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  • 1
    Monograph available for loan
    Monograph available for loan
    New York, NY [u.a.] : Oxford Univ. Press
    Call number: M 98.0528
    Type of Medium: Monograph available for loan
    Pages: xi, 343 S.
    ISBN: 0195069641
    Classification: D.4.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York ; Oxford : Oxford University Press
    Call number: AWI G7-98-0403
    Type of Medium: Monograph available for loan
    Pages: XI, 343 S. : Abb. ; 26 cm
    ISBN: 0195069641
    Branch Library: AWI Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: AWI G7-93-0181/1 ; AWI G7-93-0181/2
    Description / Table of Contents: Contents: Chapter 1 Late Weichselian lce Sheets in Eurasia and Greenland / Bjöm G. Andersen. - NORTHERN EUROPE. - Holland. - Germany. - Denmark. - Sweden. - Finland. - Poland. - Western USSR (including Baltic SSR). - Northwestern USSR. - Norway. - North Sea. - British Isles. - lceland. - SOUTHERN EUROPE. - BARENTS SEA AND ARCTIC ISLANDS. - ASIA. - GREENLAND. - REFERENCES CITED. - Chapter 2 Late Wisconsin Ice Sheets of North America / Paul A. Mayewski, George H. Denton, Terence J. Hughes. - INTRODUCTION. - LAURENTIDE ICE SHEET. - Eastern Sector. - Southern Sector. - Western Sector. - Northern Sector. - Northeastern Sector. - Interior Sector. - QUEEN ELIZABETH ISLANDS. - Late Wisconsin Maximum. - Late Wisconsin Recession. - CORDILLERAN ICE SHEET. - Late Wisconsin Maximum. - Late Wisconsin Recession. - NORTH AMERICAN ICE SHEETS: AN OVERVIEW . - Maximum and Minimum. - Reconstructions. - Fundamental Questions About Late Wisconsin Deglaciation. - Glaciological Speculations. - REFERENCES CITED. - APPENDIX. - Chapter 3 Late Wisconsin-Weichselian Mountain Glaciers and Small Ice Caps / John T. Hollin, David H. Schiling. - INTRODUCTION. - ALASKA. - WESTERN UNITED STATES. - MEXICO AND CENTRAL AMERICA. - SOUTH AMERICA. - Venezuela. - Colombia. - Ecuador. - Peru. - Bolivia. - Chile and Argentina to Lat 36°30'S. - Chile and Argentina South of Lat 36°30'S. - Islas Juan Fernandez. - Falkland Islands (Islas Malvinas). - Brazil. - Areas and Volumes. - NEWZEALAND. - AUSTRALIA, NEW GUINEA, AND SABAH. - The Australian Mainland. - Tasmania. - New Guinea and Sabah. - Conclusions. - AFRICA. - Northwest Africa and Atlantic Islands. - Mountains in Ethiopia. - Mountains Surrounding Lake Victoria. - South and West Africa. - SUBANTARCTIC ISLANDS. - CONCLUSIONS. - REFERENCES CITED. - Chapter 4 Numerical Reconstruction of Valley Glaciers and Small Ice Caps / David H. Schilling, John T. Hollin. - INTRODUCTION. - VALLEY GLACIERS AND PERFECT PLASTICITY. - The Iterative Scheme. - The Shape Factor. - Choice of the Yield Stress. - Choice of Step Length, [Delta x]. - The First Step and the Snout. - Steep and Mountainous Areas. - The VALLEY Program. - ICE CAPS, WITH SLIDING AND ABLATION. - Perfect Plasticity. - Law of Sliding and Iterative Scheme. - The ABLATE Program. - Various Models and the Flow Law. - An Application of the ABLATE Program. - Some Remaining Problems. - CONCLUSIONS. - REFERENCES CITED. - Chapter 5 Numerical Reconstruction of Paleo-Ice Sheets / Terence J. Hughes. - ICE-BED COUPLING AND SUBGLACIAL HYDROLOGY. - SUBGLACIAL HYDROLOGY AND EROSION-DEPOSITION PROCESSES. - TOPOGRAPHIC CRITERIA FOR RECONSTRUCTING FORMER ICE SHEETS. - Subglacial Landscapes. - Ice Domes. - Ice Saddles. - Melting