Wind/Big Horn Basin Plan Technical Memorandum
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Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture
THE UNIVERSITY OF ALABAMA® University Libraries Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture Kyle Cheesbrough – University of Wyoming Jake Edmunds – University of Wyoming Glenn Tootle – University of Tennessee Greg Kerr – University of Wyoming Larry Pochup – University of Wyoming Deposited 10/17/2018 Citation of published version: Cheesbrough, K., Edmunds, J., Tootle, G., Kerr, G., Pochup, L. (2009): Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture. Remote Sensing, 1(4). DOI: https://doi.org/10.3390/rs1040818 © 2009 by the authors; licensee Molecular Diversity Preservation International, Basel, Switzerland. This work is licensed under a Creative Commons Attribution 4.0 International License. Remote Sens. 2009, 1, 818-828; doi:10.3390/rs1040818 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture Kyle Cheesbrough 1, Jake Edmunds 1, Glenn Tootle 2,*, Greg Kerr 1 and Larry Pochop 1 1 University of Wyoming, Department of Civil and Architectural Engineering, 1000 East University Avenue, Laramie, WY 82070, USA; E-Mails: [email protected] (K.C.); [email protected] (J.E.); [email protected] (G.K.); [email protected] (L.P.) 2 University of Tennessee, Department of Civil and Environmental Engineering, 223 Perkins Hall, Knoxville, TN 37996, USA * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-865-974-7777. Received: 4 September 2009; in revised form: 1 October 2009 / Accepted: 19 October 2009 / Published: 28 October 2009 Abstract: In 2008, Wyoming was ranked 8th in barley production and 20th in hay production in the United States and these crops support Wyoming’s $800 million cattle industry. -
Nordic Hydrology, 25, 1994, 371-388 No Part May Be Reproduced by Any Process Wlthout Complete Rekrence
Nordic Hydrology, 25, 1994, 371-388 No part may be reproduced by any process wlthout complete rekrence Assessment of Spatial Variability of Major-Ion Concentrations and DEL Oxygen-18 Values in Surface Snow, Upper Fremont Glacier, Wyoming, U.S.A. D. L. Naftz U.S. Geological Survey, Salt Lake City, UT 84104, U.S.A. P. F. Schuster and M. M. Reddy U.S. Geological Survey, Boulder, CO 80303, U.S.A. One hundred samples were collected from the surface of the Upper Fremont Glacier at equally spaced intervals defined by an 8,100 m 2 snow grid to assess the significance of lateral variability in major-ion concentrations and del oxy- gen-18 values. For the major ions, the largest concentration range within the snow grid was sodium (0.5056 mgll) and the smallest concentration range was sulfate (0.125 mgll). Del oxygen-18 values showed a range of 7.45 per mil. Comparison of the observed variability of each chemical constituent to the variability expected by measurement error indicated substantial lateral variab- ility within the surface-snow layer. Results of the nested ANOVA indicate most of the variance for every constituent is in the values grouped at the two smaller geographic scales (between 506 m2 and within 506 m2 sections). Cal- cium and sodium concentrations and del oxygen-18 values displayed the largest amount of variance at the largest geographic scale (between 2,025 m 2 sections) within the grid and ranged from 14 to 26 per cent of the total variance. The variance data from the snow grid were used to develop equations to evaluate the significance of both positive and negative concentrationlvalue peaks of nitrate and del oxygen-18 with depth, in a 160 m ice core. -
It Is an Honor to Receive the Kirk Bryan Award. I Am Especially Pleased To
