Fuel Treatment Effectiveness in the Context of Landform, Vegetation, and Large, Wind-Driven Wildfires
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Dynamics and Disturbance in an Old-Growth Forest Remnant In
DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Thesis Submitted to The College of Arts and Sciences of the UNIVERSITY OF DAYTON In Partial Fulfillment of the Requirements for The Degree of Master of Science in Biology By Sean Michael Goins UNIVERSITY OF DAYTON Dayton, Ohio August, 2012 DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Name: Goins, Sean Michael APPROVED BY: __________________________________________ Ryan W. McEwan, Ph.D. Committee Chair Assistant Professor __________________________________________ M. Eric Benbow, Ph.D. Committee Member Assistant Professor __________________________________________ Mark G. Nielsen, Ph.D. Committee Member Associate Professor ii ABSTRACT DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Name: Goins, Sean Michael University of Dayton Advisor: Dr. Ryan W. McEwan Forest communities are dynamic through time, reacting to shifts in disturbance and climate regimes. A widespread community shift has been witnessed in many forests of eastern North America wherein oak (Quercus spp.) populations are decreasing while maple (Acer spp.) populations are increasing. Altered fire regimes over the last century are thought to be the primary driver of oak-to-maple community shifts; however, the influence of other non-equilibrium processes on this community shift remains under- explored. Our study sought to determine the community structure and disturbance history of an old-growth forest remnant in an area of western Ohio where fires were historically uncommon. To determine community structure, abundance of woody species was measured within 32 plots at 4 canopy strata and dendrochronology was used to determine the relative age-structure of the forest. -
Characterization of Fuel Before and After a Single Prescribed Fire in an Appalachian Hardwood Forest • Elizabeth Bucks, Mary A
Characterization of Fuel before and after a Single Prescribed Fire in an Appalachian Hardwood Forest • Elizabeth bucks, Mary A. Arthur, Jessi E. Lyons, and David L. Loftis Improved understanding of how fuel loads and prescribed fire interact in Appalachian hardwood forests can help managers evaluate the impacts of increased use of prescribed fire in the region. The objective of this study was to characterize fuel loads before and after a single late-winter/early spring prescribed fire and after autumn leaf fall. A repeated measures split-plot design was used to examine dead and down fuels by treatment, sampling time, and landscape position. Preburn mean fuel moss was 40.5 Mg/ha with the duff (Oea) comprising the largest component (19.5 Mg/ha; 48%), followed by large (more than 7.6 cm in diameter) downed lags (9.6 Mg/ha; 24%). Fuel mass was similar across landscape positions; however, duff depth was greater on subxeric compared with intermediate and submesic landscape positions. Burning reduced litter mass (0i; P < 0.00]) and duff depth (P = 0.01). Changes in woody fuels (1-, 10-, 100-, and 1,000-hour) and duff mass were not statistically significant. Post—leaf fall fuel masses did not differ from preburn masses. Thus, a single prescribed burn did not accomplish significant fuel reduction. However, significant declines in duff depth and fuel bed continuity may limit the spread of fire beyond leaf fall and increase potential for soil erosion. This study contributes to the dialogue regarding the use of fire in the Appalachian forest region and impacts on fuel loads. -
Old-Growth Forests
Pacific Northwest Research Station NEW FINDINGS ABOUT OLD-GROWTH FORESTS I N S U M M A R Y ot all forests with old trees are scientifically defined for many centuries. Today’s old-growth forests developed as old growth. Among those that are, the variations along multiple pathways with many low-severity and some Nare so striking that multiple definitions of old-growth high-severity disturbances along the way. And, scientists forests are needed, even when the discussion is restricted to are learning, the journey matters—old-growth ecosystems Pacific coast old-growth forests from southwestern Oregon contribute to ecological diversity through every stage of to southwestern British Columbia. forest development. Heterogeneity in the pathways to old- growth forests accounts for many of the differences among Scientists understand the basic structural features of old- old-growth forests. growth forests and have learned much about habitat use of forests by spotted owls and other species. Less known, Complexity does not mean chaos or a lack of pattern. Sci- however, are the character and development of the live and entists from the Pacific Northwest (PNW) Research Station, dead trees and other plants. We are learning much about along with scientists and students from universities, see the structural complexity of these forests and how it leads to some common elements and themes in the many pathways. ecological complexity—which makes possible their famous The new findings suggest we may need to change our strat- biodiversity. For example, we are gaining new insights into egies for conserving and restoring old-growth ecosystems. canopy complexity in old-growth forests. -
Sass Forestecomgt 2018.Pdf