Zone. - Equilibrium Zone. - Freezing Zone. - Ice Streams. - BASIC EQUATIONS FOR STEADY-STATE CREEP IN ICE SHEETS. - BASAL SHEAR STRESS AND TWO-DIMENSIONAL LAMINAR FLOW. - BASAL SHEAR STRESS AND BASAL SLIDING. - BASAL SHEAR STRESS AND CONSTRUCTING ICE-SHEET PROFILES. - BASAL SHEAR STRESS FOR FROZEN AND MELTED BEDS. - BASAL SHEAR STRESS FOR FREEZING AND MELTING BEDS. - BASAL SHEAR STRESS FOR ICE STREAMS AND ICE LOBES. - BASAL SHEAR STRESS FOR ICE DIVIDES. - EVALUATING TERMS IN THE FLOW AND SLIDING LAWS FOR GLACIAL ICE. - RADIAL FLOW AND SNOW ACCUMULATION FOR ICE DOMES. - LATERAL SHEAR AND DOWNDRAW FOR ICE STREAMS. - ISOSTATIC ADJUSTMENTS BENEATH ICE SHEETS. - SUMMARY. - REFERENCES CITED. - Chapter 6 The Last Great Ice Sheets: A Global View / Terence J. Hughes, George H. Denton, Björn G. Andersen, David H. Schilling, James L. Fastook, Craig S. Lingle. - AREAL EXTENT OF LATE WISCONSIN-WEICHSELIAN ICE SHEETS. - North America. - Greenland. - Eurasia. - Antarctica. - Minimum and Maximum. - Reconstructions of Late Wisconsin-Weichselian Ice Extent. - VERTICAL EXTENT OF LATE WISCONSIN-WEICHSELIAN ICE SHEETS. - The Critical Problem of Marine Ice Sheets. - Flowline Profiles for Variable Bed Topography. - Flowline Profiles for Variable Isostatic Compensation. - Flowline Profiles for Variable Basal Shear Stress. - Flowline Profiles for Present-day Ice Sheets. - Flowline Profiles for Late Wisconsin-Weichselian Ice Sheets. - Isostatic Conditions for Late Wisconsin-Weichselian Ice Sheets. - Basal Conditions for Late Wisconsin-Weichselian Ice Sheets. - Elevations and Volumes of Late Wisconsin-Weichselian Ice Sheets. - DISCUSSION. - REFERENCES CITED. - Chapter 7 History of the Marine Ice Sheet In West Antarctica During the Last Glaciation: A Working Hypothesis / Minze Stuiver, George H. Denton, Terence J. Hughes, James L. Fastook. - INTRODUCTION . - McMURDO SOUND AREA. - Ross Sea Drift: Description. - Ross Sea Drift: Interpretation. - Radiometric Dates and Ross Sea Drift. - Older Drift: Description and Interpretation. - Discussion. - TERRA NOVA BAY. - BEAUFORT AND FRANKLIN ISLANDS. - GLACIAL-MARINE SEDIMENTS IN THE ROSS SEA. - RECONSTRUCTION OF LATE WISCONSIN ANTARCTIC ICE SHEET. - Geologic Background. - Glaciological Background: Steady-State Model. - Conclusions. - DISINTEGRATION OF MARINE ICE SHEET IN WEST ANTARCTICA. - Disintegration Model. - Disintegration of Ice Shelves. - Late Wisconsin-Holocene Disintegration. - Disintegration during Super Interglacials. - SUMMARY. - REFERENCES CITED. - Chapter 8 The Arctic Ice Sheet: An Outrageous Hypothesis / George H. Denton, T erence J. Hughes. - ICE-SHELF ORIGIN OF NORTHERN HEMISPHERE ICE DOMES. - Growth Rates of Arctic Ice Domes. - Sites for lnitiating Arctic Ice Domes. - Thickening Rates of Arctic Sea Ice. - Sites for Grounding Arctic Sea Ice. - Forming Arctic Ice Shelves on Deep Oceans. - Assessing the lce-Shelf Hypothesis for Forming Marine Ice Domes. - LA TE WISCONSIN-WEICHSELIAN ARCTIC ICE SHEET. - Ice Domes. - Ice Streams. - Ice Shelves. - DISINTEGRATION OF LATE WISCONSIN-WEICHSELIAN ARCTIC ICE SHEET. - Initiation of Late Wisconsin-Weichselian Glacial Surges. - Maintenance of Late Wisconsin-Weichselian Glacial Surges. - Environmental Impact of Late Wisconsin-Weichselian Glacial Surges. - CONCLUSIONS. - REFERENCES CITED. - INDEX.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 484 S. : Ill., Kt. ; 27 Kt.-Beil.
