Mountain Goat Population Modeling, Appendix B
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Ignimbrites to Batholiths Ignimbrites to Batholiths: Integrating Perspectives from Geological, Geophysical, and Geochronological Data
Ignimbrites to batholiths Ignimbrites to batholiths: Integrating perspectives from geological, geophysical, and geochronological data Peter W. Lipman1,* and Olivier Bachmann2 1U.S. Geological Survey, Mail Stop 910, Menlo Park, California 94028, USA 2Institute of Geochemistry and Petrology, ETH Zurich, CH-8092 Zürich, Switzerland ABSTRACT related intrusions cooled and solidified soon shorter. Magma-supply estimates (from ages after zircon crystallization, as magma sup- and volcano-plutonic volumes) yield focused Multistage histories of incremental accu- ply waned. Some researchers interpret these intrusion-assembly rates sufficient to gener- mulation, fractionation, and solidification results as recording pluton assembly in small ate ignimbrite-scale volumes of eruptible during construction of large subvolcanic increments that crystallized rapidly, leading magma, based on published thermal models. magma bodies that remained sufficiently to temporal disconnects between ignimbrite Mid-Tertiary processes of batholith assembly liquid to erupt are recorded by Tertiary eruption and intrusion growth. Alternatively, associated with the SRMVF caused drastic ignimbrites, source calderas, and granitoid crystallization ages of the granitic rocks chemical and physical reconstruction of the intrusions associated with large gravity lows are here inferred to record late solidifica- entire lithosphere, probably accompanied by at the Southern Rocky Mountain volcanic tion, after protracted open-system evolution asthenospheric input. field (SRMVF). Geophysical -
Long-Term Hydrological Response to Forest Harvest During Seasonal Low flow: Potential Implications for Current Forest Practices☆
Science of the Total Environment 730 (2020) 138926 Contents lists available at ScienceDirect Science of the Total Environment journal homepage: www.elsevier.com/locate/scitotenv Review Long-term hydrological response to forest harvest during seasonal low flow: Potential implications for current forest practices☆ Ashley A. Coble a,⁎, Holly Barnard b, Enhao Du c, Sherri Johnson d, Julia Jones e, Elizabeth Keppeler f, Hyojung Kwon g, Timothy E. Link c, Brooke E. Penaluna d, Maryanne Reiter h, Mark River h, Klaus Puettmann g, Joseph Wagenbrenner i a National Council for Air and Stream Improvement, Inc., 227 NW Third St., Corvallis, OR 97330, USA b Department of Geography, Institute of Arctic and Alpine Research University of Colorado, Boulder, CO, USA c College of Natural Resources, University of Idaho, Moscow, ID, USA d USDA Forest Service, Pacific Northwest Research Station, Corvallis, OR, USA e Geography CEOAS, Oregon State University, Corvallis, OR, USA f USDA Forest Service, Pacific Southwest Research Station, Fort Bragg, CA, USA g Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR, USA h Weyerhaeuser Company, Springfield, OR, USA i USDA Forest Service, Pacific Southwest Research Station, Arcata, CA, USA HIGHLIGHTS GRAPHICAL ABSTRACT • Climate-related low flow declines may also be influenced by forest manage- ment. • Few studies describe multi-decade ef- fects of forest management on streamflow. • We assembled catchment studies of long-term effects of harvest (N10 years). • We define 3 periods of expected low flow responses to forest regrowth after harvest. • Decreased low flow was observed years after harvest in 16 of 25 catchments. article info abstract Article history: Seasonal changes in the magnitude and duration of streamflow can have important implications for aquatic spe- Received 24 March 2020 cies, drinking water supplies, and water quality. -
Downloaded 09/27/21 11:47 PM UTC 25.2 METEOROLOGICAL MONOGRAPHS VOLUME 59
CHAPTER 25 PETERS-LIDARD ET AL. 25.1 Chapter 25 100 Years of Progress in Hydrology a b c c CHRISTA D. PETERS-LIDARD, FAISAL HOSSAIN, L. RUBY LEUNG, NATE MCDOWELL, d e f g MATTHEW RODELL, FRANCISCO J. TAPIADOR, F. JOE TURK, AND ANDREW WOOD a Earth Sciences Division, NASA Goddard Space Flight Center, Greenbelt, Maryland b Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington c Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington d Hydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, Maryland e Department of Environmental Sciences, Institute of Environmental Sciences, University of Castilla–La Mancha, Toledo, Spain f Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California g Research Applications Laboratory, National Center for Atmospheric Research, Boulder, Colorado ABSTRACT The focus of this chapter is progress in hydrology for the last 100 years. During this period, we have seen a marked transition from practical engineering hydrology to fundamental developments in hydrologic science, including contributions to Earth system science. The first three sections in this chapter review advances in theory, observations, and hydrologic prediction. Building on this foundation, the growth of global hydrology, land–atmosphere interactions and coupling, ecohydrology, and water management are discussed, as well as a brief summary of emerging challenges and future directions. Although the review attempts -
