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Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range
Portland State University PDXScholar Environmental Science and Management Faculty Publications and Presentations Environmental Science and Management 3-2016 Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range Megan K. Creutzburg Portland State University, [email protected] Robert M. Scheller Portland State University, [email protected] Melissa S. Lucash Portland State University, [email protected] Louisa B. Evers Bureau of Land Management Stephen D. LeDuc United States Environmental Protection Agency See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/esm_fac Part of the Forest Biology Commons Let us know how access to this document benefits ou.y Citation Details Creutzburg, M. K., Scheller, R. M., Lucash, M. S., Evers, L. B., LeDuc, S. D., & Johnson, M. G. (2015). Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range. GCB Bioenergy. This Article is brought to you for free and open access. It has been accepted for inclusion in Environmental Science and Management Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Megan K. Creutzburg, Robert M. Scheller, Melissa S. Lucash, Louisa B. Evers, Stephen D. LeDuc, and Mark G. Johnson This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/esm_fac/118 GCB Bioenergy (2016) 8, 357–370, doi: 10.1111/gcbb.12255 Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range MEGAN K. CREUTZBURG1 , ROBERT M. SCHELLER1 , MELISSA S. LUCASH1 , LOUISA B. EVERS2 , STEPHEN D. LEDUC3 and MARK G. -
The Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-Huei Chen Jane Kertis Pete Teensma
Forests of the Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-huei Chen Jane Kertis Pete Teensma The Oregon Coast Range supports some of the most dense Ocean, so they are warm and often highly productive, com- and productive forests in North America. In the pre-harvest- pared to the Cascade Range and central Oregon forests. ing period these forests arose as a result of large fires-the Isaac's (1949) site index map shows much more site class I largest covering 330,000 ha (Teensma and others 1991). and I1 land in the Coast Range than in the Cascades. In the These fires occurred mostly at intervals of 150 to 300 years. summers, humid maritime air creates a moisture gradient The natural disturbance regime supported a diverse fauna from the coastal western hemlock-Sitka spruce (Tsuga and large populations of anadromous salmonids (salmon heterophylla-Piceasitchensis) zone with periodic fog extend- and related fish). In contrast, the present disturbance re- ing 4 to 10 km inland, through Douglas-fir (Pseudotsuga gime is dominated by patch clearcuts of about 10-30 ha menziesii var. rnenziesii)-western hemlock forests in the superimposed on most of the forest land with agriculture on central zone to the drier interior-valley foothill zone of the flats near rivers. Ages of most managed forests are less Douglas-fir, bigleaf maple (Acer rnacrophyllum)and Oregon than 60 years. This logging has coincided with significant oak (Quercus garryana). declines in suitable habitat and populations of some fish and wildlife species. Some of these species have been nearly extirpated. -
Global Climate Influencer – Madden Julian Oscillation
MADDEN-JULIAN OSCILLATION GLOBAL CLIMATE INFLUENCER By James Rohman | February 2014 May 17, 2013 October 24, 2013 Figure 1. Following heavy rainfall influenced by the Madden-Julian Oscillation, Typhoon Nari caused substantial flooding along the Mekong and Tonlé Sap Rivers in Cambodia. The flood affected more than 500,000 people, and 300,000 hectares of rice fields were destroyed. The capital city of Phnom Penh (with a population 2.2 million) is marked in the image. Global Climate Influencer | Madden-Julian Oscillation 1 1 IntroductionIntroduction The Madden-Julian Oscillation (MJO) is a slow-moving atmospheric The Madden-Julian Oscillation (MJO) is a slow-moving atmospheric pattern that impacts global tropical and sub-tropical weather. pattern that impacts global tropical and sub-tropical weather. The phenomenon was discovered by Roland Madden and Paul Julian in The phenomenon was discovered by Roland Madden and Paul Julian in 1971. They used ten years of pressure records from Kanton Island and 1971. They used ten years of pressure records from Kanton Island and Singapore to identify a 40-50 day oscillation of zonal wind anomalies in Singapore to identify a 40-50 day oscillation of zonal wind anomalies in the tropical Pacific. the tropical Pacific. Since then, MJO’s recurring pattern of intense rain and thunderstorms Since then, MJO’s recurring pattern of intense rain and thunderstorms followed by an unseasonably dry phase has been identified as occurring followed by an unseasonably dry phase has been identified as occurring every 30-60 days. every 30-60 days. MJO starts in the Indian Ocean as a band of low pressure caused by the MJO starts in the Indian Ocean as a band of low pressure caused by the Indian Ocean Dipole (IOD). -
