Intro to Glaciology

Total Page:16

File Type:pdf, Size:1020Kb

Intro to Glaciology Intro to Glaciology Drs. Dan McGrath and Doug MacAyeal CSU/USGS Glacial Seismology School June 12, 2017 Outline • Brief history • The who, what, and where • Glacier mass balance • Glacier flow • Glacier hydrology • Glacial geology • Glacier and ice sheet mass balance; contribution to SLR A long history…. Ice and Glaciers Glaciers and Ice Sheets NASA Earth Observatory Classifying glaciers Thermal Landscape/Size Tidewater glacier Anderson and Anderson, 2010 Cirque Glaciers Valley Glaciers Ice Sheets Ice Caps Ice Shelves Sea Ice Sea ice covers most Sea ice fringes the entire of the Arctic Ocean. continent of Antarctica. Glacier Mass Balance Anderson and Anderson, 2010 Antarcticglaciers.org Glacier mass balance Balance Profiles Local Change in Ice mass thickness discharge with time balance Glacier mass balance Cogley et al., 2011 How do we measure mass balance? W. Colgan The Movement of Glacial Ice The Movement of Glacial Ice Valley Glacier H = 130 m, θ = 5° Ice sheet H =1300 m, θ = 0.5° Ice rheology and Glen’s Flow Law Velocity Discharge Velocity Observations AIS Ice Velocity Ice Streams Winberry et al., 2009 Glacier Hydrology Vena Chu Supraglacial Englacial Basal Hydrology and Ice velocity Bartholomaus et al,. 2015 Bartholomaus et al., 2008 Crevasses Colgan et al., 2016 Tidewater Glaciers Iceberg Calving Benn et al., 2007 Anderson and Anderson, 2010 Luckman et al., 2016 Columbia Glacier, Alaska http://earthobservatory.nasa.gov/Features/WorldOfChange/columbia_glacier.php Tidewater glacier cycle Marine Ice Sheet Instability Cryoseismology Podolskiy and Walter, 2016 Glacial Erosion Glacial Erosional Landscapes Glacial Erosional Landscapes Glacial Erosional Landscapes Depositional Landforms Drumlins Kettle Lakes Ice sheet mass balance from 1992-2011. Shepherd et al., 2013. Regional glacier mass balance from 2003- 2009. Gardner et al., 2013 Pritchard et al., 2009; Nature .
Recommended publications
  • What Glaciers Are Telling Us About Earth's Changing Climate
    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 8, 3475–3491, 2014 www.the-cryosphere-discuss.net/8/3475/2014/ doi:10.5194/tcd-8-3475-2014 TCD © Author(s) 2014. CC Attribution 3.0 License. 8, 3475–3491, 2014 This discussion paper is/has been under review for the journal The Cryosphere (TC). What glaciers are Please refer to the corresponding final paper in TC if available. telling us about Earth’s changing What glaciers are telling us about Earth’s climate changing climate W. Tangborn and M. Mosteller W. Tangborn1 and M. Mosteller2 1HyMet Inc., Vashon Island, WA, USA Title Page 2 Vashon IT, Vashon Island, WA, USA Abstract Introduction Received: 12 June 2014 – Accepted: 24 June 2014 – Published: 1 July 2014 Conclusions References Correspondence to: W. Tangborn ([email protected]) and Tables Figures M. Mosteller ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. J I J I Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion 3475 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD A glacier monitoring system has been developed to systematically observe and docu- ment changes in the size and extent of a representative selection of the world’s 160 000 8, 3475–3491, 2014 mountain glaciers (entitled the PTAAGMB Project). Its purpose is to assess the impact 5 of climate change on human societies by applying an established relationship between What glaciers are glacier ablation and global temperatures. Two sub-systems were developed to accom- telling us about plish this goal: (1) a mass balance model that produces daily and annual glacier bal- Earth’s changing ances using routine meteorological observations, (2) a program that uses Google Maps climate to display satellite images of glaciers and the graphical results produced by the glacier 10 balance model.