1976 Bicentennial Mckinley South Buttress Expedition
THE MOUNTAINEER • Cover:Mowich Glacier Art Wolfe The Mountaineer EDITORIAL COMMITTEE Verna Ness, Editor; Herb Belanger, Don Brooks, Garth Ferber. Trudi Ferber, Bill French, Jr., Christa Lewis, Mariann Schmitt, Paul Seeman, Loretta Slater, Roseanne Stukel, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Annual Editor, The Mountaineer, at the address below, before January 15, 1978 for consideration. Photographs should be black and white prints, at least 5 x 7 inches, with caption and photo grapher's name on back. Manuscripts should be typed double· spaced, with at least 1 Y:z inch margins, and include writer's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be returned. Properly identified photographs and graphics will be returnedabout June. Copyright © 1977, The Mountaineers. Entered as second·class matter April8, 1922, at Post Office, Seattle, Washington, under the act of March 3, 1879. Published monthly, except July, when semi-monthly, by The Mountaineers, 719 Pike Street,Seattle, Washington 98101. Subscription price, monthly bulletin and annual, $6.00 per year. ISBN 0-916890-52-X 2 THE MOUNTAINEERS PURPOSES To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanentform the history and tra ditions of thisregion; To preserve by the encouragement of protective legislation or otherwise the natural beauty of NorthwestAmerica; To make expeditions into these regions in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all loversof outdoor life. 0 � . �·' ' :···_I·:_ Red Heather ' J BJ. Packard 3 The Mountaineer At FerryBasin B. -
Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington by R.W. Tabor1 , R.A. Haugerud2, D.B. Booth3, and E.H. Brown4 Prepared in cooperation with the Washington State Department of Natural Resources, Division of Geology and Earth Resources, Olympia, Washington, 98504 OPEN FILE REPORT 94-403 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, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. iu.S.G.S., Menlo Park, California 94025 2U.S.G.S., University of Washington, AJ-20, Seattle, Washington 98195 3SWMD, King County Department of Public Works, Seattle, Washington, 98104 ^Department of Geology, Western Washington University, Bellingham, Washington 98225 INTRODUCTION The Mount Baker 30- by 60-minute quadrangle encompasses rocks and structures that represent the essence of North Cascade geology. The quadrangle is mostly rugged and remote and includes much of the North Cascade National Park and several dedicated Wilderness areas managed by the U.S. Forest Service. Geologic exploration has been slow and difficult. In 1858 George Gibbs (1874) ascended the Skagit River part way to begin the geographic and geologic exploration of the North Cascades. In 1901, Reginald Daly (1912) surveyed the 49th parallel along the Canadian side of the border, and George Smith and Frank Calkins (1904) surveyed the United States' side. Daly's exhaustive report was the first attempt to synthesize what has become an extremely complicated geologic story. -
Geologic Map of Washington - Northwest Quadrant
GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit. -
Spatial and Temporal Shifts in Historic and Future Temperature and Precipitation Patterns Related to Snow Accumulation and Melt Regimes in Alberta, Canada
water Article Spatial and Temporal Shifts in Historic and Future Temperature and Precipitation Patterns Related to Snow Accumulation and Melt Regimes in Alberta, Canada Brandi W. Newton 1,* , Babak Farjad 2 and John F. Orwin 1 1 Airshed and Watershed Stewardship Branch, Resource Stewardship Division, Alberta Environment and Parks, 3535 Research Road NW, Calgary, AB T2L 2K8, Canada; [email protected] 2 Environmental Knowledge and Prediction Branch, Resource Stewardship Division, Alberta Environment and Parks, 3535 Research Road NW, Calgary, AB T2L 2K8, Canada; [email protected] * Correspondence: [email protected] Abstract: Shifts in winter temperature and precipitation patterns can profoundly affect snow accumu- lation and melt regimes. These shifts have varying impacts on local to