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Wilderness Visitors and Recreation Impacts: Baseline Data Available for Twentieth Century Conditions
United States Department of Agriculture Wilderness Visitors and Forest Service Recreation Impacts: Baseline Rocky Mountain Research Station Data Available for Twentieth General Technical Report RMRS-GTR-117 Century Conditions September 2003 David N. Cole Vita Wright Abstract __________________________________________ Cole, David N.; Wright, Vita. 2003. Wilderness visitors and recreation impacts: baseline data available for twentieth century conditions. Gen. Tech. Rep. RMRS-GTR-117. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 52 p. This report provides an assessment and compilation of recreation-related monitoring data sources across the National Wilderness Preservation System (NWPS). Telephone interviews with managers of all units of the NWPS and a literature search were conducted to locate studies that provide campsite impact data, trail impact data, and information about visitor characteristics. Of the 628 wildernesses that comprised the NWPS in January 2000, 51 percent had baseline campsite data, 9 percent had trail condition data and 24 percent had data on visitor characteristics. Wildernesses managed by the Forest Service and National Park Service were much more likely to have data than wildernesses managed by the Bureau of Land Management and Fish and Wildlife Service. Both unpublished data collected by the management agencies and data published in reports are included. Extensive appendices provide detailed information about available data for every study that we located. These have been organized by wilderness so that it is easy to locate all the information available for each wilderness in the NWPS. Keywords: campsite condition, monitoring, National Wilderness Preservation System, trail condition, visitor characteristics The Authors _______________________________________ David N. -
Basal Control of Supraglacial Meltwater Catchments on the Greenland Ice Sheet
The Cryosphere, 12, 3383–3407, 2018 https://doi.org/10.5194/tc-12-3383-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Basal control of supraglacial meltwater catchments on the Greenland Ice Sheet Josh Crozier1, Leif Karlstrom1, and Kang Yang2,3 1University of Oregon Department of Earth Sciences, Eugene, Oregon, USA 2School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China 3Joint Center for Global Change Studies, Beijing 100875, China Correspondence: Josh Crozier ([email protected]) Received: 5 April 2018 – Discussion started: 17 May 2018 Revised: 13 October 2018 – Accepted: 15 October 2018 – Published: 29 October 2018 Abstract. Ice surface topography controls the routing of sur- sliding regimes. Predicted changes to subglacial hydraulic face meltwater generated in the ablation zones of glaciers and flow pathways directly caused by changing ice surface to- ice sheets. Meltwater routing is a direct source of ice mass pography are subtle, but temporal changes in basal sliding or loss as well as a primary influence on subglacial hydrology ice thickness have potentially significant influences on IDC and basal sliding of the ice sheet. Although the processes spatial distribution. We suggest that changes to IDC size and that determine ice sheet topography at the largest scales are number density could affect subglacial hydrology primarily known, controls on the topographic features that influence by dispersing the englacial–subglacial input of surface melt- meltwater routing at supraglacial internally drained catch- water. ment (IDC) scales ( < 10s of km) are less well constrained. Here we examine the effects of two processes on ice sheet surface topography: transfer of bed topography to the surface of flowing ice and thermal–fluvial erosion by supraglacial 1 Introduction meltwater streams. -
Life History Traits for Common Blue Mountains Conifer Trees 1