    [Show full text]
  • Surface Mass Balance of Davies Dome and Whisky Glacier on James Ross Island, North-Eastern Antarctic Peninsula, Based on Different Volume-Mass Conversion Approaches
    CZECH POLAR REPORTS 9 (1): 1-12, 2019 Surface mass balance of Davies Dome and Whisky Glacier on James Ross Island, north-eastern Antarctic Peninsula, based on different volume-mass conversion approaches Zbyněk Engel1*, Filip Hrbáček2, Kamil Láska2, Daniel Nývlt2, Zdeněk Stachoň2 1Charles University, Faculty of Science, Department of Physical Geography and Geoecology, Albertov 6, 128 43 Praha, Czech Republic 2Masaryk University, Faculty of Science, Department of Geography, Kotlářská 2, 611 37 Brno, Czech Republic Abstract This study presents surface mass balance of two small glaciers on James Ross Island calculated using constant and zonally-variable conversion factors. The density of 500 and 900 kg·m–3 adopted for snow in the accumulation area and ice in the ablation area, respectively, provides lower mass balance values that better fit to the glaciological records from glaciers on Vega Island and South Shetland Islands. The difference be- tween the cumulative surface mass balance values based on constant (1.23 ± 0.44 m w.e.) and zonally-variable density (0.57 ± 0.67 m w.e.) is higher for Whisky Glacier where a total mass gain was observed over the period 2009–2015. The cumulative sur- face mass balance values are 0.46 ± 0.36 and 0.11 ± 0.37 m w.e. for Davies Dome, which experienced lower mass gain over the same period. The conversion approach does not affect much the spatial distribution of surface mass balance on glaciers, equilibrium line altitude and accumulation-area ratio. The pattern of the surface mass balance is almost identical in the ablation zone and very similar in the accumulation zone, where the constant conversion factor yields higher surface mass balance values.
    [Show full text]
  • Mass-Balance Reconstruction for Kahiltna Glacier, Alaska
    Journal of Glaciology (2018), Page 1 of 14 doi: 10.1017/jog.2017.80 © The Author(s) 2018. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. The challenge of monitoring glaciers with extreme altitudinal range: mass-balance reconstruction for Kahiltna Glacier, Alaska JOANNA C. YOUNG,1 ANTHONY ARENDT,1,2 REGINE HOCK,1,3 ERIN PETTIT4 1Geophysical Institute, University of Alaska, Fairbanks, AK, USA 2Applied Physics Laboratory, Polar Science Center, University of Washington, Seattle, WA, USA 3Department of Earth Sciences, Uppsala University, Uppsala, Sweden 4Department of Geosciences, University of Alaska Fairbanks, Fairbanks, AK, USA Correspondence: Joanna C. Young <[email protected]> ABSTRACT. Glaciers spanning large altitudinal ranges often experience different climatic regimes with elevation, creating challenges in acquiring mass-balance and climate observations that represent the entire glacier. We use mixed methods to reconstruct the 1991–2014 mass balance of the Kahiltna Glacier in Alaska, a large (503 km2) glacier with one of the greatest elevation ranges globally (264– 6108 m a.s.l.). We calibrate an enhanced temperature index model to glacier-wide mass balances from repeat laser altimetry and point observations, finding a mean net mass-balance rate of −0.74 − mw.e. a 1(±σ = 0.04, std dev. of the best-performing model simulations). Results are validated against mass changes from NASA’s Gravity Recovery and Climate Experiment (GRACE) satellites, a novel approach at the individual glacier scale.
    [Show full text]
  • A Strategy for Monitoring Glaciers
    COVER PHOTOGRAPH: Glaciers near Mount Shuksan and Nooksack Cirque, Washington. Photograph 86R1-054, taken on September 5, 1986, by the U.S. Geological Survey. A Strategy for Monitoring Glaciers By Andrew G. Fountain, Robert M. Krimme I, and Dennis C. Trabant U.S. GEOLOGICAL SURVEY CIRCULAR 1132 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government U.S. GOVERNMENT PRINTING OFFICE : 1997 Free on application to the U.S. Geological Survey Branch of Information Services Box 25286 Denver, CO 80225-0286 Library of Congress Cataloging-in-Publications Data Fountain, Andrew G. A strategy for monitoring glaciers / by Andrew G. Fountain, Robert M. Krimmel, and Dennis C. Trabant. P. cm. -- (U.S. Geological Survey circular ; 1132) Includes bibliographical references (p. - ). Supt. of Docs. no.: I 19.4/2: 1132 1. Glaciers--United States. I. Krimmel, Robert M. II. Trabant, Dennis. III. Title. IV. Series. GB2415.F68 1997 551.31’2 --dc21 96-51837 CIP ISBN 0-607-86638-l CONTENTS Abstract . ...*..... 1 Introduction . ...* . 1 Goals ...................................................................................................................................................................................... 3 Previous Efforts of the U.S. Geological Survey ...................................................................................................................
