The Impact of Disturbance on Carbon Stores and Dynamics in Forests of Coastal Alaska

The Impact of Disturbance on Carbon Stores and Dynamics in Forests of Coastal Alaska PDF Author: Mikhail A. Yatskov
Publisher:
ISBN:
Category : Carbon sequestration
Languages : en
Pages : 223

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Book Description
Changes in climate caused by increased concentrations of carbon dioxide (CO2) in the Earth’s atmosphere have led land and ocean surface temperatures to increase by 0.85°C and sea level to increase by 19 cm relative to preindustrial times. Global climate change will lead to further alterations in mean temperature and precipitation, as well as their extremes that are likely to influence disturbance regimes. Disturbance play an important role in forest dynamics and succession, by influencing forest ecosystems structure and function, reorganizing forests by reducing live and increasing dead matter, and thus affecting ecosystem carbon (C) balances. Under a changing climate disturbances are likely to cause widespread tree mortality across forested landscapes, creating vast amounts of coarse woody debris (CWD) that will emit C to the atmosphere to a degree that regional C balances and future C dynamics are likely to change. C balance of forested regions depends on inputs in form of C sequestered by live components during growth and outputs in form of C emitted from dead components through decomposition and combustion. Live trees in many forest ecosystems represent the largest aboveground C pool and the dynamics of this pool, as controlled by growth and mortality, have been extensively studied. In contrast, few have examined either the post-disturbance fate of CWD C or assessed C storage potential of salvaged biomass despite the occurrence of multiple recent large-scale disturbance events. Biomass and C stores and their uncertainty were estimated in the Temperate and the Boreal ecoregions of Coastal Alaska using the empirical data from the Forest Inventory and Analysis (FIA) program, literature data, and modeling using standard methods employed by the FIA program. The average aboveground woody live (218.9±4.6 Mg/ha) and log (28.1±1.8 Mg/ha) biomass in the Temperate ecoregion were among the lowest in the Pacific Northwest, whereas snag biomass (30.5±1.0 Mg/ha) was among the highest. In the Boreal ecoregion, CWD biomass comprised almost 50% of the regional aboveground woody store (76.7±3.8 Mg/ha) with bark beetle damaged stands containing 82% of the total CWD biomass. In contrast, in the Temperate ecoregion, CWD comprised 20% of the regional aboveground woody store (277.5 ±5.4 Mg/ha) with 76% of total CWD biomass in undisturbed stands. Total C stores estimates in Coastal Alaska ranged between 1523.6 and 1892.8 Tg with the highest contribution from soils and the largest potential reductions in uncertainty related to the tree and soils C pools. The impact of a large-scale spruce bark beetle (SBB) outbreak on aboveground dead wood C dynamics on the Kenai Peninsula was modeled utilizing data from the FIA program and CWD decomposition rate-constants from a chronosequence and decomposition-vectors analysis. Decomposition rate-constants from the chronosequence ranged between -0.015 yr−1 and -0.022 yr−1 for logs and -0.003 yr−1 and +0.002 yr−1 for snags. Decomposition rate-constants from the decomposition-vectors ranged between -0.045 yr−1 and +0.003 yr−1 among decomposition phases and -0.048 yr−1 and +0.006 yr−1 among decay classes. Relative to log generating disturbances those creating snags delayed C flux from CWD to the atmosphere, produced a smaller magnitude C flux, and had the potential to store 10% to 66% more C in a disturbed system over time. The effect of several management strategies ranging from "leave-as-is" to "salvage-and-utilization" on C stores and emissions following SBB outbreak on Kenai Peninsula, Alaska was evaluated. A forest with immediate post-disturbance regeneration reached pre-disturbance C stores faster than one with delayed regeneration. Lack of regeneration, representing a loss of tree cover on the disturbed portion of the landscape, caused a permanent decrease in wood C stores. Among the "salvage-and-utilization" scenarios considered, biomass fuel production with substitution for fossil fuels created the largest long-term C storage assuming the substitution was permanent. Given that reduction in near-term emissions may be a more robust strategy than long-term ones, the "leave-as-is" scenarios may represent the most feasible way to mitigate global climate change following disturbance.