    ISBN: 0471060062
    Series Statement: A Wiley interscience publication
    Location: AWI Reading room
    Location: AWI Reading room
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 281 (1979), S. 610-610 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] I HAVE recently realised that we did not give Dr John Mercer full credit for his earlier contributions when we wrote our paper Was there a late-Wrm Arctic Ice Sheet?1. In our reference to Mercer's paper A former ice sheet in the Arctic Ocean?2 we should have noted that he was the first to make a ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 273 (1978), S. 477-478 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] TWELVE scientists on the cutting-edge of climatic research have contributed to the five sections of this book: studying past climates, the Earth's heat budget, astronomical influences, modelling changing climates, and climate and man. In general, they assume that their particular field of study is ...
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2019-06-28
    Description: Observational results from the Interball Tail Probe spacecraft are presented. One of the main objectives of the Interball project is to study the dynamic processes in the magnetosphere. Three events observed by the spacecraft's instruments are investigated: a pseudobreakup during which earthward streaming ions were observed in the vicinity of a thin current sheet; a substorm in which the magnetic signatures in the lobe and on the ground were preceeded by northward re-orientation of the interplanetary magnetic field Bz component; and a magnetic storm at the beginning of which extreme deformation of the magnetotail was observed.
    Keywords: Geophysics
    Type: ; 497-506
    Format: text
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  • 7
    Publication Date: 1982-04-01
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
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  • 8
    Publication Date: 1989-01-01
    Print ISSN: 0260-3055
    Electronic ISSN: 1727-5644
    Topics: Geography , Geosciences
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  • 9
    Publication Date: 2003-01-01
    Description: Jakobshavn Isbræ is a major ice stream that drains the west-central Greenland ice sheet and becomes afloat in Jakobshavn Isfjord (69° N, 49° W), where it has maintained the world’s fastest-known sustained velocity and calving rate (7 kma−1) for at least four decades. The floating portion is approximately 12 km long and 6 km wide. Surface elevations and motion vectors were determined photogrammetrically for about 500 crevasses on the floating ice, and adjacent grounded ice, using aerial photographs obtained 2 weeks apart in July l985. Surface strain rates were computed from a mesh of 399 quadrilateral elements having velocity measurements at each corner. It is shown that heavy crevassing of floating ice invalidates the assumptions of linear strain theory that (i) surface strain in the floating ice is homogeneous in both space and time, (ii) the squares and products of strain components are nil, and (iii) first- and second-order rotation components are small compared to strain components. Therefore, strain rates and rotation rates were also computed using non-linear strain theory. The percentage difference between computed linear and non-linear second invariants of strain rate per element were greatest (mostly in the range 40–70%) where crevassing is greatest. Isopleths of strain rate parallel and transverse to flow and elevation isopleths relate crevassing to known and inferred pinning points.
    Print ISSN: 0260-3055
    Electronic ISSN: 1727-5644
    Topics: Geography , Geosciences
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  • 10
    Publication Date: 2017-01-31
    Description: Two approaches to ice-sheet modeling are available. Analytical modeling is the traditional approach. It solves the force (momentum), mass, and energy balances to obtain three-dimensional solutions over time, beginning with the Navier-Stokes equations for the force balance. Geometrical modeling employs simple geometry to solve the force and mass balance in one dimension along ice flow. It is useful primarily to provide the first-order physical basis of ice-sheet modeling for students with little background in mathematics (Hughes, 2012). The geometric approach uses changes in ice-bed coupling along flow to calculate changes in ice elevation and thickness, using floating fraction φ along a flowline or flowband, where φ = 0 for sheet flow, 0 
    Print ISSN: 1994-0432
    Electronic ISSN: 1994-0440
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union (EGU).
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