Mill Creek Watershed Assessment
Yamhill Basin Council Mill Watershed Assessment December 30, 1999 Funding for the Mill Assessment was provided by the Oregon Watershed Enhancement Board and Resource Assistance for Rural Environments. Mill Assessment Project Manager: Robert J. Bower, Principal Author Co-authors: Chris Lupoli, Linfield College intern, for Riparian section and assisted with Wetlands Conditions section. Tamara Quandt, Linfield College intern, for Sensitive Species section. Editors: Melissa Leoni, Yamhill Basin Council, McMinnville, OR Alison Bower, Forest Ecologist, Corvallis, OR Contributors: Bill Ferber, Salem, Water Resources Department (WRD) Chester Novak, Salem, Bureau Land Management (BLM) Dan Upton, Dallas, Willamette Industries David Anderson, Monmouth, Boise Cascade Dean Anderson, Dallas, Polk County Geographical Information Systems (GIS) Dennis Ades, Salem, Department of Environmental Quality (DEQ) Gary Galovich, Corvallis, Oregon Department Fish and Wildlife (ODFW) Mark Koski, Salem, Bureau of Land Management (BLM) Patrick Hawe, Salem, Bureau of Land Management (BLM) Rob Tracey, McMinnville, Natural Resource and Conservation Service (NRCS) Stan Christensen, McMinnville, Yamhill Soil Water Conservation District Susan Maleki, Corvallis, Oregon Watershed Enhancement Board (OWEB) Warren Tausch, Tillamook Bureau of Land Management (BLM) Special Thanks: ! John Cruickshank, Gooseneck Creek resident for his assistance with the Historical, and Channel Modification sections and in the gathering of historical photographs. ! Gooseneck Creek Watershed Group for their support and guidance. ! John Caputo, Yamhill County GIS. ! BLM and Polk County GIS for providing some of the GIS base layers used to create the maps in this assessment. ! USDA Service Center, Natural Resource Conservation Service, McMinnville, for copying and office support. ! Polk and Yamhill Soil and Water Conservation Districts. ! Nick Varnum, PNG Environmental Inc., Tigard, for assisting with the Hydrology and Channel Habitat Typing sections. -
"Preserve Analysis : Saddle Mountain"
PRESERVE ANALYSIS: SADDLE MOUNTAIN Pre pare d by PAUL B. ALABACK ROB ERT E. FRENKE L OREGON NATURAL AREA PRESERVES ADVISORY COMMITTEE to the STATE LAND BOARD Salem. Oregon October, 1978 NATURAL AREA PRESERVES ADVISORY COMMITTEE to the STATE LAND BOARD Robert Straub Nonna Paul us Governor Clay Myers Secretary of State State Treasurer Members Robert Frenkel (Chairman), Corvallis Bill Burley (Vice Chainnan), Siletz Charles Collins, Roseburg Bruce Nolf, Bend Patricia Harris, Eugene Jean L. Siddall, Lake Oswego Ex-Officio Members Bob Maben Wi 11 i am S. Phe 1ps Department of Fish and Wildlife State Forestry Department Peter Bond J. Morris Johnson State Parks and Recreation Branch State System of Higher Education PRESERVE ANALYSIS: SADDLE MOUNTAIN prepared by Paul B. Alaback and Robert E. Frenkel Oregon Natural Area Preserves Advisory Committee to the State Land Board Salem, Oregon October, 1978 ----------- ------- iii PREFACE The purpose of this preserve analysis is to assemble and document the significant natural values of Saddle Mountain State Park to aid in deciding whether to recommend the dedication of a portion of Saddle r10untain State Park as a natural area preserve within the Oregon System of I~atural Areas. Preserve management, agency agreements, and manage ment planning are therefore not a function of this document. Because of the outstanding assemblage of wildflowers, many of which are rare, Saddle r·1ountain has long been a mecca for· botanists. It was from Oregon's botanists that the Committee initially received its first documentation of the natural area values of Saddle Mountain. Several Committee members and others contributed to the report through survey and documentation. -
Atmospheric River Landfall-Latitude Changes in Future Climate Simulations
PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Atmospheric river landfall-latitude changes 10.1002/2016GL070470 in future climate simulations Key Points: Christine A. Shields1 and Jeffrey T. Kiehl1 • Hdeg CCSM4 projects more landfalling winter ARs for Southern 1National Center for Atmospheric Research, Boulder, Colorado, USA California for RCP8.5 scenario due to influences from the subtropical jet • Landfall changes in ARs affecting UK are projected to be seasonally Abstract The latitude of landfall for atmospheric rivers (ARs) is examined in the fully coupled half-degree dependent and influenced primarily version of the Community Climate System Model, version 4 (CCSM4) for warm future climate simulations. by eddy-driven jets fi • Causality of future changes to AR Two regions are examined: U.S. West Coast/North Paci c ARs and United Kingdom/North Atlantic ARs. landfall location differs dynamically Changes in AR landfall-latitude reflect changes in the atmospheric steering flow. West Coast U.S. ARs are between Pacific and Atlantic ARs projected to push equatorward in response to the subtropical jet climate change. UK AR response is dominated by eddy-driven jets and is seasonally dependent. UK simulated AR response is modest in the winter with the largest relative changes occurring in the seasonal transition months. Precipitation associated Correspondence to: with ARs is also projected to increase in intensity under global warming. CCSM4 projects a marked shift to C. A. Shields, higher rainfall rates for Southern California. Small to modest rainfall rates may increase for all UK latitudes, for [email protected] the Pacific Northwest, and central and northern California. Citation: Shields, C. -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
Read Book Pineapple Express : Fun, Colorful Recipes
PINEAPPLE EXPRESS : FUN, COLORFUL RECIPES FROM HAWAII - AMAZING PINEAPPLE RECIPES FOR A FRUITFUL LIFE PDF, EPUB, EBOOK Susan Gray | 82 pages | 14 Oct 2020 | Independently Published | 9798697620229 | English | none Pineapple Express : Fun, Colorful Recipes from Hawaii - Amazing Pineapple Recipes for A Fruitful Life PDF Book Free Return Exchange or money back guarantee for all orders Learn more. Annie books friends. Flagging a list will send it to the Goodreads Customer Care team for review. In the s, Old Tom gin, a style with quite a bit more sweetness than London dry, was just beginning to gain popularity in America. Tags: exotic, pineapple, colorful, tropical, summer, pineapple pattern, yellow, green, fresh, pineapple, pineapple, pineapple express, happiness, philippines, cheer, pulp, juice. By Darra Goldstein. How To Stop Emotional Eating. The Double-Decker River hits These are easier than open tarts because the jam doesn't dry out during baking. Blend almond milk, strawberry and pineapple for a smoothie that's so easy you can make it on busy mornings. No matter the time of year, I love taking advantage seasonal fresh fruit when serving signature cocktails at my clients' weddings. By James J. Easy steps to make bite-size pastries topped with pineapple jam. Pineapple Pork Fried Rice. Tropical Overnight Oats Rating: Unrated. Andrea Fazzari. Tags: pineapple, express, pattern, fruit. For over a week California was hit by record-breaking storm after storm. Searching for alcoholic drink recipes? The salsa also works well with chicken and pork. Tags: james franco, comedy, funny, pineapple express, comedy central, roast, this is the end, freaks and geeks, hot, actor, the interview, pop culture. -
Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 Minute Quadrangles)
(a-0g) R ago (na. 96-53 14. U.S. DEPARTMENT OF THE INTERIOR , U.S. GEOLOGICAL SURVEY Alatzi2/6 (Of (c,c) - R qo rite 6/6-53y Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr.', Alan Niem 2 , Florence L. Wong', Norman S. MacLeod 3, and Tracy K. Calhoun 4 with major contributions by Diane L. Minasian' and Wendy Niem2 Open File Report 96-0534 1996 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1/ U.S. Geological Survey, Menlo Park, CA 94025 2/ Oregon State University, Corvallis, OR 97403 3/ Consultant, Vancouver, WA 98664 4/ U.S. Forest Service, Corvallis, OR 97339 TABLE OF CONTENTS INTRODUCTION 1 GEOLOGIC SKETCH 2 DESCRIPTION OF MAP UNITS SURFICIAL DEPOSITS 7 BEDROCK UNITS Sedimentary and Volcanic Rocks 8 Intrusive Rocks 14 ACKNOWLEDGMENTS 15 REFERENCES CITED 15 MAP SHEETS Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range, scale 1:24,000, 2 sheets. Geologic Map of the Cascade Head Area, Northwest Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr., Alan Niem, Florence L. Wong, Norman S. MacLeod, and Tracy K. Calhoun with major contributions by Diane L. Minasian and Wendy Niem INTRODUCTION The geology of the Cascade Head (W.W. -
Meteorological Conditions Associated with Rain-Related Periglacial Debris Flows on Mount Hood, Oregon and Mount Rainier, Washington