WHITE PAPER F14-SO-WP-SILV-42 Life History Traits for Common Blue Mountains Conifer Trees 1 David C. Powell; Forest Silviculturist Supervisor’s Office; Pendleton, OR Initial Version: OCTOBER 2004 Most Recent Revision: MARCH 2017 INTRODUCTION There are two basic philosophies with respect to plant succession – one is based on popula- tion or community dynamics, and the other is rooted in interactions between individual plants or species (Huston and Smith 1987). A community-based model shares many similarities with a relay floristics pattern of plant succession; an individual-based model has much in common with initial floristics (Powell 2000, pages 26-30, provides a discussion about relay and initial floristics). A community model was favored early in the 20th century, an era when mutualism and in- ter-species dependence were being emphasized in plant ecology. Beginning with the latter half of the 20th century, succession has been viewed primarily as a plant-by-plant or species-by-spe- cies replacement process, and dynamics of plant succession are understandable in those terms. If we assume that succession, a species-by-species replacement process, is controlled by the life history characteristics of plants making up a community, then understanding these charac- teristics will help us grasp how succession might progress. Forest succession, for example, is controlled largely by five traits (life history characteristics) influencing competition among trees: growth rate, size, longevity, rate of seedling establish- ment, and shade tolerance. These traits have an important bearing on a tree species’ capability to compete for site resources collectively referred to as growing space. -
Interpreting Landscape Change in High Mountains of Northeastern Oregon from Long-Term Repeat Photography
United States Department of Interpreting Landscape Change in High Agriculture Forest Service Mountains of Northeastern Oregon from Pacific Northwest Research Station Long-Term Repeat Photography General Technical Report Jon M. Skovlin, Gerald S. Strickler, Jesse L. Peterson, PNW-GTR-505 May 2001 and Arthur W. Sampson Photo by Harley Richardson 1920 Photo by David Jensen 1992 Authors Jon M. Skovlin (retired) was a principal research scientist, Forestry and Range Sciences Laboratory, 1401 Gekeler Lane, La Grande, OR 97850. He now is a consultant on renewable natural resources, P.O. Box 121, Cove, OR 97824. Gerald S. Strickler (deceased) was a range scientist, Forestry and Range Sciences Laboratory, 1401 Gekeler Lane, La Grande, OR 97850. Jesse L. Peterson (deceased) was range examiner, Wallowa National Forest, Wallowa, OR, and later chief range examiner, Whitman National Forest, Baker City, OR. Arthur W. Sampson (deceased) was the pioneer range scientist, U.S. Department of Agriculture, Forest Service, and later Professor of Forestry, University of California, Berkeley, CA. This publication was prepared under contract with the Blue Mountains Natural Resources Institute, La Grande, OR. All photos not otherwise credited were taken by the senior author. Cover Photos Glacier Peak is a satellite point along Eagle Cap Ridge, which is the central watershed feature of the Wallowa Mountain batholith. Upper–This photo of Benson Glacier looking south from Glacier Lake was taken in about 1920. The conspicuous glacier flow lines and crevasses affirm its activity, which had been in recession since about 1870 after the end of the Little Ice Age in about 1850. Harley Richardson captured the Benson Glacier on film when it was in rapid retreat. -
Geomorphic Character, Age and Distribution of Rock Glaciers in the Olympic Mountains, Washington
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington Steven Paul Welter Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Welter, Steven Paul, "Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington" (1987). Dissertations and Theses. Paper 3558. https://doi.org/10.15760/etd.5440 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. For more information, please contact [email protected]. AN ABSTRACT OF THE THESIS OF Steven Paul Welter for the Master of Science in Geography presented August 7, 1987. Title: The Geomorphic Character, Age, and Distribution of Rock Glaciers in the Olympic Mountains, Washington APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true glaciers. Previous reports have identified and briefly described several rock glaciers in the Olympic Mountains, Washington {Long 1975a, pp. 39-41; Nebert 1984), but no detailed integrative study has been made regarding the geomorphic character, age, 2 and distribution of these features. -
