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  • Books  (66)
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  • 1970-1974  (66)
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  • 1
    Series available for loan
    Series available for loan
    Ice fog : low temperature air pollution (1970)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-121
    In: Research report / Cold Regions Research and Engineering Laboratory, 121
    Description / Table of Contents: Abstract: Stable pressure systems over interior Alaska, sometimes produce prolonged, extreme (below -40°C) cold spells at the surface. The meteorological conditions responsible for two such cold spells are discussed in detail in Appendix A, where it is shown that the rate of radiative cooling of the air is enhanced by suspended ice crystals which are themselves a result of the initial cooling. Radiation fogs formed during the onset of cold spells are generally of short duration because the air soon becomes desiccated. These fogs consist of supercooled water droplets until the air temperature goes below the "spontaneous freezing point" for water droplets (about -40°C); the fog then becomes an ice crystal fog, or simply "ice fog. " During the cooling cycle water is gradually condensed out of the air until the droplets freeze. At this point there is a sharp, discontinuous decrease in the saturation vapor pressure of the air because it must be reckoned over ice rather than over water. The polluted air over Fairbanks allows droplets to begin freezing at the relatively high temperature of -35°C. Between -35 and -40°C the amount of water vapor condensed by freezing of super cooled water droplets is 3 to 5 times greater than the amount condensed by 1°C of cooling at these temperatures. This results in rapid and widespread formation of ice fog (Appendix B) which persists in the Fairbanks area as long as the cold spell lasts. The persistence of Fairbanks ice fog depends on a continual source of moisture (4.1 x 10^6 kg H20 per day) from human activities within the fog. Ice fog crystals are an order of magnitude smaller than diamond dust or cirrus cloud crystals, which in turn are an order of magnitude smaller than common snow crystals (0.01, 0.1 and 1 to 5 mm respectively). The difference in size are shown to result from the differences in cooling rates over five orders of magnitude. Most of the ice fog crystals have settling rates which are smaller than the upward velocity of air over a city center. The upward air movement is caused by convection cells driven by the 6°C "heat island" over Fairbanks. This causes a reduced precipitation rate which permits the density of ice fog in the center center to be three times greater than that in the outlying areas. The inversions which occur during cold spells over Fairbanks begin at ground level and are among the strongest and most persistent in the world. They are three times stronger than those in the inversion layer over Los Angeles. Thus, the low-lying air over Fairbanks stagnates and becomes effectively decoupled from the atmosphere above, permitting high concentrations all pollutants. The combustion of fuel oil, gasoline and coal provides daily inputs of 4.1 x 10^6 kg CO2, 8.6 x 10^3 kg SO2, and 60, 46 and 20 kg of Pb, Br, and Cl respectively, into a lens-like layer of air resting on the surface with a total volume less than 3 x 10^9 m^3. The air pollution over Fairbanks during cold spells is further worsened, because the mechanisms for cleaning the air are virtually eliminated while all activities which pollute the air are increased.
    Type of Medium: Series available for loan
    Pages: v, 118 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 121
    URL: https://hdl.handle.net/11681/5972
    Language: English
    Note: CONTENTS I. Introduction II. Air pollution Types of air pollution Temperature in versions Low temperature air pollution III. Sources of pollution-water Combustion products Cooling water from power plants · Miscellaneous sources IV. Sources of pollution other than water Electrical conductance and particulates Combustion products Summary V. Economic growth and ice fog VI. General physical properties of ice fog Optical properties Cooling rate of exhaust gases Development of a typical ice fog The effect of freezing droplets on the growth rate of ice fog VII. Structure of the polluted air layer Volume Temperature distribution and convection in Fairbanks air VIII. Mass budget of ice fog Ice fog precipitation rates Density of ice fog Ice fog evaporation rates Use of the mass budget equation Summary of the mass budget IX. Air pollution aspects of ice fog Air pollution Remedial action Ice fog probability Literature cited Appendix A. :The effect of suspended ice crystals on radiative cooling Appendix B. Nucleation and freezing of supercooled water droplets Abstract
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  • 2
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    Geomorphic and sedimentologic processes of rivers and coast, Yukon coastal plain (1973)
    Ottawa : Department of Energy, Mines and Resources, Geological Survey of Canada
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    Call number: AWI G3-20-94305
    Description / Table of Contents: The primary objective of this study was to obtain reconnaissance data about modern river and coastal environments for the Yukon coastal plain between the Mackenzie Delta and the Alaskan border that would be useful in future decision making about development of the area.