    [Show full text]
  • Glacier Mass Balance This Summary Follows the Terminology Proposed by Cogley Et Al
    Summer school in Glaciology, McCarthy 5-15 June 2018 Regine Hock Geophysical Institute, University of Alaska, Fairbanks Glacier Mass Balance This summary follows the terminology proposed by Cogley et al. (2011) 1. Introduction: Definitions and processes Definition: Mass balance is the change in the mass of a glacier, or part of the glacier, over a stated span of time: t . ΔM = ∫ Mdt t1 The term mass budget is a synonym. The span of time is often a year or a season. A seasonal mass balance is nearly always either a winter balance or a summer balance, although other kinds of seasons are appropriate in some climates, such as those of the tropics. The definition of “year” depends on the measurement method€ (see Chap. 4). The mass balance, b, is the sum of accumulation, c, and ablation, a (the ablation is defined here as negative). The symbol, b (for point balances) and B (for glacier-wide balances) has traditionally been used in studies of surface mass balance of valley glaciers. t . b = c + a = ∫ (c+ a)dt t1 Mass balance is often treated as a rate, b dot or B dot. Accumulation Definition: € 1. All processes that add to the mass of the glacier. 2. The mass gained by the operation of any of the processes of sense 1, expressed as a positive number. Components: • Snow fall (usually the most important). • Deposition of hoar (a layer of ice crystals, usually cup-shaped and facetted, formed by vapour transfer (sublimation followed by deposition) within dry snow beneath the snow surface), freezing rain, solid precipitation in forms other than snow (re-sublimation composes 5-10% of the accumulation on Ross Ice Shelf, Antarctica).
    [Show full text]
  • GLACIER MASS-BALANCE MEASUREMENTS a Manual for Field and Office Work O^ O^C
    '' f1 ^^| Geographisches |^ Institut | "| Universitat NHRI Science Report No. 4 VJ Zurich GLACIER MASS-BALANCE MEASUREMENTS A manual for field and office work o^ O^c G. 0strem and M. Brugman NVE NORWEGIAN WATER RESOURCES AND • <j<L • EnvironmenEnvironi t Environnemant ENERGY ADMINISTRATION •^rB Canada Canada PREFACE During the International Hydrological Decade (1965-1975) it was proposed that the hydrology of selected glaciers should be included in National IHD programs, in addition to various other aspects of hydrology. In Scandinavia it was agreed that Denmark should concentrate on low-land hydrology, including ground water; Sweden should emphasize forested basins, including bogs; and Norwegian hydrologists should study alpine hydrology, including glaciers. Representative, basins were then selected in each country, according to this inter-Scandinavian agreement. In Norway, the selected alpine basins did not comprise glaciers, so some of the already observed glaciers were included in the IHD program. In Canada, the Geographical Branch, within the Department of Mines and Technical Surveys, initiated mass-balance studies on selected glaciers along an east-west profile from the National Hydrology Research Institute Rockies to the Coast Mountains. Inland Waters Directorate Canada, and later Norway, felt that glacier field crews and office technicians Conservation and Protection needed written instructions for their work. This would save time at the start of the Environment Canada EHD program, because new activities were planned at several glaciers almost simultaneously. 11 Innovation Boulevard Therefore, a "cookbook" was prepared in Ottawa by Gunnar 0strem and Alan Saskatoon, Saskatchewan Stanley. This first "Manual for Field Work" was printed in the spring of 1966 for Canada S7N 3H5 use during the following field season.
    [Show full text]
  • Glaciers I: Intro, Geology and Mass Balance
    T. Perron – 12.001 – Glaciers 1 Glaciers I: Intro, Geology and Mass Balance I. Why study glaciers? • Role in freshwater budget o Fraction of earth’s water that is fresh (non-saline): 3% o Fraction of earth’s freshwater that is ice: ~2/3 o Fraction of earth’s surface covered by ice: ~8% • Climate records, climate effects & feedbacks: more in climate lecture • Postglacial rebound helps constrain mantle viscosity • Major driver of erosion, sediment transport, and landscape evolution • But how important have glaciers been over Earth’s history? o Over very long timescales, there seems to be a rhythm to glaciations . From geologic evidence: 950 Ma, 750, 650, 450, 350-250, 4-? . Proposed to reflect arrangement of continents (supercontinents promote accumulation of continental ice). But we don’t even have a very good record of this beyond a few hundred Myr, let alone precise climate records o We have better records for more recent intervals . Antarctic glaciation began 25 Ma, Greenland 20Ma, Alaska 7Ma. Major Northern hemisphere glaciations began ~4Myr. And this has been the typical climate state since! . Again, more in climate lecture. For now, suffice to say that glacial periods have dominated recent climate history. We’re in an interglacial, the first major one since ~125 ka. And our interglacial is an anomalously warm one. We must remind ourselves of this when examining landforms today. o What was North America like during glacial conditions? During LGM, we know there were . Extensive ice sheets [PPT] . Alpine glaciers in mountains beyond the ice margin . Large glacially-dammed lakes (Missoula, Bonneville) [PPT] .