The Impact of Disturbance on Carbon Stores and Dynamics in Forests of Coastal Alaska

The Impact of Disturbance on Carbon Stores and Dynamics in Forests of Coastal Alaska PDF Author: Mikhail A. Yatskov
Publisher:
ISBN:
Category : Carbon sequestration
Languages : en
Pages : 223

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Book Description
Changes in climate caused by increased concentrations of carbon dioxide (CO2) in the Earth’s atmosphere have led land and ocean surface temperatures to increase by 0.85°C and sea level to increase by 19 cm relative to preindustrial times. Global climate change will lead to further alterations in mean temperature and precipitation, as well as their extremes that are likely to influence disturbance regimes. Disturbance play an important role in forest dynamics and succession, by influencing forest ecosystems structure and function, reorganizing forests by reducing live and increasing dead matter, and thus affecting ecosystem carbon (C) balances. Under a changing climate disturbances are likely to cause widespread tree mortality across forested landscapes, creating vast amounts of coarse woody debris (CWD) that will emit C to the atmosphere to a degree that regional C balances and future C dynamics are likely to change. C balance of forested regions depends on inputs in form of C sequestered by live components during growth and outputs in form of C emitted from dead components through decomposition and combustion. Live trees in many forest ecosystems represent the largest aboveground C pool and the dynamics of this pool, as controlled by growth and mortality, have been extensively studied. In contrast, few have examined either the post-disturbance fate of CWD C or assessed C storage potential of salvaged biomass despite the occurrence of multiple recent large-scale disturbance events. Biomass and C stores and their uncertainty were estimated in the Temperate and the Boreal ecoregions of Coastal Alaska using the empirical data from the Forest Inventory and Analysis (FIA) program, literature data, and modeling using standard methods employed by the FIA program. The average aboveground woody live (218.9±4.6 Mg/ha) and log (28.1±1.8 Mg/ha) biomass in the Temperate ecoregion were among the lowest in the Pacific Northwest, whereas snag biomass (30.5±1.0 Mg/ha) was among the highest. In the Boreal ecoregion, CWD biomass comprised almost 50% of the regional aboveground woody store (76.7±3.8 Mg/ha) with bark beetle damaged stands containing 82% of the total CWD biomass. In contrast, in the Temperate ecoregion, CWD comprised 20% of the regional aboveground woody store (277.5 ±5.4 Mg/ha) with 76% of total CWD biomass in undisturbed stands. Total C stores estimates in Coastal Alaska ranged between 1523.6 and 1892.8 Tg with the highest contribution from soils and the largest potential reductions in uncertainty related to the tree and soils C pools. The impact of a large-scale spruce bark beetle (SBB) outbreak on aboveground dead wood C dynamics on the Kenai Peninsula was modeled utilizing data from the FIA program and CWD decomposition rate-constants from a chronosequence and decomposition-vectors analysis. Decomposition rate-constants from the chronosequence ranged between -0.015 yr−1 and -0.022 yr−1 for logs and -0.003 yr−1 and +0.002 yr−1 for snags. Decomposition rate-constants from the decomposition-vectors ranged between -0.045 yr−1 and +0.003 yr−1 among decomposition phases and -0.048 yr−1 and +0.006 yr−1 among decay classes. Relative to log generating disturbances those creating snags delayed C flux from CWD to the atmosphere, produced a smaller magnitude C flux, and had the potential to store 10% to 66% more C in a disturbed system over time. The effect of several management strategies ranging from "leave-as-is" to "salvage-and-utilization" on C stores and emissions following SBB outbreak on Kenai Peninsula, Alaska was evaluated. A forest with immediate post-disturbance regeneration reached pre-disturbance C stores faster than one with delayed regeneration. Lack of regeneration, representing a loss of tree cover on the disturbed portion of the landscape, caused a permanent decrease in wood C stores. Among the "salvage-and-utilization" scenarios considered, biomass fuel production with substitution for fossil fuels created the largest long-term C storage assuming the substitution was permanent. Given that reduction in near-term emissions may be a more robust strategy than long-term ones, the "leave-as-is" scenarios may represent the most feasible way to mitigate global climate change following disturbance.