    Type of Medium: Series available for loan
    Pages: 245 Seiten , Illustrationen, Karten , 6 Karten
    Series Statement: Report / Environmental-Social Committee. Northern Pipelines. Task Force on Northern Oil Development 73,39
    Language: English
    Note: CONTENTS SUMMARY 1.1. Objectives of the Study 1.1.1. River Objectives. 1.1.2. The Coastal Objectives 1.2. Scientific Conclusions 1.2.1. Rivers 1.2.2. Coast 1.3. Implications and Reconnnendations 1.3.1. Rivers 1.3.2. Coast 2 INTRODUCTION 2.1. General Nature and Scope of Study 2.2. Specific Objectives 2.2.1. Rivers 2.2.2. Coast 2.3. Relevance to Pipeline Development 2.4. Acknowledgements 3. CURRENT STATE OF KNOWLEDGE 4. STUDY AREA 4.1. Physiography 4.2. Climate 4.3. General Geology 5. SOURCES, METHODS, AND RATIONALE OF DATA COLLECTION 5.1. Rivers 5.1.1. Drainage Basin Characteristics Area Shape Hypsometry Hydrograph estimation 5.1.2. River Valleys 5.1.3. River Channels 5.1.4. River Hydraulics and Discharge Estimation 5.1.5. Sediment Transport Bedload Suspended and dissolved load 5.1.6. Channel Stability Bed Scour Lateral Stability 5.2. Coast 5.3. Laboratory Techniques 6. RESULTS 6.1. Rivers 6.1.1. Drainage Basin Characteristics Area Shape Hypsometry Hydrology and hydrograph estimation 6.1.2. River valley and long profiles 6.1.3. Channel pattern and channel form 6.1.4. River hydraulics and discharge estimation 6.1.5. Sediment transport Bedload Suspended and dissloved load 6.1.6 Channel stability Bed scour Lateral stability 6.2. Coast 6.2.1. Sea-ice conditions General pattern during summer season Break-up 6.2.2. Coastal erosion Introduction Alaska borer to mouth of Firth River Herschel Island Herschel Island to the Babbage River delta Kay Point to King Point King Point to Sabine Point Sabine Point to Blow River delta 6.2.3. Coastal sedimentation General patterns of near-shore sediment movement Beaches and spits - general form and sediment types Areal variations and stability of near-shore sediment bodies International border to Komakuk Beach Komakuk Beach to Herschel Island Herschel Island Herschel Island to Babbage River delta Kay Point spit Kay Point to Sabine Point Sabine Point to Blow River delta 6.2.4. Major coastal deltas Firth River fan delta Babbage River delta Running River delta Blow River delta 7. DISCUSSION 7.1. Rivers 7.2. Coast 8. CONCLUSIONS 8.1. Rivers 8.2. Coast 9. IMPLICATIONS AND RECOMMENDATIONS 9.1. Rivers 9.1.1. General scientific 9.1.2. Matters relevant to pipeline activity 9.2. Coast 9.2.1. General scientific 9.2.2. Matters relevant to pipeline activity 10. NEEDS FOR FURTHER STUDY 11. REFERENCES 12. NOTATIONS AND ABBREVIATIONS 13. APPENDIX: HYDRAULIC, SEDIMENTOLOGIC AND GEOMORPHIC DATA FOR EACH RIVER REACH STUDIED
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  • 3
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    Physical properties and internal structure of Greenland snow (1970)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-89
    In: Research report / Cold Regions Research and Engineering Laboratory, 89
    Description / Table of Contents: Abstract: Experiments were carried out near Thule, Greenland, on the correlation between the physical properties and internal structure of snow. About 150 snow samples obtained to 26 m depth were measured for elastic modulus, air permeability, unconfined compressive strength, static compression and creep. The observed density profile curve deviated from the theoretical curve at a depth of 10 m. and density of 0.52 g/cm^3, a value almost equivalent to the limiting density obtainable by simple mechanical packing. Therefore, further densification must proceed through plastic flow in grains. A similar critical depth was observed in the vertical distribution of Young's modulus. A positive correlation was found between Young's modulus and density, and an inverse correlation between average grain diameter and Young's modulus or density. There were reciprocal correlations