large-scale hydro-ecological systems and freshwater distribution, especially in cold regions with high hydroclimatic heterogeneity. We evaluate winter climate changes in the six ecozones (Mountains, Foothills, Prairie, Parkland, Boreal, and Taiga) in Alberta, Canada, and identify regions of elevated susceptibility to change. Evaluation of historic trends and future changes in winter climate use high-resolution (~10 km) gridded data for 1950–2017 and projections for the 2050s (2041–2070) and 2080s (2071–2100) under medium (RCP 4.5) and high (RCP 8.5) emissions scenarios. Results indicate continued declines in winter duration and earlier onset of spring above-freezing temperatures from historic through future periods, with greater changes in Prairie and Mountain ecozones, and extremely short or nonexistent winter durations in future climatologies. Decreases in November–April precipitation and a shift from snow to rain Citation: Newton, B.W.; Farjad, B.; Orwin, J.F. -
The Journal of the North Cascades Conservation Council Spring 2011
The Wild CasCades The Journal of The norTh CasCades ConservaTion CounCil Spring 2011 visit www.northcascades.org • americanalps.blogspot.com/ The Wild CasCades • Spring 2011 1 The North CasCades CoNseRvaTioN Council was The Wild CASCades spring 2011 formed in 1957 “To protect and preserve the North Cascades’ scenic, in This issue scientific, recreational, educational, and wilderness values.” Continuing this mission, NCCC keeps government 3 President’s Report — marc Bardsley officials, environmental organizations, 4 It's in the air — John S. edwards and the general public informed about 5 Celebrating crumbling roads in the backcountry — robert Kendall issues affecting the Greater North 7 Swamp Mountain: Perspectives on the Skagit river, source of North- Cascades ecosystem. action is pursued west life, livelihood and quality of life — Tom hammond through legislative, legal, and public participation channels to protect the 9 Massive overbuilding threatens North Fork sky road — rick mcguire lands, waters, plants and wildlife. 10 American alps Challenge, september 24 over the past half century the NCCC 12 A brief history of the Wild Cascades: A call to action — Tom has led or participated in campaigns hammond to create the North Cascades National Park Complex, Glacier Peak Wilder- 14 In memoriam: Conway leovy ness, and other units of the National 15 NCCC joins intervention against Black Canyon hydro proposal — Wilderness System from the W.o. rick mcGuire douglas Wilderness north to the 16 The suiattle lawsuit: why it happened, what is at stake, and what alpine lakes Wilderness, the henry m. comes next — Kevin Geraghty Jackson Wilderness, the Chelan-Saw- 17 Grizzly bear sighting confirmed in the North Cascades last fall — tooth Wilderness, the Wild Sky Wil- mark Yuasa, The Seattle Times derness and others. -
Contribution of Snow-Melt Water to the Streamflow Over the Three-River
remote sensing Article Contribution of Snow-Melt Water to the Streamflow over the Three-River Headwater Region, China Sisi Li 1, Mingliang Liu 2 , Jennifer C. Adam 2,*,† , Huawei Pi 1,†, Fengge Su 3, Dongyue Li 4 , Zhaofei Liu 5 and Zhijun Yao 5 1 Key Research Institute of Yellow River Civilization and Sustainable Development & Collaborative Innovation Center on Yellow River Civilization Jointly Built by Henan Province and Ministry of Education, Henan University, Kaifeng 475001, China; [email protected] (S.L.); [email protected] (H.P.) 2 Department of Civil and Environmental Engineering, Washington State University, Pullman, WA 99164, USA; [email protected] 3 Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; [email protected] 4 Department of Geography, University of California, Los Angeles, CA 90095, USA; [email protected] 5 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; zfl[email protected] (Z.L.); [email protected] (Z.Y.) * Correspondence: [email protected] † These authors contributed equally to this work. Abstract: Snowmelt water is essential to the water resources management over the Three-River Headwater Region (TRHR), where hydrological processes are influenced by snowmelt runoff and sensitive to climate change. The objectives of this study were to analyse the contribution of snowmelt water to the total streamflow (fQ,snow) in the TRHR by applying a snowmelt tracking algorithm and Variable Infiltration Capacity (VIC) model. The ratio of snowfall to precipitation, and the variation of Citation: Li, S.; Liu, M.; Adam, J.C.; the April 1 snow water equivalent (SWE) associated with fQ,snow, were identified to analyse the role Pi, H.; Su, F.; Li, D.; Liu, Z.; Yao, Z. -
Snow Hydrologyhydrology Importanceimportance Ofof Snowsnow Soso What?What?