Calving Processes and the Dynamics of Calving Glaciers ⁎ Douglas I
Earth-Science Reviews 82 (2007) 143–179 www.elsevier.com/locate/earscirev Calving processes and the dynamics of calving glaciers ⁎ Douglas I. Benn a,b, , Charles R. Warren a, Ruth H. Mottram a a School of Geography and Geosciences, University of St Andrews, KY16 9AL, UK b The University Centre in Svalbard, PO Box 156, N-9171 Longyearbyen, Norway Received 26 October 2006; accepted 13 February 2007 Available online 27 February 2007 Abstract Calving of icebergs is an important component of mass loss from the polar ice sheets and glaciers in many parts of the world. Calving rates can increase dramatically in response to increases in velocity and/or retreat of the glacier margin, with important implications for sea level change. Despite their importance, calving and related dynamic processes are poorly represented in the current generation of ice sheet models. This is largely because understanding the ‘calving problem’ involves several other long-standing problems in glaciology, combined with the difficulties and dangers of field data collection. In this paper, we systematically review different aspects of the calving problem, and outline a new framework for representing calving processes in ice sheet models. We define a hierarchy of calving processes, to distinguish those that exert a fundamental control on the position of the ice margin from more localised processes responsible for individual calving events. The first-order control on calving is the strain rate arising from spatial variations in velocity (particularly sliding speed), which determines the location and depth of surface crevasses. Superimposed on this first-order process are second-order processes that can further erode the ice margin. -
A General Theory of Glacier Surges
Journal of Glaciology A general theory of glacier surges D. I. Benn1, A. C. Fowler2,3, I. Hewitt2 and H. Sevestre1 1School of Geography and Sustainable Development, University of St. Andrews, St. Andrews, KY16 9AL, UK; 2Oxford Centre for Industrial and Applied Mathematics, University of Oxford, Oxford, OX2 6GG, UK and 3Mathematics Paper Applications Consortium for Science and Industry, University of Limerick, Limerick, Ireland Cite this article: Benn DI, Fowler AC, Hewitt I, Sevestre H (2019). A general theory of glacier Abstract surges. Journal of Glaciology 1–16. https:// We present the first general theory of glacier surging that includes both temperate and polythermal doi.org/10.1017/jog.2019.62 glacier surges, based on coupled mass and enthalpy budgets. Enthalpy (in the form of thermal Received: 19 February 2019 energy and water) is gained at the glacier bed from geothermal heating plus frictional heating Revised: 24 July 2019 (expenditure of potential energy) as a consequence of ice flow. Enthalpy losses occur by conduc- Accepted: 29 July 2019 tion and loss of meltwater from the system. Because enthalpy directly impacts flow speeds, mass and enthalpy budgets must simultaneously balance if a glacier is to maintain a steady flow. If not, Keywords: Dynamics; enthalpy balance theory; glacier glaciers undergo out-of-phase mass and enthalpy cycles, manifest as quiescent and surge phases. surge We illustrate the theory using a lumped element model, which parameterizes key thermodynamic and hydrological processes, including surface-to-bed drainage and distributed and channelized Author for correspondence: D. I. Benn, drainage systems. Model output exhibits many of the observed characteristics of polythermal E-mail: [email protected] and temperate glacier surges, including the association of surging behaviour with particular com- binations of climate (precipitation, temperature), geometry (length, slope) and bed properties (hydraulic conductivity). -
Generalized Sliding Law Applied to the Surge Dynamics of Shisper Glacier