Quaternary Geologist & Geomorphologist Newsletter of the Quaternary Geology and Geomorphology Division http://rock.geosociety.org/qgg Spring 2004 Vol. 45, No.1 Glacial lake that drained from head of Grasshopper Glacier, northern Wind River Range, Wyoming, in October, 2003. View is to west. Lake drained beneath glacier to north, and flooded to north then east down the drainage of Grasshopper Creek, to Down’s Fork Creek, and to Dinwoody Creek. Outwash deposits along the Down’s Fork Creek where an ephemeral lake ponded at Down’s Fork Meadows near the confluence of the Down’s Fork and Dinwoody creeks. Dinwoody Lakes are seen at upper left. View is to east. (More details of this event inside on p. 2) Photos provided by Dennis Dahms, courtesy of Liz Oswald, South Zone Hydrologist, Shoshone National Forest, Lander, Wyoming 1 Cover: Jökulhlaup at Grasshopper Glacier, Wind River Mountains, Wyoming A jökulhlaup, or glacial outburst flood, burst from an ice-dammed lake at the head of the Grasshopper Glacier, Wind River Mountains, Wyoming, in early September this year. The 30-acre lake drained an estimated 850 million gallons of water downslope, underneath the glacier, and, charged with subglacial sediment, flooded tributary valleys and into the Dinwoody River valley. The event was recorded at the USGS gage site (USGS 06221400 Dinwoody Creek above Lakes, near Burris, WY) about 20 mi downstream from the ice-dammed lake. The Grasshopper Glacier is situated at the continental divide nested between high-level erosion surfaces and the eastward-facing cirque walls of the mountain front. The glacier, oriented south to north, drops from an elevation of 12,000 ft down a steep (0.11) slope to its snout at about 11,300 ft elevation. -
Chesseborough Thesis.Pdf
Cheesbrough, Kyle S., Glacial Recession in Wyoming’s Wind River Range , M.S., Department of Civil and Architectural Engineering, December 2007 Abstract The Wind River Range (WRR), located in western Wyoming, is host to more than 60 glaciers making it the largest concentration of glaciers in the Rocky Mountain region. Several studies have been performed on the glaciers of the WRR, dating back to the 1930’s focusing on only the largest, most accessible glaciers such as Gannett and Dinwoody Glaciers. Each of the previous studies have documented the WRR glaciers as being in an overall receding trend since 1850, with some localized periods of advancement (Pochop et al., 1990). This study documents glacial surface area change, volume change and change in terminus position for 42 glacial complexes in the WRR from 1985 through 2005, through utilization of remote sensing techniques. The use of remote sensing techniques allows more of the glaciers in the WRR to be analyzed, rather than focusing on only the most geographically accessible glaciers. In addition to documenting the area changes since 1985 for all of the WRR glaciers, the changes in surface area and terminus position for nine selected glaciers was estimated from 1966 through 2001 using aerial photographs. It has been noted in previous studies that glaciers of smaller area are typically more sensitive to changes in climate than large glaciers (Granshaw & Fountain, 2006). Out of the 42 glacial complexes analyzed, 25 of them had an area of <0.5 km 2 in 1985, while the others were >0.5 km 2 in 1985. -
Glacial Lake Reflectance As a Proxy for Changing Glacial Conditions and Impacts on Streamflow Lance Diangelis
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects January 2018 Glacial Lake Reflectance As A Proxy For Changing Glacial Conditions And Impacts On Streamflow Lance Diangelis Follow this and additional works at: https://commons.und.edu/theses Recommended Citation Diangelis, Lance, "Glacial Lake Reflectance As A Proxy For Changing Glacial Conditions And Impacts On Streamflow" (2018). Theses and Dissertations. 2400. https://commons.und.edu/theses/2400 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. GLACIAL LAKE REFLECTANCE AS A PROXY FOR CHANGING GLACIAL CONDITIONS AND IMPACTS ON STREAMFLOW by Lance Vincent DiAngelis Bachelor of Arts, University of Phoenix, 2011 Master of Science, University of Saint Francis, 2013 A Thesis Submitted to the Graduate Faculty Of the University of North Dakota In partial fulfillment of the requirements For the degree of Master of Science Grand Forks, North Dakota December 2018 PERMISSION Title Glacial Lake Reflectance as a Proxy for Changing Glacial Conditions and Impacts on Streamflow Department Earth System Science and Policy Degree Master of Science In presenting this thesis in partial fulfillment of the requirements for a graduate degree from the University of North Dakota, I agree that the library of this University shall make it freely available for inspection. I further agree that permission for extensive copying for scholarly purposes may be granted by the professor who supervised my thesis work or, in his absence, by the Chairperson of the department or dean of the School of Graduate studies. -