The Effects of Wind Disturbance on Temperate Rain Forest Structure and Dynamics of Southeast Alaska

The Effects of Wind Disturbance on Temperate Rain Forest Structure and Dynamics of Southeast Alaska PDF Author: Gregory Jay Nowacki
Publisher:
ISBN:
Category : Forest dynamics
Languages : en
Pages : 32

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Book Description
Wind disturbance plays a fundamental role in shaping forest dynamics in southeast Alaska. Recent studies have increased our appreciation for the effects of wind at both large and small scales. Current thinking is that wind disturbance characteristics change over a continuum dependent on landscape features (e.g. exposure, landscape position, topography). Data modeling has revealed the existance of fistinct wind disturbance regimes, grading from exposed landscapes where recurrent, large-scale wind events prevail to wind-protected landscapes where small-scale canopy gaps predominate. Emulating natural disturbances offers a way to design future management plans and silvicultural prescriptions consistent with prevailing ecological conditions.

Colossal Carbon!

Colossal Carbon! PDF Author: John Kirkland
Publisher:
ISBN:
Category : Chugach National Forest
Languages : en
Pages : 5

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Book Description
The Chugach and Tongass National Forests are changing, possibly in response to global warming. Forested areas within Alaska's temperate rain forests are creeping into areas that were previously too cold or too wet. These forests are also becoming denser. As biomass increases, the amount of carbon stored in the forest also increases. Tara Barrett, a research forester with the U.S. Forest Service, Pacific Northwest Research Station, recently measured these changes. She and her colleagues compared Forest Inventory and Analysis survey data collected from 1995 to 2003 with follow-up inventories taken from 2004 to 2010. The comparison showed that carbon mass increased 4.5 percent in live trees in the Chugach. Carbon storage remained about the same in the Tongass; however, tree species there changed slightly. These observed changes in the Chugach and Tongass National Forests may be related to warmer temperatures and higher levels of carbon dioxide in the atmosphere. This research is being used by the U.S. Forest Service and other government agencies to assess the vulnerability of Alaska's forests and to plan for their future. The Chugach National Forest, for example, used it to establish a baseline assessment of carbon stocks in accordance with 2012 forest planning rules.

Alaska's Changing Boreal Forest

Alaska's Changing Boreal Forest PDF Author: F. Stuart Chapin
Publisher: Oxford University Press
ISBN: 019028854X
Category : Science
Languages : en
Pages : 368

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Book Description
The boreal forest is the northern-most woodland biome, whose natural history is rooted in the influence of low temperature and high-latitude. Alaska's boreal forest is now warming as rapidly as the rest of Earth, providing an unprecedented look at how this cold-adapted, fire-prone forest adjusts to change. This volume synthesizes current understanding of the ecology of Alaska's boreal forests and describes their unique features in the context of circumpolar and global patterns. It tells how fire and climate contributed to the biome's current dynamics. As climate warms and permafrost (permanently frozen ground) thaws, the boreal forest may be on the cusp of a major change in state. The editors have gathered a remarkable set of contributors to discuss this swift environmental and biotic transformation. Their chapters cover the properties of the forest, the changes it is undergoing, and the challenges these alterations present to boreal forest managers. In the first section, the reader can absorb the geographic and historical context for understanding the boreal forest. The book then delves into the dynamics of plant and animal communities inhabiting this forest, and the biogeochemical processes that link these organisms. In the last section the authors explore landscape phenomena that operate at larger temporal and spatial scales and integrates the processes described in earlier sections. Much of the research on which this book is based results from the Bonanza Creek Long-Term Ecological Research Program. Here is a synthesis of the substantial literature on Alaska's boreal forest that should be accessible to professional ecologists, students, and the interested public.