https://doi.org/10.5194/tc-2021-96 Preprint. Discussion started: 22 April 2021 c Author(s) 2021. CC BY 4.0 License. Generalized sliding law applied to the surge dynamics of Shisper Glacier and constrained by timeseries correlation of optical satellite images Flavien Beaud1,2, Saif Aati1, Ian Delaney3,4, Surendra Adhikari3, and Jean-Philippe Avouac1 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA 2Now at Department of Geography, University of British Columbia, Vancouver, BC, CA 3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA 4Now at Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland Correspondence: Flavien Beaud (fl[email protected]) Abstract. Understanding fast ice flow is key to assess the future of glaciers. Fast ice flow is controlled by sliding at the bed, yet that sliding is poorly understood. A growing number of studies show that the relationship between sliding and basal shear stress transitions from an initially rate-strengthening behavior to a rate-independent or rate-weakening behavior. Studies that have 5 tested a glacier sliding law with data remain rare. Surging glaciers, as we show in this study, can be used as a natural laboratory to inform sliding laws because a single glacier shows extreme velocity variations at a sub-annual timescale. The present study has two parts: (1) we introduce a new workflow to produce velocity maps with a high spatio-temporal resolution from remote sensing data combining Sentinel-2 and Landsat 8 and use the results to describe the recent surge of Shisper glacier, and (2) we present a generalized sliding law and provide a first-order assessment of the sliding-law parameters using the remote sensing 10 dataset. -
GLACIERS Glacial Ice Is One of the Foremost Scenic and Scientific Values of Olympic National Park
OLYMPIC NATIONAL PARK Glaciers MOUNT OLYMPUS GLACIERS Glacial ice is one of the foremost scenic and scientific values of Olympic National Park. There are about sixty glaciers crowning the Olympics peaks; most of them are quite small in contrast to the great rivers of ice in Alaska. The prominent glaciers are those on Mount Olympus covering approximately ten square miles. Beyond the Olympic complex are the glaciers of Mount Carrie, the Bailey Range, Mount Christie, and Mount Anderson. In the company of these glaciers are perpetual snowbanks that have the superficial appearance of glacial ice. Because they are lacking in the criteria below, they are (aerial view) not true glaciers. True glaciers are structurally three layered bodies of frozen water. The top layer is snow; the middle neve, or mixed snow and ice; and the bottom layer is of pure ice, which is quite plastic in nature. Crevasses or deep cracks in the glaciers form as the ice is subjected to uneven flow over alpine terrain. Another structural feature is the bergschrund, which is a prominent crevasse-like opening at the head of the glacier where the ice has been pulled away from the mountain wall. The rate of glacial flow is quite variable, and Olympic glaciers are "slow-moving" in contrast to some in Alaska which occasionally move at the rate of several hundred feet per day for short periods of time. There is no great advance of Olympic glaciers today, but there is not a rapid melting back of the ice either. Forward surges in glacial flow often occur after a number of very heavy winters and cool summers, but such activity has been relatively infrequent with Olympic glaciers in recorded time. -
Mountain Goat Unit Management Plan | Wasatch and Central Mountains
MOUNTAIN GOAT UNIT MANAGEMENT PLAN Wasatch and Central Mountains Lone Peak / Box Elder Peak / Timpanogos / Provo Peak / Nebo August 2019 BOUNDARY DESCRIPTIONS Lone Peak – Salt Lake County: Boundary begins at the junction of I-15 and I-80 in Salt Lake City; east on I-80 to the Salt Lake-Summit county line; south along this county line to the Salt Lake-Wasatch county line; southwest along this county line to the Salt Lake-Utah county line; southwest along this county line to I-15; north on I-15 to I-80 in Salt Lake City. Box Elder Peak – Utah County: Boundary begins at I-15 and the Salt Lake-Utah county line; east along this county line to the Utah-Wasatch county line; south along this county line to “Pole Line Pass” on the Snake Creek-North Fork American Fork Canyon road; west on this road to SR-92; west on SR-92 to I-15; north on I-15 to the Salt Lake-Utah county line. Timpanogos – Utah County: Boundary begins at the junction of SR-92 and SR-146; southeast on SR-92 to US-189; southwest on US-189 to SR-52; west on SR-52 to US-89; north on US-89 to SR-146; north on SR-146 to SR-92. Provo Peak – Utah County: Boundary begins at the junction of I-15 and US-6 at Spanish Fork; north on I-15 to SR-52; east on SR-52 to US-189; northeast on US-189 to the South Fork Drainage of Provo Canyon; east along this drainage bottom to the Berryport trail; south along this trail to the Left Fork of Hobble Creek road; south on this road to the Right Fork of Hobble Creek road; east on this road to Cedar Canyon; south along this canyon bottom to Wanrhodes Canyon; south along this canyon bottom to Diamond Fork Creek; southwest along this creek to US-6; northeast on US-6 to I-15. -