between air permeability and density or unconfined compressive strength, and between the number of grains and their average diameters. Kozeny's constant of Greenland snow was obtained from air permeability values and the length of peripheries of cross sections of grains. To demonstrate the change of internal structure of snow due to densification, static compression tests of snow cylinders were conducted, and thin sections of snow texture were compared before and after compression. Creep curves of snow cylinders were analyzed using Nutting's formula and are discussed in connection with change of internal structure. Basal slip, buckling, cell or sub-grain formation, recrystallization and grain boundary migration occurring during plastic deformation of snow texture were observed by static compression of thin section snow under the microscope.
    Type of Medium: Series available for loan
    Pages: vi, 32 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 89
    URL: https://hdl.handle.net/11681/5874
    Language: English
    Note: CONTENTS Preface Nomenclature Introduction Experimental methods Density profile and densification Internal structure in typical samples Average grain size obtained from thin section Two-dimensional porosity, total pore periphery and tortuosity Vertical distribution of Young's modulus Air permeability and its structlU'al dependence Porosity dependence Grain size dependence Kozeny's constant for Greenland snow Correlation between air permeability and tortuosity of grains Unconfined compressive strength Static compression and creep in snow under high stresses Microscopic observation of the change in snow textlU'e under compression Literature cited Abstract
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  • 4
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    Antarctic geology and solid-earth geophysics : guidelines for U.S. program planning, 1973-1983 (1974)
    Washington : National Academy of Science
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    Call number: AWI G9-19-92302
    Description / Table of Contents: Report which attempts to assess the principal problems of antarctic solid-earth science over the decade 1973-83, to evaluate their importance in relation to the south polar regions and the earth as a whole, and to suggest ways and a priority ordering for undertaking their solutions.
    Type of Medium: Monograph available for loan
    Pages: x, 26 Seiten , Illustrationen
    URL: https://www.nap.edu/catalog/20174/antarctic-geology-and-solid-earth-geophysics-guidelines-for-us-program
    Language: English
    Note: Contents: 1. INTRODUCTION. - 2. PARTICULAR CONCERNS AND REQUIREMENTS. - Environmental Safeguards. - Topographic Mapping. - Regional Geological and Geophysical Surveying. - Stateside Analyses. - Remote Sensing. - Core Drilling into Bedrock beneath the Ice. - New Techniques. - 3. INTERCONTINENTAL AND INTRACONTINENTAL RELATIONSIDPS. - Present Continental Margins. - Passive Continental Margins. - Active Continental Margins. - Pre-Andean Orogenic Belts. - Gondwanide (Ellsworth) Orogen. - Borchgrevink Orogen. - Ross Orogen. - Relations between East and West Antarctica. - West Antarctic Geochronology and Geophysics. - The Ross Embayment. - Surface-Wave-Dispersion Studies. - 4. ACTIVE CRUSTAL MOVEMENTS AND VOLCANICITY. - Seismicity. - Volcanicity. - Gravity Base Station Ties. - Gravity Surveys. - Establishment of Tide Stations and Bench Marks. - Nonisostatic Crustal Uplift. - 5. STUDIES OF THE LATE CENOZOIC ENVIRONMENT. - Comparative Glacial Geologic Chronologies. - Drilling beneath the Ross Ice Shelf. - Ocean Core Studies. - 6. SPECIAL GEOLOGICAL PROBLEMS. - Igneous Processes. - Jurassic Basalt. - Active Continental Margin Processes. - Paleontology. - Vertebrate Paleontology. - Invertebrate Paleontology. - Permian and Triassic Floras. - 7. ANTARCTIC MINERAL RESOURCES. - 8. PRIORITY ORDERING. - 9. SPECIAL RECOMMENDATIONS. - REFERENCES.