THE EFFECTS OF WIND DISTURBANCE ON TEMPERATE RAIN FOREST STRUCTURE AND DYNAMICS OF SOUTHEAST ALASKA... GENERAL TECHNICAL REPORT PNW-GTR-421

THE EFFECTS OF WIND DISTURBANCE ON TEMPERATE RAIN FOREST STRUCTURE AND DYNAMICS OF SOUTHEAST ALASKA... GENERAL TECHNICAL REPORT PNW-GTR-421 PDF Author: United States. Forest Service
Publisher:
ISBN:
Category :
Languages : en
Pages :

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Book Description


Climate Change

Climate Change PDF Author: J. B. Haufler
Publisher: DIANE Publishing
ISBN: 1437933742
Category : Science
Languages : en
Pages : 57

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Book Description
Summarizes potential impacts that are likely from predicted climate change (CC) in Southern Alaska (SA), identifies on-going collaborative efforts directed at climate change, and suggests some possible responses that the Alaska Region (AR) could take to address this challenge. Contents: (1) Intro.; (2) Overview of the AR; (3) Ecosystem Services of the SC and SE Landscapes; (4) CC Threats to Ecosystem Services in Southern Coastal Alaska: Observed Changes in Alaska¿s Climate; Predicted CC in Alaska Climate; (5) Impacts of CC on Ecosystem Services: Changing Sea Levels; Increased Ocean Temp. and Changing Circulation Patterns; Increased Ocean Acidification; Increased Storm Intensities; Changes to Stream Temp. and Flows; Loss of Glaciers; Changes to Wetlands; Forest Temp. and Precipitation Changes; Increases in Invasive Species; (6) Initiatives for CC in Southern Alaska Coastal Landscapes; (7) Strategic Plan for CC. Figures.

Climate, Management, and Forest Type Influences on Carbon Dynamics of West-Coast U.S. Forests

Climate, Management, and Forest Type Influences on Carbon Dynamics of West-Coast U.S. Forests PDF Author: Tara M. Hudiburg
Publisher:
ISBN:
Category : Atmospheric carbon dioxide
Languages : en
Pages : 148

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Book Description
Net uptake of carbon from the atmosphere (net ecosystem production, NEP) is dependent on climate, disturbance history, management practices, forest age, and forest type. To improve understanding of the influence of these factors on forest carbon flux in the western U.S., a combination of federal inventory data and supplemental ground measurements was used to estimate several important components of NEP in forests in Oregon and Northern California during the 1990's. The specific components studied were live and dead biomass stores, net primary productivity (NPP), and mortality. In the semi-arid Northern Basin and mesic Coast Range, mean total biomass was 4 and 24 Kg C m−2, and mean NPP was 0.28 and 0.78 Kg C m−2 y−1, respectively. These values were obtained using species- and ecoregionspecific allometric equations and tended to be higher than those obtained from more generalized approaches. There is strong evidence that stand development patterns of biomass accumulation, net primary production, and mortality differ due to climate (ecoregion), management practices (ownership), and forest type. Among those three factors and across the whole region, maximum NPP and dead biomass stores were most influenced by climate, while maximum live biomass stores and mortality were mostly influenced by forest type. Live and dead biomass, NPP, and mortality were most influenced by forest type. Decrease in NPP with age was not general across ecoregions, with no marked decline in old stands (>200 years) in some ecoregions, and in others, the age at which NPP declined was very high (458 years in East Cascades, 325 in Klamath Mountains, 291 in Sierra Nevada). There is high potential for increasing total carbon storage by increasing rotation age and reducing harvest rates in this region. Only 1% of forest plots on private lands were >200 years old, whereas 41% of the plots were greater than 200 years old on public lands. Total carbon stocks could increase from 3.2 Pg C to 7.3 Pg C and NPP could increase from 0.109 Pg C y−1 to .168 Pg C y−1 (a 35% increase) if forests were managed for maximum carbon storage by increasing rotation age.