Seattle the Potential for More Depth and Richness Than Any Other Culture I Can Think Of
WWW.MOUNTAINEERS.ORG ANNUAL REPORT SPECIAL EDITION SPRING 2016 • VOLUME 110 • NO. 2 MountaineerEXPLORE • LEARN • CONSERVE The Doug Walker I Knew PAGE 12 Your Go-To Adventure Buddy PAGE 16 Leading the Way - Annual Report PAGES 19 - 40 Rescue on Dome Peak PAGE 41 2 mountaineer » spring 2016 tableofcontents Spring 2016 » Volume 110 » Number 2 Annual Report The Mountaineers enriches lives and communities by helping people explore, conserve, learn about and enjoy 19 Leading the Way the lands and waters of the Pacific Northwest and beyond. The Mountaineers Annual Report 2015 Features 12 The Doug Walker I knew a special tribute by Glenn Nelson 16 Your Go-To Adventure Buddy an interview with Andre Gougisha 41 Rescue on Dome Peak Everett Mountaineers save the day 16 Columns 6 PEAK FITNESS reducing knee pain 7 MEMBER HIGHLIGHT Tom Vogl 8 OUTDOOR EDUCATION from camper to pioneer 10 SAFETY FIRST VHF radios and sea kayaking 14 CONSERVATION CURRENTS our four conservation priorities 46 RETRO REWIND Wolf Bauer - a wonderful life 50 BRANCHING OUT your guide to the seven branches 52 GO GUIDE activities and courses listing 60 OFF BELAY 41 celebrating lives of cherished members 63 LAST WORD explore by Steve Scher Mountaineer magazine would like to thank The Mountaineers Foundation for its financial assistance. The Foundation operates as Discover The Mountaineers a separate organization from The Mountaineers, which has received about one-third of the Foundation’s gifts to various nonprofit If you're thinking of joining — or have joined and aren’t sure where organizations. to start — why not set a date to Meet The Mountaineers? Check the Branching Out section of the magazine for times and locations of Mountaineer uses: informational meetings at each of our seven branches. -
TRAVERSING the BAILEY RANGE Solitude and Scenery on Olympic National Park’S Premier High Route
TRAVERSING THE BAILEY RANGE Solitude and scenery on Olympic National Park’s premier high route By Karl Forsgaard Deep in the northern wilderness of Olympic Na- tional Park, the Bailey Range Traverse crosses high, scenic country with grand views of surrounding river valleys and peaks—including 7,965-foot Mount Olympus. At each end of the traverse you’ll find popular trails – the Sol Duc River, Seven Lakes Basin and High Divide in the west, the Elwha River in the east. Be- tween those trails are several days of cross-country travel, re- quiring route-finding skills and mountaineering skills above and beyond basic backpack- ing. Good rock, snow and ice scrambling skills are essential. Sometimes you have to earn solitude: The Bailey Range Traverse in the Olympics When Bill and I started the is a rigorous combination of off-trail hiking, climbing, and snow-and-ice travel. trip in late July 2002, the up- But the views and loneliness are the payoffs. per Seven Lakes Basin was still mostly snow-covered, but east of Heart Lake earlier, so we were just the second regulations (including party size limits) the High Divide Trail and the Bailey party of the year. We did not see any apply. route above the Hoh had almost en- people on the off-trail part of the Day One: tirely melted out, so we rarely needed route . to use our ice axes (except in a few The traverse route is described Sol Duc River, Deer Lake snowfingers in creek gullies), and we in Climber’s Guide to the Olympic We left Seattle in two cars, took the never needed to use the crampons, Mountains by Olympic Mountain Bainbridge Island ferry and drove to rope or climbing hardware that we Rescue (Mountaineers, 1988) and in Port Angeles.