The Fate of Dinwoody Glacier: Present State of Mass Balance and Downstream Impacts of Glacier Runoff
THESIS THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. Submitted by Brooke E. Stamper Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Summer 2018 Master’s Committee: Advisor: Andrew K. Bliss Neil S. Grigg Steven R. Fassnacht Copyright by Brooke E. Stamper 2018 All Rights Reserved ABSTRACT THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. The Wind River Range in Wyoming supports many of the few remaining continental glaciers of the North American Rocky Mountains; the glacier meltwater runoff feeds four major river sys- tems within the U.S. West. Runoff from glaciers affects downstream ecosystems by influencing the quantity, seasonality, and chemistry of the water. We describe the present state of Dinwoody Glacier, the fourth largest glacier in the Wind River Range. We utilize photogrammetry, snow depth measurements, and ablation measurements to characterize surface mass balance for summer of 2017. Localized and nearby stream gauge measurements help to quantify glacial meltwater runoff inputs to Dinwoody Creek. Both of these methods allowed us to put the changes of the Dinwoody Glacier into the broader context of the Missouri River Watershed. If melted, Dinwoody Glacier would no longer provide a reliable source of melt water for thousands of people living in the Missouri River Watershed. Understanding how shrinking glaciers and decreasing melt-water runoff will impact communities and ecosystems downstream is critical for effective environmental management. The response of the Wind River glaciers to future climate is uncertain; however, past research has shown declines in glacial mass, snow cover, snowmelt timing and stream power. -
Glaciers of North America—
Glaciers of North America— GLACIERS OF THE CONTERMINOUS UNITED STATES GLACIERS OF THE WESTERN UNITED STATES By ROBERT M. KRIMMEL With a section on GLACIER RETREAT IN GLACIER NATIONAL PARK, MONTANA By CARL H. KEY, DANIEL B. FAGRE, and RICHARD K. MENICKE SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–2 Glaciers, having a total area of about 580 km2, are found in nine western states of the United States: Washington, Oregon, California, Montana, Wyoming, Colorado, Idaho, Utah, and Nevada. Only the first five states have glaciers large enough to be discerned at the spatial resolution of Landsat MSS images. Since 1850, the area of glaciers in Glacier National Park has decreased by one-third CONTENTS Page Abstract ---------------------------------------------------------------------------- J329 Introduction----------------------------------------------------------------------- 329 Historical Observations -------------------------------------------------------- 330 FIGURE 1. Historical map of a part of the Sierra Nevada, California ------ 331 2. Early map of the glaciers of Mount Rainier, Washington------- 332 Glacier Inventories -------------------------------------------------------------- 332 Mapping of Glaciers------------------------------------------------------------- 333 TABLE 1. Areas of glaciers in the western conterminous United States -- 334 Landsat Images of the Glaciers of the Western United States--------- 335 FIGURE 3. Temporal -
Shoshone National Forest Map Pdf