Forest Ecology and Management 419–420 (2018) 31–41 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Lasting legacies of historical clearcutting, wind, and salvage logging on old- T growth Tsuga canadensis-Pinus strobus forests ⁎ Emma M. Sassa, , Anthony W. D'Amatoa, David R. Fosterb a Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT 05405, USA b Harvard Forest, Harvard University, 324 N Main St, Petersham, MA 01366, USA ARTICLE INFO ABSTRACT Keywords: Disturbance events affect forest composition and structure across a range of spatial and temporal scales, and Coarse woody debris subsequent forest development may differ after natural, anthropogenic, or compound disturbances. Following Compound disturbance large, natural disturbances, salvage logging is a common and often controversial management practice in many Forest structure regions of the globe. Yet, while the short-term impacts of salvage logging have been studied in many systems, the Large, infrequent natural disturbance long-term effects remain unclear. We capitalized on over eighty years of data following an old-growth Tsuga Pine-hemlock forests canadensis-Pinus strobus forest in southwestern New Hampshire, USA after the 1938 hurricane, which severely Pit and mound structures damaged forests across much of New England. To our knowledge, this study provides the longest evaluation of salvage logging impacts, and it highlights developmental trajectories for Tsuga canadensis-Pinus strobus forests under a variety of disturbance histories. Specifically, we examined development from an old-growth condition in 1930 through 2016 across three different disturbance histories: (1) clearcut logging prior to the 1938 hurricane with some subsequent damage by the hurricane (“logged”), (2) severe damage from the 1938 hurricane (“hurricane”), and (3) severe damage from the hurricane followed by salvage logging (“salvaged”). -
The Impacts of Increasing Drought on Forest Dynamics, Structure, and Biodiversity in the United States
Global Change Biology (2016) 22, 2329–2352, doi: 10.1111/gcb.13160 SPECIAL FEATURE The impacts of increasing drought on forest dynamics, structure, and biodiversity in the United States JAMES S. CLARK1 , LOUIS IVERSON2 , CHRISTOPHER W. WOODALL3 ,CRAIGD.ALLEN4 , DAVID M. BELL5 , DON C. BRAGG6 , ANTHONY W. D’AMATO7 ,FRANKW.DAVIS8 , MICHELLE H. HERSH9 , INES IBANEZ10, STEPHEN T. JACKSON11, STEPHEN MATTHEWS12, NEIL PEDERSON13, MATTHEW PETERS14,MARKW.SCHWARTZ15, KRISTEN M. WARING16 andNIKLAUS E. ZIMMERMANN17 1Nicholas School of the Environment, Duke University, Durham, NC 27708, USA, 2Forest Service, Northern Research Station 359 Main Road, Delaware, OH 43015, USA, 3Forest Service 1992 Folwell Avenue,Saint Paul, MN 55108, USA, 4U.S. Geological Survey, Fort Collins Science Center Jemez Mountains Field Station, Los Alamos, NM 87544, USA, 5Forest Service, Pacific Northwest Research Station, Corvallis, OR 97331, USA, 6Forest Service, Southern Research Station, Monticello, AR 71656, USA, 7Rubenstein School of Environment and Natural Resources, University of Vermont, 04E Aiken Center, 81 Carrigan Dr., Burlington, VT 05405, USA, 8Bren School of Environmental Science and Management, University of California, Santa Barbara, CA 93106, USA, 9Department of Biology, Sarah Lawrence College, New York, NY 10708, USA, 10School of Natural Resources and Environment, University of Michigan, 2546 Dana Building, Ann Arbor, MI 48109, USA, 11U.S. Geological Survey, Southwest Climate Science Center and Department of Geosciences, University of Arizona, 1064 E. Lowell -
Ecological Insights from Long-Term Research Plots in Tropical and Temperate Forests
Ecological Insights from Long-term Research Plots in Tropical and Temperate Forests Organized Oral Session 40 was co-organized by Amy Wolf, Stuart Davies, and Richard Condit, and held on 6 August 2009 during the 94th ES A Annual Meeting in Albuquerque, New Mexico. An International Network of Forest Research Sites This session was devoted to findings from an international network of long-term forest dynamics plots, providing some of the first comparisons between the tropical and temperate study areas. Whereas most ecologists recognize the importance of long-term research (Callahan 1984, Likens 1989, Magnuson 1990, Hobbie et al. 2003, and others), large-scale projects like this one are rare. The global network of forest dynamics plots has expanded since its origin in the early 1980s, yet research at the plots has remained integrated due to a combination of individual scientists' efforts and institutional commitments from the Center for Tropical Forest Science (CTFS, <www.ctfs.si.edu> of the Smithsonian Tropical Research Institute and the Arnold Arboretum of Harvard University (Hubbell and Foster 1983, Condit 1995). Today, 26 large plots have been established in tropical or subtropical forests of Central and South America, Africa, Asia, and Oceania, along with 8 recently added temperate forest plots. A standard protocol (Condit 1998) is followed at all sites, including the marking, mapping, and measuring of all trees and shrubs with stem diameters >1 cm. Reports October 2009 519 Reports An underlying objective of the ESA session was to illustrate how an understanding of forest dynamics can contribute to long-term strategies of sustainable forest management in a changing global environment. -
The Burdiehouse Burn Valley Park