    [Show full text]
  • Fifty-Year Record of Glacier Change Reveals Shifting Climate in the Pacific Northwest and Alaska, USA
    Fifty-Year Record of Glacier Change Reveals Shifting Climate in the Pacific Northwest and Alaska, USA Fifty years of U.S. Geological Survey (USGS) research on glacier change shows recent dramatic shrinkage of glaciers in three climatic Alaska regions of the United States. These long periods of record provide Gulkana clues to the climate shifts that may be driving glacier change. Wolverine The USGS Benchmark Glacier Program began in 1957 as a result Canada of research efforts during the International Geophysical Year (Meier and others, 1971). Annual data collection occurs at three glaciers that represent three climatic regions in the United States: Pacific Ocean South Cascade Glacier in the Cascade Mountains of Washington South Cascade State; Wolverine Glacier on the Kenai Peninsula near Anchorage, United States Alaska; and Gulkana Glacier in the interior of Alaska (fig. 1). Figure 1. The Benchmark Glaciers. Glaciers respond to climate changes by thickening and advancing down-valley towards warmer lower altitudes or by thinning and retreating up-valley to higher altitudes. Glaciers average changes in climate over space and time and provide a picture of climate trends in remote mountainous regions. A qualitative method 1928 1959 for observing these changes is through repeat photography—taking photographs from the same position through time (fig. 2). The most direct way to quantitatively observe changes in a glacier is to measure its mass balance: the difference between the amount of snowfall, or accumulation, on the glacier, and the amount of snow and ice that melts and runs off or is lost as icebergs or water vapor, collectively termed ablation (fig.
    [Show full text]
  • Glacier Mass Changes and Their Effect on the Earth System (Sea Level)
    The Earth’s Dynamic Cryosphere and the Earth System Glacier Mass Changes and Their Effect on the Earth System (Sea Level) By Mark B. Dyurgerov1 and Mark F. Meier1 Glaciers are indicators of climate. rate of sea-level change. This contribu- 20 They also have significant impacts on tion from glaciers is likely to increase, 1993–2005 other globally important processes, such not decrease, in the future. The acceler- average: 0.98 mm as sea-level rise, hydrology of mountain- ating rate of the rise in global sea level 15 per annum fed rivers, fresh water inflow to the has important ramifications for human oceans, and even the shape and rotation populations and associated infrastruc- of the Earth. Observational results about ture in low-lying coastal regions, such 1961–2005 change in glacier mass (mass balance) col- as deltas, and atolls in the Pacific Ocean 10 average: lected since the mid-20th century in many (fig. 3). The reduction in volume of glacier 0.58 mm per annum mountain and subpolar regions on Earth ice can also uplift deglacierized land present clear evidence that the volume of areas regionally. the Earth’s glaciers is being reduced, with Glacier mass-balance data (both 5 substantial reductions since the mid-1970s annual and seasonal) can be used to infer seal-level rise, in millimeters and even more rapid loss since the end of climatic variables such as precipitation and the 1980s. The total area of non-ice-sheet temperature. Knowing the spatial distri- Cumulative nonpolar glacier contribution to 0 glaciers globally is newly estimated to be bution of these variables can assist in the 1960 1970 1980 1990 2000 763×103 square kilometers (km2), some- analysis and modeling of climate change, what larger than earlier estimates, because especially important in high-mountain and Year of more accurate information on isolated high-latitude areas, where precipitation glaciers and on ice caps around the periph- data are few and biased (there are fewer Figure 1.