Shoshone national forest map pdf Continue National Forest in Wyoming, USA Shoshone National ForestFrance Peak is the highest peak in the Absaroka RangeLocation Shoshone National ForestShow map of Wyomingsshawn National Forest (United States)Show map of the U.S.LocationPark, Fremont, Hot Springs, Sublette, and Teton Counties, Wyoming, USNearest CityCody, WYCoordinates4427'52N 109'36'49W / 44.46444'N 109.61361'W/ 44.46444; -109.61361Coordinates: 44'27'52N 109'36'49W / 44.46444'N 109.61361'W / 44.46444; -109.61361 -Area2,466,909 acres (9,983.23 km2) Forest ServiceWebsiteShoshone National Forest Shoshone National Forest (/ʃoʊˈʃoʊniː/shoh-SHOH-nee) is the first federally protected National Forest in the United States and covers nearly 2.5 million acres (1,000,000 hectares) in Wyoming. The forest was originally part of the Yellowstone Timerland Nature Reserve, and is administered by the U.S. Forest Service and was created by an act of Congress and signed by U.S. President Benjamin Harrison in 1891. Shoshone National Forest is one of the first nationally protected land parcels anywhere. Native Americans have lived in the region for at least 10,000 years, and when the region was first explored by European adventurers, the forestlands were occupied by several different tribes. Never largely settled or exploited, the forest retained much of its savagery. The Shoshone National Forest is part of the Great Yellowstone Ecosystem, an almost continuous space of federally protected land covering an estimated 20,000,000 acres (8,100,000 hectares). The Absaroka and Beartut mountains are partly located in the northern part of the forest. -
Ice Core Record of Dust Sources in the Western United States Over the Last 300 Years
Chemical Geology 442 (2016) 160–173 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Ice core record of dust sources in the western United States over the last 300 years S.M. Aarons a,⁎, S.M. Aciego a,P.Gabriellib,c, B. Delmonte d, J.M. Koornneef e, C. Uglietti b,f,A.Wegnerb,g, M.A. Blakowski a, C. Bouman h a Glaciochemistry and Isotope Geochemistry Lab, University of Michigan, 1100 N. University Ave, Ann Arbor, MI 48109, USA b Byrd Polar and Climate Research Center, The Ohio State University, 108 Scott Hall, 1090 Carmack Road, Columbus, OH 43210, USA c School of Earth Sciences, The Ohio State University, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210, USA d Disat, University of Milano-Bicocca, Piazza della Scienza 1, Milan 20126, Italy e Vrije University Amsterdam, de Boelelaan 1085, 1081HV Amsterdam, The Netherlands f Laboratory of Environmental Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland g Stiftung Alfred-Wegener-Institut für Polar- und Meeresforschung, Am Alten Hafen 26, Bremerhaven 27568, Germany h Thermo Fisher Scientific, Hanna-Kunath-Str. 11, Bremen 28199, Germany article info abstract Article history: Over the past ~5000 years, amplified dust generation and deposition in the American West has been linked to Received 22 April 2016 human activity. In recent decades, intensified rates of agriculture and livestock grazing have been correlated Received in revised form 1 July 2016 with greater dust production detected on seasonal to annual timescales. The combination of land use intensifica- Accepted 7 September 2016 tion and climate change (i.e. -
Chlorine-36 in Water, Snow
DOE/I D-22156 CHLORINE-36 IN WATER, SNOW, AND MID-LATITUDE GLACIAL ICE OF NORTH AMERICA: METEORIC AND WEAPONS-TESTS PRODUCTION IN THE VICINITY OF THE IDAHO NATIONAL ENGINEERING AND ENVIRONMENTAL LABORATORY, IDAHO U.S. GEOLOGICAL SURVEY Water Resources Investigations Report 99-4037 Prepared in cooperation with the U.S. DEPARTMENT OF ENERGY science lor a changing world Cover: The Upper Fremont Glacier, Wind River Range, Wyoming, courtesy of Flint Hall, State of Idaho INEEL Oversight Program. Photograph taken from the Lower Fremont Glacier. CHLORINE-36 IN WATER, SNOW, AND MID-LATITUDE GLACIAL ICE OF NORTH AMERICA: METEORIC AND WEAPONS-TESTS PRODUCTION IN THE VICINITY OF THE IDAHO NATIONAL ENGINEERING AND ENVIRONMENTAL LABORATORY, IDAHO By L. DeWayne Cecil and Jaromy R. Green, U.S. Geological Survey, Idaho Falls, Idaho; Stephan Vogt, Purdue University, West Lafayette, Indiana; Shaun K. Frape, University of Waterloo, Ontario, Canada; Stanley N. Davis, University of Arizona, Tucson, Arizona; Gary L. Cottrell, U.S. Geological Survey, Arvada, Colorado; and Pankaj Sharma, Purdue University, West Lafayette, Indiana U.S. GEOLOGICAL SURVEY Water Resources Investigations Report 99-4037 Prepared in cooperation with the U.S. DEPARTMENT OF ENERGY Idaho Falls, Idaho 1999 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not constitute endorsement by the U.S. Government. For additional information -