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  • 5
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    Internationales Ozonkolloquium und Vergleich von Meßgeräten : Siófok, UVR, 4.5.-25.5.1969 (1971)
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik bei der Deutschen Akademie der Wissenschaften zu Berlin
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    Call number: MOP Per 581(2/16) ; ZSP-319/B-16
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre, Heft 16
    Type of Medium: Series available for loan
    Pages: 87 Seiten , Illustrationen
    ISSN: 0533-7585
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre 16
    Language: German , English , Russian
    Note: INHALT: 1) Vorwort. - Vorträge. - 2) Über den gegenwärtigen Stand der Ozonforschung / E. BORBELY. - 3) Über eine elektrochemische Ozonsonde / H. RÖTHIG, D. SONNTAG. - 4) Die Abweichung der Werte des Gesamtgehalts des Ozons,der mit dem Ozonometer M-83 in Luftmassen verschiedenen Verunreinigungsgrades gemessen wurde / E. VENTURA. - 5) Über den aerosolbedingten Fehler der Daten des Gesamtozongehalts der Atmosphäre im Stationsnetz des Hydrometrischen Dienstes der UdSSR / G. P. GUSCHTSCHIN. - 6) Zur Methodik der Einführung der aerosolbedingten Korrektur in die Meßergebnisse des Gesamtozongehalts der Atmosphäre / G. P. GUSCHTSCHIN. - 7) Variationen des totalen Ozongehalts der Atmosphäre im Zusammenhang mit stratosphärischen Erwärmungen / W. HOEBBEL. - 8) Markante Schwankungen der kurzperiodischen Variationen des Gasamtozonbetrages und ihre Beziehungen zur Zirkulation, zu plötzlichen stratosphärischen Erwärmungen und zur Mesosphäre / W. Schwahn. - 9) Screen effect in the Ozonosphere / R. S. Steblova. - 10) Vergleich von Ozonmeßgeräten. - DOBSON-Spectrophotometer. - Universalozonometer M-83. - Spektrometer ISP 22. - 11) Verzeichnis der Tabellen des Meßgerätevergleichs. - 12) Schlußbetrachtung. - Anschriften der Autoren und der Teilnehmer am Meßgerätevergleich. , Beiträge teilweise in deutscher, teilweise in englischer, teilweise in russischer Sprache
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  • 6
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    Beiträge zur Ozonforschung (1974)
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik
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    Call number: MOP Per 581(2/18) ; ZSP-319/B-18
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre, Heft 18
    Type of Medium: Series available for loan
    Pages: 107 Seiten , Illustrationen
    ISSN: 0533-7585
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre 18
    Language: German , English
    Note: INHALT: Vorwort / K. H. GRASNICK. - Frühjahrs- und Herbstumstellung der Felder der meteorologischen Elemente in der Stratosphäre / E. BORBÉLY. - On the variations of the total amount of ozone in relation to the behaviour of some ionospheric parameters in the winter-time upper atmosphere = (Über Variationen des Gesamtozongehalts der Atmosphäre in Beziehung zum Verhalten einiger ionosphärischer Parameter in der winterlichen Hochatmosphäre) / K. H. GRASNICK, G. ENTZIAN. - Gesamtozongehalt und Temperaturänderungen der 100 mbar-Fläche im europäischen Raum in den