    [Show full text]
  • Half a Century of Measurements of Glaciers on Axel Heiberg Island, Nunavut, Canada J.G
    ARCTIC VOL. 64, NO. 3 (SEPTEMBER 2011) P. 371 – 375 Half a Century of Measurements of Glaciers on Axel Heiberg Island, Nunavut, Canada J.G. COGLEY,1,2 W.P. ADAMS1 and M.A. ECCLESTONE1 (Received 17 November 2010; accepted in revised form 27 February 2011) ABSTRACT. We illustrate the value of longevity in high-latitude glaciological measurement series with results from a programme of research in the Expedition Fiord area of western Axel Heiberg Island that began in 1959. Diverse investi- gations in the decades that followed have focused on subjects such as glacier zonation, the thermal regime of the polythermal White Glacier, and the contrast in evolution of White Glacier (retreating) and the adjacent Thompson Glacier (advancing until recently). Mass-balance monitoring, initiated in 1959, continues to 2011. Measurement series such as these provide invaluable context for understanding climatic change at high northern latitudes, where in-situ information is sparse and lacks historical depth, and where warming is projected to be most pronounced. Key words: glacier mass balance, glacier changes, Axel Heiberg Island RÉSUMÉ. Nous illustrons la valeur de la longévité en ce qui a trait à une série de mesures glaciologiques en haute latitude au moyen des résultats découlant d’un programme de recherche effectué dans la région du fjord Expédition du côté ouest de l’île Axel Heiberg, programme qui a été entrepris en 1959. Diverses enquêtes réalisées au cours des décennies qui ont suivi ont porté sur des sujets tels que la zonation des glaciers, le régime thermique du glacier White et le contraste entourant l’évolution du glacier White (en retrait) et du glacier Thompson adjacent (qui s’avançait jusqu’à tout récemment).
    [Show full text]
  • Geodetic Mass Balance of the South Shetland Islands Ice Caps, Antarctica, from Differencing Tandem-X Dems
    remote sensing Article Geodetic Mass Balance of the South Shetland Islands Ice Caps, Antarctica, from Differencing TanDEM-X DEMs Kaian Shahateet 1,* , Thorsten Seehaus 2 , Francisco Navarro 1 , Christian Sommer 2 and Matthias Braun 2 1 Escuela Técnica Superior de Ingenieros de Telecomunicación, Universidad Politécnica de Madrid, 28040 Madrid, Spain; [email protected] 2 Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, D-91058 Erlangen, Germany; [email protected] (T.S.); [email protected] (C.S.); [email protected] (M.B.) * Correspondence: [email protected] Abstract: Although the glaciers in the Antarctic periphery currently modestly contribute to sea level rise, their contribution is projected to increase substantially until the end of the 21st century. The South Shetland Islands (SSI), located to the north of the Antarctic Peninsula, are lacking a geodetic mass balance calculation for the entire archipelago. We estimated its geodetic mass balance over a 3–4-year period within 2013–2017. Our estimation is based on remotely sensed multispectral and interferometric SAR data covering 96% of the glacierized areas of the islands considered in our study and 73% of the total glacierized area of the SSI archipelago (Elephant, Clarence, and Smith Islands were excluded due to data limitations). Our results show a close to balance, slightly negative average −1 specific mass balance for the whole area of −0.106 ± 0.007 m w.e. a , representing a mass change of −238 ± 12 Mt a−1. These results are consistent with a wider scale geodetic mass balance estimation Citation: Shahateet, K.; Seehaus, T.; and with glaciological mass balance measurements at SSI locations for the same study period.
    [Show full text]
  • 1 Overview 2 Mass Balance Equations
    Aircraft Altimetry and its Application to Glaciology by Anthony Arendt for the UAF Summer School in Glaciology, June 2010 1 Overview Aircraft laser altimetry is a relatively new tool in glaciology that allows us to monitor the evolution of the surface elevation of glaciers and ice sheets. Altimetry flights usually follow a profile along the centerline of a glacier in an effort to characterize the elevation change of an entire basin. Ex- trapolation of elevation changes to broader regions allows for an assessment of glacier contribution to rising sea level. Some of the earliest assessments of the mass balance of the Greenland ice sheet was acquired using the NASA Airborne Topographic Mapping (ATM) laser altimeter (Krabill et al., 1995, 1999, 2000, 2002). The ATM system has also been used to monitor glaciers in Iceland (Garvin and R.S. Williams, 1993), Arctic Canada (Abdalati et al., 2004), Alaska (Arendt et al., 2008) and other regions. Aircraft laser altimetry using small aircraft has also been applied extensively to mountain glacier systems in the Swiss Alps (Favey et al., 1999), the Canadian Rocky Mountains (Hopkinson and Demuth, 2006), Svalbard (Arnold et al., 2006) and Alaska/northwestern Canada (Echelmeyer et al., 1996; Aðalgeirsdóttir et al., 1998; Sapiano et al., 1998; Rabus and Echelmeyer, 1998; Arendt et al., 2002, 2006). This goal of this document is to explain the mass balance equations relevant to elevation change measurements, followed by a description of altimetry technology. It also describes methods for calculating elevation, volume and mass changes from altimetric measurements. 2 Mass Balance Equations The continuity equation illustrates the way in which altimetry measurements of elevation change relate to the surface mass balance h˙ = b − ∇ · q (1) where h˙ is the rate of change of glacier surface elevation, b is the mass balance, and q is the ice flux per unit cross section of the glacier.
    [Show full text]