Late Summer Glacial Meltwater Contributions to Bull Lake Creek Stream Flow and Water Quality, Wind River Range, Wyoming, USA
University of North Dakota UND Scholarly Commons Earth System Science and Policy Faculty Publications Department of Earth System Science and Policy 2-4-2019 Late summer glacial meltwater contributions to Bull Lake Creek stream flow and water quality, Wind River Range, Wyoming, USA Jeffrey VanLooy University of North Dakota, [email protected] Gregory S. Vandeberg University of North Dakota, [email protected] Follow this and additional works at: https://commons.und.edu/essp-fac Part of the Earth Sciences Commons, and the Geography Commons Recommended Citation VanLooy, Jeffrey and Vandeberg, Gregory S., "Late summer glacial meltwater contributions to Bull Lake Creek stream flow and water quality, Wind River Range, Wyoming, USA" (2019). Earth System Science and Policy Faculty Publications. 14. https://commons.und.edu/essp-fac/14 This Article is brought to you for free and open access by the Department of Earth System Science and Policy at UND Scholarly Commons. It has been accepted for inclusion in Earth System Science and Policy Faculty Publications by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. Late summer glacial meltwater contributions to Bull Lake Creek stream flow and water quality, Wind River Range, Wyoming, USA Jeffrey A. VanLooya* and Gregory S. Vandebergb aDepartment of Earth System Science and Policy, University of North Dakota, 4149 University Avenue, Stop 9011, Grand Forks, ND 58202-9011, USA e-mail: [email protected] Phone: 701-777-4755 *corresponding author bDepartment of Geography and GISc., University of North Dakota, 221 Centennial Drive, Stop 9020, Grand Forks, ND 58202-9020, USA e-mail: [email protected] Phone: 701-777-4588 1 Abstract The Wind River Range in Wyoming contains more glacial ice than any other location within the Rocky Mountain States of Colorado, Idaho, Montana, and Wyoming of the United States. -
A 50-Year Record of Nox and SO2 Sources in Precipitation in the Northern Rocky Mountains, USA David L Naftz1*, Paul F Schuster2, Craig a Johnson3
Naftz et al. Geochemical Transactions 2011, 12:4 http://www.geochemicaltransactions.com/content/12/1/4 RESEARCHARTICLE Open Access A 50-year record of NOx and SO2 sources in precipitation in the Northern Rocky Mountains, USA David L Naftz1*, Paul F Schuster2, Craig A Johnson3 Abstract Ice-core samples from Upper Fremont Glacier (UFG), Wyoming, were used as proxy records for the chemical composition of atmospheric deposition. Results of analysis of the ice-core samples for stable isotopes of nitrogen δ15 − δ34 2− − 2− ( N, NO3 ) and sulfur ( S, SO4 ), as well as NO3 and SO4 deposition rates from the late-1940s thru the early-1990s, were used to enhance and extend existing National Atmospheric Deposition Program/National Trends Network (NADP/NTN) data in western Wyoming. The most enriched δ34S value in the UFG ice-core samples coincided with snow deposited during the 1980 eruption of Mt. St. Helens, Washington. The remaining δ34S values were similar to the isotopic composition of coal from southern Wyoming. The δ15N values in ice-core samples representing a similar period of snow deposition were negative, ranging from -5.9 to -3.2 ‰ and all fall within the δ15N values expected from vehicle emissions. Ice-core nitrate and sulfate deposition data reflect the sharply increasing U.S. emissions data from 1950 to the mid-1970s. Introduction expressed as δ34S, were monitored in bulk snowpack The chemical quality of snowfall deposited in high-eleva- samples collected from a network of 52 high-elevation tion areas in the Rocky Mountain region can be affected sites in the Rocky Mountains from 1993 to 1999 [5].