Jahren 1967-1968 / J. PICHA. - Zwei einfache Registriergeräte zur Bestimmung des bodennahen Ozons auf der Grundlage der amperometrischen Titration und des coulometrischen Meßprinzips nach Novák / H. MROSE, W. WARMBT. - Vorläufige Meßergebnisse des bodennahen Ozons unter Verwendung von Chromtrioxydfiltern / W. WARMBT, H. MROSE, G. PHILIPP. - Erfahrungen über Ozonmessungen mit dem DOBSON-Spektrophotometer in Potsdam seit den Vergleichsmessungen in Siófok, UVR, im Jahre 1969 / P. PLESSING. - Ozonvariationen über Havanna während der Sonnenfinsternis vom 7. März 1970 unter Berücksichtigung der Randverdunkelung / K. H. GRASNICK, H. WÖRNER, P. PLESSING. - SHORT GONTRIBUTION Ozone measurements data during the solar eclipse on March 7, 1970 = (Daten der Ozonmessungen während der Sonnenfinsternis vom 7. März 1970) / R. S. STEBLOVA, V. G. UTROBIN. -
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  • 7
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    Antarctic glaciology : guidelines for U.S. program planning, 1973-1983 (1974)
    Washington : National Academy of Sciences
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    Call number: AWI G7-18-91940
    Type of Medium: Series available for loan
    Pages: x, 66 Seiten , 23 cm
    URL: https://www.nap.edu/catalog/20110/antarctic-glaciology-guidelines-for-us-program-planning-1973-1983
    Language: English
    Note: Contents: 1. PRIMARY OBJECTIVES. - 2. DYNAMICS OF THE ICE: FIELD STUDIES. - Major Regional Studies. - In Progress. - Newly Proposed. - Continentwide Measurements. - Surface and Bed Topography. - Mass Balance. - Complementary Field Studies. - Glacier and Local Ice-Cap Studies. - Related Studies outside Antarctica. - Development of New Observational Techniques and Instrumentation. - 3. ANALYSIS AND INTERPRETATION OF FIELD DATA. - Description of the Dynamic State of the Ice Sheet. - Physical Properties of the Ice. - Sea-Ice Modeling. - 4. GLACIAL HISTORY. - Glacial Geology. - Core Studies. - Numerical Modeling. - 5. ENVIRONMENTAL INTERACTION. - Meteorology. - Oceanography. - Geology and Geophysics. - Biology. - Application of New Techniques. - Satellites and Systems. - Automatic stations. - Oceanographic Instruments. - Global Numerical Modeling. - REFERENCES AND BIBLIOGRAPHY. - APPENDIX A. International Antarctic Glaciological Project. - APPENDIX B. The International Antarctic Glaciological Project Standardization Document. - APPENDIX C. Abstracts of Projects Considered by the Glaciology Panel during the Antarctic Planning Exercise, November 11-13, 1971. - Core Drilling and Analysis. - Ice-Thickness Mapping. - Ross Ice Shelf Project (RISP). - Glacial and Periglacial Studies. - Sea Ice. - Ice Streamline Cooperative Antarctic Project (ISCAP). - Sub-Ice-Surface Remote Sensing. - Alpine Outlet Glaciers. - Roosevelt Island. - APPENDIX D. Antarctic Sea Ice Programm. - Differences between the Arctic and Antarctic Ice Packs. - Importance of the Antarctic Pack. - Proposed programs. - Satellite Programs. - Airborne Remote Sensing. - Unmanned Drifting Stations. - Manned Drifting Stations. - Coastal Stations. - Timing. - Conclusion. - Bibliography. - APPENDIX E. Abbreviations and Terms Used in this Report.