Ecosystems of Disturbed Ground

Ecosystems of Disturbed Ground PDF Author: L.R. Walker
Publisher: Elsevier
ISBN: 0080550843
Category : Science
Languages : en
Pages : 881

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Book Description
As the human population inexorably grows, its cumulative impact on the Earth's resources is hard to ignore. The ability of the Earth to support more humans is dependent on the ability of humans to manage natural resources wisely. Because disturbance alters resource levels, effective management requires understanding of the ecology of disturbance. This book is the first to take a global approach to the description of both natural and anthropogenic disturbance regimes that physically impact the ground. Natural disturbances such as erosion, volcanoes, wind, herbivory, flooding and drought plus anthropogenic disturbances such as foresty, grazing, mining, urbanization and military actions are considered. Both disturbance impacts and the biotic recovery are addressed as well as the interactions of different types of disturbance. Other chapters cover processes that are important to the understanding of disturbance of all types including soil processes, nutrient cycles, primary productivity, succession, animal behaviour and competition. Humans react to disturbances by avoiding, exacerbating, or restoring them or by passing environmental legislation. All of these issues are covered in this book.Managers need better predictive models and robust data-collections that help determine both site-specfic and generalized responses to disturbance. Multiple disturbances have a complex effect on both physical and biotic processes as they interact. This book provides a wealth of detail about the process of disturbance and recovery as well as a synthesis of the current state of knowledge about disturbance theory, with extensive documentation.

Changes in Carbon Dynamics Following Wildfire in Soils of Interior Alaska

Changes in Carbon Dynamics Following Wildfire in Soils of Interior Alaska PDF Author: Katherine P. O'Neill
Publisher:
ISBN:
Category : Fire ecology
Languages : en
Pages : 526

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Book Description
"Boreal forests contain large amounts of soil carbon and are susceptible to periodic wildfires. Predicting the response of soil carbon dynamics to fire disturbance requires understanding: (1) the environmental factors governing CO2 efflux; (2) the extent to which fire alters these factors; and, (3) the length of time over which these perturbations persist. In interior Alaska seasonal patterns of CO2 efflux, soil temperature. and soil moisture potential were measured in burned and control pairs of aspen, white spruce, and black spruce stands. Averaged over the growing season, mean CO2 efflux from burned stands (0.51 ± 0.26 g CO2 m−2 hr−1) was two-thirds that of control stands (0.77 ± 0.44 g CO2 M−2 hr1). Soil temperature explained 85 to 90% of the seasonal variability in the control, whereas moisture was a more important determinant in burned stands. Laboratory incubations of recently burned and control humic material indicate that changes in substrate chemistry and increased temperature may enhance rates of decomposition by a factor of 2.2 to 2.8 in the first decade after fire, resulting in a release of 6.3 to 13.4 Mg C ha−1 to the atmosphere. Under saturated moisture conditions, respiration from mosses may contribute 16 to 50% of total soil CO2 emissions. In a 140-year age-sequence of burned black spruce stands, CO2 efflux increased at an average rate of 8.3 kg C ha−1 yr1 up to a maximum of 1.83 Mg C ha−1 yr1. During this same time, accumulation of carbon in organic horizons ranges from 0.34 to 0.50 Mg C ha−1 yr1 and the ratio of microbial to root respiration decreased from 76:24 to 13:87. Numerical modeling of carbon accumulation suggests that these soils functioned as a net source of carbon for the first 7 to 15 years after fire and released 1.8 to 11.0 Mg C ha−1 to the atmosphere. Although conservative, these estimates of post-fire biogenic emissions are on the same order of magnitude as carbon losses during combustion itself, suggesting that current models may underestimate the impact of fire in northern latitudes by as much as a factor of two"--Leaves iv-v.

Climate Change Impacts on Boreal Forest Disturbance Regimes

Climate Change Impacts on Boreal Forest Disturbance Regimes PDF Author:
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 44

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Book Description