, litter and four size classes of downed woody fuels to overstorey structure and composition. Overstorey variables explained a significant but somewhat small percentage of variation in fuel load, with marginal R2 values for predictive models ranging from 0.16 to 0.29. Canopy cover was a relatively important predictor for all fuel components, although relationships varied with tree species. White fir abundance had a positive relationship with total fine woody fuel load. Greater pine abundance was associated with lower load of fine woody fuels and greater load of litter. Duff load was positively associated with total basal area and negatively associated with oak abundance. Knowledge of relationships contributing to within-stand variation in fuel loads can increase our understanding of fuel accumulation and improve our ability to anticipate fine-scale variability in fire behaviour and effects in heterogeneous mixed species stands.


2016 ◽  
Vol 62 (3) ◽  
pp. 268-280 ◽  
Author(s):  
Kyle C. Rodman ◽  
Andrew J. Sánchez Meador ◽  
David W. Huffman ◽  
Kristen M. Waring

Author(s):  
Cathy Whitlock ◽  
Rosemary Sherriff

The Yellowstone region has been divided into geovegetation regions based on characteristics of the vegetation, climate, and geology (Despain, 1990). The Northern Range or Yellowstone-Lamar valleys features open Douglas-fir parkland, summer­wet conditions, and substrates composed of glacial debris and sedimentary and granitic material. The Central Plateau is an area of lodgepole forest, relatively dry summers, and infertile rhyolite soils. The Absaroka region consists of mixed conifer forest, relatively dry summers, and andesitic and sedimentary rock types. The environmental history of the geovegetation regions, as revealed from a network of pollen and charcoal records, has been equally distinctive (Whitlock, 1993; Whitlock and Bartlein, 1993; Whitlock et al., 1994, 1995). The Northern Range experienced wetter-than-present summers in the early Holocene between 10 and 7 ka (ka = 1000 14C years before present) as a result of intensified monsoonal circulation. The development of Douglas-fir parkland there has occurred with drying in the late Holocene. The paleoecologic record shows few fires in the early Holocene and increased burning in the last 7000 years as the climate became drier (Millspaugh, in prep.). In the Central Plateau, areas of rhyolite supported lodgepole-pine forest for the last 10,000 years with little change. Charcoal data from this region indicate that fires were most frequent in the early Holocene between 10 and 7 ka, when southern and central Yellowstone National Park (YNP) and Grand Teton National Park (GTNP) were warmer and drier than at present. Fire frequency has decreased in the last few millennia with the onset of present-day cool conditions (Millspaugh, in prep.; Whitlock and Millspaugh, in press). Despite these changes in Holocene climate and fire regime the vegetation of the Central Plateau remained a lodgepole pine forest, presumably because of the infertile soils.


2010 ◽  
Vol 259 (5) ◽  
pp. 904-915 ◽  
Author(s):  
Siyan Ma ◽  
Amy Concilio ◽  
Brian Oakley ◽  
Malcolm North ◽  
Jiquan Chen

2008 ◽  
Vol 69 (2) ◽  
pp. 263-275 ◽  
Author(s):  
R. Scott Anderson ◽  
Renata B. Jass ◽  
Jaime L. Toney ◽  
Craig D. Allen ◽  
Luz M. Cisneros-Dozal ◽  
...  

Chihuahueños Bog (2925 m) in the Jemez Mountains of northern New Mexico contains one of the few records of late-glacial and postglacial development of the mixed conifer forest in southwestern North America. The Chihuahueños Bog record extends to over 15,000 cal yr BP. AnArtemisiasteppe, then an openPiceawoodland grew around a small pond until ca. 11,700 cal yr BP whenPinus ponderosabecame established. C/N ratios,δ13C andδ15N values indicate both terrestrial and aquatic organic matter was incorporated into the sediment. Higher percentages of aquatic algae and elevated C/N ratios indicate higher lake levels at the opening of the Holocene, but a wetland developed subsequently as climate warmed. From ca. 8500 to 6400 cal yr BP the pond desiccated in what must have been the driest period of the Holocene there. C/N ratios declined to their lowest Holocene levels, indicating intense decomposition in the sediment. Wetter conditions returned after 6400 cal yr BP, with conversion of the site to a sedge bog as groundwater levels rose. Higher charcoal influx rates after 6400 cal yr BP probably result from greater biomass production rates. Only minor shifts in the overstory species occurred during the Holocene, suggesting that mixed conifer forest dominated throughout the record.


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