AN ABSTRACT OF THE THESIS OF Lauren E. Parker for the degree of Master of Science in Geography presented on June 10, 2009. Title: Meteorological Conditions Associated with Rain-Related Periglacial Debris Flows on Mount Hood, Oregon and Mount Rainier, Washington Abstract approved: _____________________________________________ Anne W. Nolin In November of 2006 an intense rainstorm of tropical origin, known colloquially as the “Pineapple Express,” inundated the Pacific Northwest region of the United States, initiating numerous periglacial debris flows on several of the stratovolcanoes in the Cascade Range of Oregon and Washington. These debris flows rapidly aggrade channels, deposit thick sediments in their path, and severely damage infrastructure. Consequently, this work seeks to understand the potential meteorological triggering mechanisms of these flow events. Here we focus on Mount Hood, Oregon and Mount Rainier, Washington in the investigation of the meteorological conditions associated with rain-related periglacial debris flow events and the variability of these conditions over time. The objectives of this research are to assess the correlation between “Pineapple Express” and “Atmospheric River” events and rain-related debris flows, and to explore the meteorological conditions associated with debris flow events based on 5 parameters: storm track based on geostrophic flow patterns, temperature, precipitation and orographic enhancement, integrated atmospheric moisture transport, and antecedent snow water equivalent (SWE). Dates for the debris flow events for each mountain were linked with corresponding Pineapple Express circulation and Atmospheric River events. Analysis from this work suggests that there is not a strong correlation between the occurrence of debris flows and the occurrence of Pineapple Express or Atmospheric River events as they are presently defined in the literature. -
December 1-4 2007 Meteorological Analysis
December 1-4 2007 Meteorological Analysis By Greg Sinnett DNR Chief Meteorologist December 2007 Storm Event The December 1-3 storms offered nearly every winter season hazard … •Snow •Strong Winds •Heavy Rainfall •Major Flooding •Landslides •Avalanches •High Coastal Surf •Coastal Flooding NWS Seattle, Washington 19 December 2007. 4 pm Sun Very cold Dec 2 Arctic Air Dam Since Friday… Snow and or mixed L Snow and Rain … Variable Snow Amounts 10 pm Sun Dec 2 L 4 am Mon Dec 3 L 10 am Mon Dec 3 L 4 pm Mon Dec 3 24 hours L 10 pm Mon Dec 3 L 4 am Tue Dec 4 L 10 am Tue Dec 4 L 4 pm Tue Dec 4 48 hours L 4 pm Sun Dec 2 Washington L Hawaii Pineapple Express 10 pm Sun Dec 2 Washington L Hawaii Pineapple Express 4 am Mon Dec 3 Washington L Hawaii Pineapple Express 4 pm Mon Dec 3 24 Hr Washington L Hawaii Pineapple Express 10 pm Mon Dec 3 Washington L Hawaii Pineapple Express 1 am Tue Dec 4 Washington L Hawaii Pineapple Express 4 am Tue Dec 4 Washington L Hawaii Pineapple Express 10 am Tue Dec 4 Washington L Hawaii Pineapple Express 4 pm Tue Dec 4 48 Hours Washington L Hawaii Pineapple Express Mauna Kea Weather Center Katrina Storm was an Extra Tropical Cyclone NOT A Hurricane Seattle Radar Estimated Precipitation 9pm Friday thru 2pm Tuesday Radar Blocked 89 hours Portland Radar Estimated Radar Blocked Precipitation 11pm Friday thru 2pm Tuesday 87 hours 4 pm Sun Dec 2 Surface Wind Speeds 60 mph 10 pm Sun Dec 2 Surface Wind Speeds 60 mph 4 am Mon Dec 3 Surface Wind Speeds 60 mph 10 am Mon Dec 3 Winds Along the Beach… 70mph… Gusts to 84+ mph 60 mph 4 pm -
Drainage Basin Morphology in the Central Coast Range of Oregon
AN ABSTRACT OF THE THESIS OF WENDY ADAMS NIEM for the degree of MASTER OF SCIENCE in GEOGRAPHY presented on July 21, 1976 Title: DRAINAGE BASIN MORPHOLOGY IN THE CENTRAL COAST RANGE OF OREGON Abstract approved: Redacted for privacy Dr. James F. Lahey / The four major streams of the central Coast Range of Oregon are: the westward-flowing Siletz and Yaquina Rivers and the eastward-flowing Luckiamute and Marys Rivers. These fifth- and sixth-order streams conform to the laws of drain- age composition of R. E. Horton. The drainage densities and texture ratios calculated for these streams indicate coarse to medium texture compa- rable to basins in the Carboniferous sandstones of the Appalachian Plateau in Pennsylvania. Little variation in the values of these parameters occurs between basins on igneous rook and basins on sedimentary rock. The length of overland flow ranges from approximately i mile to i mile. Two thousand eight hundred twenty-five to 6,140 square feet are necessary to support one foot of channel in the central Coast Range. Maximum elevation in the area is 4,097 feet at Marys Peak which is the highest point in the Oregon Coast Range. The average elevation of summits in the thesis area is ap- proximately 1500 feet. The calculated relief ratios for the Siletz, Yaquina, Marys, and Luckiamute Rivers are compara- ble to relief ratios of streams on the Gulf and Atlantic coastal plains and on the Appalachian Piedmont. Coast Range streams respond quickly to increased rain- fall, and runoff is rapid. The Siletz has the largest an- nual discharge and the highest sustained discharge during the dry summer months.