The Burdiehouse Burn Valley Park Local Nature Reserve Management Plan 2008 – 2018 Revised in 2010 D:\Ranger\My Documents\BBVP\Burdiehouse Burn Valley Park Management Plan 2008\green flag Management plan.doc 1 INDEX PAGE Introduction .................................................................................................................................... 3 SECTION ONE –Site description........................................................................................................... 3 Site maps I, II, III and IV…………………………………………………………………………………………...6-9 1.1 Management plan framework........................................................................................................... 10 SECTION TWO – Our vision ................................................................................................................ 11 SECTION THREE – Aims ..................................................................................................................... 12 3.1 Aims and links with Green Flag criteria ............................................................................................ 12 SECTION FOUR – Surveys .................................................................................................................. 13 4.1 Introduction .................................................................................................................................. 13 4.2 Historical links ................................................................................................................................. -
Silvicultural Activities: Description and Terminology 1
WHITE PAPER F14-SO-WP-SILV-34 Silvicultural Activities: Description and Terminology 1 David C. Powell; Forest Silviculturist Supervisor’s Office; Pendleton, OR Initial Version: JUNE 1992 Most Recent Revision: FEBRUARY 2018 Introduction ........................................................................................................................ 2 Silvicultural systems ............................................................................................................ 2 Age-based silvicultural systems .................................................................................... 2 Even-aged management ............................................................................................... 3 Figure 1 – Three common stand structures ........................................................................... 4 Figure 2 – Clearcutting ............................................................................................................ 5 Figure 3 – Seed-tree and shelterwood cutting ....................................................................... 6 Figure 4 – Windthrow in spruce-fir forest in the northern Blue Mountains .......................... 8 Figure 5 – Examples of overstory removal and understory removal cutting ......................... 9 Uneven-aged management ........................................................................................ 10 Figure 6 – Examples of individual-tree selection cutting in ponderosa pine ....................... 12 Figure 7 – Examples of group selection -
EVALUATING the EFFECTS of CATASTROPHIC WILDFIRE on WATER QUALITY, WHOLE-STREAM METABOLISM and FISH COMMUNITIES Justin K
University of New Mexico UNM Digital Repository Biology ETDs Electronic Theses and Dissertations Spring 4-12-2018 EVALUATING THE EFFECTS OF CATASTROPHIC WILDFIRE ON WATER QUALITY, WHOLE-STREAM METABOLISM AND FISH COMMUNITIES Justin K. Reale Biology Follow this and additional works at: https://digitalrepository.unm.edu/biol_etds Part of the Terrestrial and Aquatic Ecology Commons Recommended Citation Reale, Justin K.. "EVALUATING THE EFFECTS OF CATASTROPHIC WILDFIRE ON WATER QUALITY, WHOLE-STREAM METABOLISM AND FISH COMMUNITIES." (2018). https://digitalrepository.unm.edu/biol_etds/265 This Dissertation is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Biology ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Justin K. Reale Candidate Biology Department This dissertation is approved, and it is acceptable in quality and form for publication: Approved by the Dissertation Committee: Dr. Clifford N. Dahm, Chairperson Dr. David J. Van Horn, Co-Chairperson Dr. Thomas F. Turner Dr. Ricardo González-Pinźon i EVALUATING THE EFFECTS OF CATASTROPHIC WILDFIRE ON WATER QUALITY, WHOLE-STREAM METABOLISM AND FISH COMMUNITIES BY JUSTIN KEVIN REALE B.S., University of New Mexico, 2009 M.S., University of New Mexico, 2016 DISSERTATION Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Biology The University of New Mexico Albuquerque, New Mexico May, 2018 ii ACKNOWLEGEMENTS I would like to express my gratitude to my co-advisors, Drs. Dahm and Van Horn, for their mentoring, teaching and support throughout my dissertation. -
Model Stormwater Management Ordinance MODEL STORMWATER ORDINANCE