FieldField MethodsMethods inin SnowSnow HydrologyHydrology ImportanceImportance ofof snowsnow SoSo what?what? The water of the world • Oceans: 97.24 % • Polar Ice: 2.15% • Groundwater: 0.61% • Lakes: 0.17% • Soil moisture: 0.005% • Atmosphere: 0.0001% • Rivers: 0.00001% • * There is a total of 0.78511% of the worlds water that is fresh and not frozen! (not all is available for use, and in fact, very little is useable) • Add: ½ groundwater, lakes, rivers and you have: 0.47501% of the worlds water available for use • • * In some areas, 50% of the surface water is polluted and non-useable. Realistically, we may have only 0.25% available for use. Terrestrial Cryosphere On average, 60% of the Northern Hemisphere has snowcover in midwinter. Over 30% of the Earth’s land surface has seasonal snow. About 10% of the Earth’s surface is covered permanently by snow and ice. Seasonally and permanently frozen soils occur over ~35% of the Earth’s land surface. Spatial extent of frozen and thawed areas vary significantly on daily, seasonal, annually, and interannual time scales. SoSo what?what? A. Effect of snow cover on climate – Albedo-reflectivity (new snow ~0.8-0.9, older snow ~0.5-0.6). Compare this to ice 0.3-0.4, forest 0.03-0.2, and water 0.05- 0.3 Result: blocks incoming radiation from heating the surface so solar radiation is returned to space instead of being retained as heat in the atmosphere. Strong climate effects: – Surface temperature-stay depressed over snow. – Ground temperatures-with low thermal conductivity, snow serves as an insulator and keep vast area of soil unfrozen. -
Snowmelt Timing and Snowmelt Augmentation of Large Peak Flow
PUBLICATIONS Water Resources Research RESEARCH ARTICLE Precipitation-snowmelt timing and snowmelt augmentation 10.1002/2014WR016877 of large peak flow events, western Cascades, Oregon Key Points: Keith Jennings1 and Julia A. Jones1 In extreme rain-on-snow floods, snowmelt continuously augmented 1Geography, CEOAS, Oregon State University, Corvallis, Oregon, USA precipitation Snowpacks seemed saturated and snowmelt was correlated in all snow- Abstract This study tested multiple hydrologic mechanisms to explain snowpack dynamics in extreme covered areas in extreme floods Snowmelt and precipitation pulses rain-on-snow floods, which occur widely in the temperate and polar regions. We examined 26, 10 day were synchronized at hourly to daily large storm events over the period 1992–2012 in the H.J. Andrews Experimental Forest in western Oregon, scales in extreme floods using statistical analyses (regression, ANOVA, and wavelet coherence) of hourly snowmelt lysimeter, air and dewpoint temperature, wind speed, precipitation, and discharge data. All events involved snowpack Supporting Information: outflow, but only seven events had continuous net snowpack outflow, including three of the five top- Supporting Information S1 ranked peak discharge events. Peak discharge was not related to precipitation rate, but it was related to the 10 day sum of precipitation and net snowpack outflow, indicating an increased flood response to con- Correspondence to: J. A. Jones, tinuously melting snowpacks. The two largest peak discharge events in the study had significant wavelet [email protected] coherence at multiple time scales over several days; a distribution of phase differences between precipita- tion and net snowpack outflow at the 12–32 h time scale with a sharp peak at p/2 radians; and strongly Citation: correlated snowpack outflow among lysimeters representing 42% of basin area. -
Chapter 3 Physical Environment
Physical Environment Chapter 3 Roy W. Lowe/USFWS Chapter 5 Chapter 4 Chapter 3 Chapter 2 Chapter 1 Human Biological Physical Management Introduction and Appendices Environment Environment Environment Direction Background Bandon Marsh National Wildlife Refuge Comprehensive Conservation Plan Chapter 3. Physical Environment 3.1 Climate and Climate Change 3.1.1 General Climate Conditions The climate at Bandon Marsh National Wildlife Refuge (NWR) is greatly influenced by the Pacific Ocean on the west and the Coast Range to the east. The Coast Range rises between 2,000 and 3,000 feet (610-914 meters) above sea level in the north and between 3,000 and 4,000 feet (914-1,219 meters) in the southwestern portion of the state with occasional mountain peaks rising an additional 1,000 to 1,500 feet (305-457 meters). The southern Oregon coastal zone is characterized by wet winters, relatively dry summers, and mild temperatures throughout the year. Because of the moderating influence of the Pacific Ocean, extremely high or low temperatures are rare and the annual temperature range is lower here than in any other Oregon climate zone. Precipitation is heavier and more persistent during the winter but regular moisture occurs from rain and fog throughout the year (WRCC 2011a). The area’s heavy precipitation during winter results from moist air masses moving from the Pacific Ocean onto land. The lower elevations along the coast receive annual precipitation of 65 to 90 inches (165-229 centimeters), which can cause flood events if abundant rainfall is consistent for several days. Occasional strong winds (50-70 mph) occur along the coast, usually in advance of winter storms.