State of Illinois Illinois Department of Natural Resources Model Stormwater Management Ordinance MODEL STORMWATER ORDINANCE Illinois Department of Natural Resources Office of Water Resources September 2015 Version 1 Page Left Intentionally Blank Table of Contents Introduction .................................................................................................................... 1 How To Use This Model Ordinance ................................................................................. 1 100.0 PURPOSE AND SCOPE ............................................................................................ 2 101.0 Purpose ............................................................................................................................. 2 102.0 Scope ................................................................................................................................. 3 200.0 ABBREVIATIONS AND DEFINITIONS ....................................................................... 3 201.0 Abbreviations .................................................................................................................... 3 202.0 Definitions ......................................................................................................................... 3 300.0 AUTHORITY AND APPROVALS .............................................................................. 14 400.0 GENERAL PROVISIONS AND JURISDICTION .......................................................... 15 401.0 Regulated Development ............................................................................................ -
Flooding Dynamics in a Large Low-Gradient Alluvial Fan, the Okavango Delta, Botswana, from Analysis and Interpretation of a 30-Year Hydrometric Record
Hydrology and Earth System Sciences, 10, 127–137, 2006 www.copernicus.org/EGU/hess/hess/10/127/ Hydrology and SRef-ID: 1607-7938/hess/2006-10-127 Earth System European Geosciences Union Sciences Flooding dynamics in a large low-gradient alluvial fan, the Okavango Delta, Botswana, from analysis and interpretation of a 30-year hydrometric record P. Wolski and M. Murray-Hudson Harry Oppenheimer Okavango Research Centre, Maun, Botswana Received: 11 August 2005 – Published in Hydrology and Earth System Sciences Discussions: 6 September 2005 Revised: 29 November 2005 – Accepted: 3 January 2006 – Published: 21 February 2006 Abstract. The Okavango Delta is a flood-pulsed wetland, tem, and the flood frequency distribution itself can change, which supports a large tourism industry and the subsistence compared to that at upstream locations (Wolff and Burges, of the local population through the provision of ecosystem 1994). The ecological role of the channel-floodplain interac- services. In order to obtain insight into the influence of var- tion is expressed by the flood pulse concept (Junk et al., 1989; ious environmental factors on flood propagation and distri- Middleton, 1999). According to this concept, floodplain wet- bution in this system, an analysis was undertaken of a 30- lands and riparian ecosystems adjust to, and are maintained, year record of hydrometric data (discharges and water lev- by the pulsing of water, sediment and nutrients that occurs els) from one of the Delta distributaries. The analysis re- during over-bank flow conditions. Odum (1994) addition- vealed that water levels and discharges at any given channel ally identifies flood pulsing at various spatial and temporal site in this distributary are influenced by a complex interplay scales as an energy subsidy to wetland ecosystems, explain- of flood wave and local rainfall inputs, modified by channel- ing in part the high ecological productivity associated with floodplain interactions, in-channel sedimentation and techni- such systems. -
Wildfire Effects on Stream Metabolism: Aquatic Succession Is Mediated by Local Riparian Succession and Stream Geomorphology
Wildfire effects on stream metabolism: Aquatic succession is mediated by local riparian succession and stream geomorphology Emily A. Davis A thesis Submitted in partial fulfillment of the requirements for the degree of Master of Science University of Washington 2015 Committee: Daniel Schindler Christian Torgersen Colden Baxter Charles Simenstad Program Authorized to Offer Degree: School of Aquatic and Fishery Science ©Copyright 2015 Emily A. Davis i University of Washington Wildfire effects on stream metabolism: Aquatic succession is mediated by local riparian succession and stream geomorphology Emily A. Davis Chair of the Supervisory Committee: Dr. Daniel Schindler School of Aquatic and Fishery Science Abstract As climate change shifts and intensifies fire regimes, it is important to understand stream ecosystem responses to fire. How stream metabolism responds remains largely unexplored. We investigated effects of fire severity and watershed geomorphology on stream ecosystem metabolism at multiple spatial scales in an Idaho wilderness watershed. We measured dissolved oxygen, temperature, and irradiance in 18 streams varying in fire history and watershed characteristics in order to model diel oxygen dynamics, from which we estimated rates of production (P) and respiration (R), then used P:R as an index of stream metabolic state. We found that post-fire riparian canopy recovery strongly influenced stream metabolic state. Severely burned streams with dense riparian regrowth were heterotrophic, whereas streams with less canopy recovery were autotrophic. Fire effects on stream metabolic state were highly mediated by watershed geomorphology, with the strongest long-term changes observed in low- order, narrow, steep streams. Effect sizes of fire and watershed geomorphology on stream metabolism changed from fine spatial scale (500-m riparian buffer) to coarse scale (watershed), and were strongest at fine scales.