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  • 8
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    The planetary boundary-layer of the atmosphere (1973)
    Offenbach a. M. : Dt. Wetterdienst
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    Call number: AWI A7-94-0327 ; MOP Per 8(7)
    In: Annalen der Meteorologie, Nr. 7
    Type of Medium: Series available for loan
    Pages: X, 346 S.
    ISSN: 0072-4122
    Series Statement: Annalen der Meteorologie 7
    URL: http://nbn-resolving.de/urn:nbn:de:101:1-201708172258
    Language: English
    Note: Contents: Preface. - Foreword. - Chapter 1 The Planetary Boundary-Layer: Definitions and Equations. - Chapter 2 Some Problems in Modelling the Planetary Boundary-Layer. - The Problem of Closing the System of the PBL-Equations. - Models Based on a Hypothesis for the Profile of the Eddy Viscosity. - Models Based on a Hypothesis for the Mixing-Length. - A Mixing-Length Hypothesis for the Planetary Boundary-Layer Flow in the Atmosphere - Beitr. Phys. Atm., 44, 215-226, 1971. - Note on the Upper Boundary Conditions. - A Note on a Method for Solving the Planetary Boundary-Layer Equations - Beitr. Phys. Atm. 44, 293-296, 1971. Chapter 3 The Structure of the Planetary Boundary-Layer. - The Eddy Viscosity in a Barotropic Planetary Boundary-Layer as Related to the Turbulent KineticEnergy - Beitr. Phys. Atm., 44,127-136, 1971. - Rossby-Number Similarity in the Planetary Boundary-Layer. - A Note on the Rossby Similarity for Flows of Barotropic Planetary Boundary-Layers (with D. YORDANOV) - Beitr. Phys. Atm., 45, 66-71, 1972. - Universal Profiles in the Barotropic Planetary Boundary-Layer - Beitr. Phys. Atm., 45, 148-163, 1972. - Note on the Energy Budget in the PBL. - Layers with a Reduced Eddy Viscosity Caused by the Baroclinicity (with D. YORDANOV) - Beitr. Phys. Atm., 45, 267-275, 1972. - The Wind Profile Very Close to the Ground - Beitr. Phys. Atm., 46, 57-63, 1973. - Numerical Study on the Effects Controlling the Low-Level Jet - Beitr. Phys. Atm., 46, 137-154, 1973. - Chapter 4 The Parameterization of PBL - Effects with the Aid of the Resistance Law. - The Resistance Law for the Planetary Boundary Layer. - The Two Constants in the Resistance Law for a Neutral Barotropic Boundary Layer of the Atmosphere - Beitr. Phys. Atm., 43, 133-140, 1970. - Note on a Paper by F. Wippermann "The Two Constants in the Resistance Law for a Neutral Barotropic Boundary Layer of the Atmosphere" by R. J. TAYLOR - Beitr. Phys. Atm., 44, 69, 1971. - Reply by F. Wippermann. - Empirical Formulae for the Universal Functions Mm (μ) and N (μ) in the Resistance Law for a Barotropic and Diabatic Planetary Boundary Layer - Beitr. Phys. Atm., 45, 305-311, 1972. - The Parameterization of the Turbulent Fluxes of Momentum, Heat and Moisture at the Ground in a Baroclinic Planetary Boundary Layer (with D. YORDANOV) - Beitr. Phys. Atm., 45, 58-65, 1972. - Baroclinic Effects on the Resistance Law for the Planetary Boundary Layer of the Atmosphere - Beitr. Phys. Atm., 45, 244-259, 1972. - A Note on the Parameterization of the Large-Scale Wind stress at the Sea Surface - Beitr. Phys. Atm., 45, 260-266, 1972. - Problems which still have to be solved before the resistance laws can be applied. - Chapter 5 Non-Stationary and/or Horizontally Non-Homogeneous Boundary-Layers. - The Effects of Non-Stationarity on the Planetary Boundary-Layer (with D.ETLING and H.LEYKAUF) - Beitr. Phys. Atm. 46, 34-56, 1973. - Boundary-Layers with a Change in the Roughness - Length and/or in the Temperature: A Bibliographical Survey. - Chapter 6 The Dynamic Instability of the Atmospheric Boundary Layer. - The Orientation of Vortices Due to Instability of the Ekman Boundary-Layer - Beitr. Phys. Atm., 42, 225-244, 1969. - The Stability of an Ekman Boundary-Layer Flow as Influenced by the Thermal Stratification (in Germ.) by D.ETLING - Beitr. Phys. Atm., 44, 168-186, 1971. - Chapter 7 The Dispersion of Windborne Material in the Planetary Boundary-Layer. - A Perspective for a Routine Prediction of Concentration Patterns (with D. YORDANOV) - Atm. Environm., 6, 877-888, 1972. - Time-Dependent Concentrations of Dispersed Material Compared with those of the Corresponding Stationary Cases (in Germ.) - Meteor. Rdsch., 26, 11-18, 1973. - Meteorological Parameters Relevant in a Statistical Analysis of Air Quality Data. - List of Symbols. - Author Index.
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  • 9
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    Glacial and periglacial geomorphology (1971)
    London : Arnold
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    Call number: AWI G7-17-90989
    Type of Medium: Monograph available for loan
    Pages: XV, 608 S. , Ill., graph. Darst., Kt.
    Edition: Repr.
    ISBN: 0713153776
    Language: English
    Note: Contents: Preface. - List of Plates. - Figures in the Text. - Introduction. - PART I. BASIC CONCEPTS OF GLACIATION AND GLACIER BEHAVIOUR. - Chapter 1 Ice Ages and World Glaciation. - Chapter 2 Glacier Régimes. - Chapter 3 The Physical Properties of Ice and Types of Glacier. - Chapter 4 Ice Motion. - Chapter 5 Some Indirect Effects of Pleistocene Glaciation. - PART II. GLACIAL AND FLUVIOGLACIAL EROSION. - Chapter 6 Small-scale Features of Glacial and Fluvioglacial Erosion. - Chapter 7 Glaciated Valleys. - Chapter 8 Cirques. - Chapter 9 Glacial Erosion in Areas of Low Relief. - Chapter 10 Glaciation in Coastal Environments. - Chapter 11 Quantitative Aspects of Glacial Erosion. - Chapter 12 Erosion by Glacial Meltwater, and Glacial Diversion of Drainage. - PART III. GLACIAL AND FLUVIOGLACIAL DEPOSITION. - Chapter 13 General Considerations of Glacial and Fluvioglacial Deposition. - Chapter 14 Drumlins. - Chapter 15 Moraines. - Chapter 16 Fluvioglacial Ice-Contact Features: Eskers and Kames. - Chapter 17 Ice Stagnation Features. - Chapter 18 Proglacial Features. - Chapter 19 Glacial Lakes and Lacustrine Deposits. - PART IV. PERIGLACIAL GEOMORPHOLOGY. - Chapter 20 The Periglacial Environment: An Introductory Survey. - Chapter 21 Frozen Ground Phenomena. - Chapter 22 Patterned Ground. - Chapter 23 Periglacial Mass Movements and Slope Deposits. - Chapter 24 Altiplanation, Tors, Blockfields, and Stone Streams. - Chapter 25 The Action of Snow. - Chapter 26 Periglacial Wind Action. - Index.
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  • 10
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    Isua, Greenland : glaciological investigations during 1973 (1974)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-318
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Drilling and field observations. - Interpretation. - Implications for the feasibility study. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: Two holes were drilled through the Greenland ice sheet during 1973 and temperature measurements were made in one hole drilled during 1972. These measurements show that the area of liquid water beneath the ice cap extends to ice depths as shallow as 100 m. The consequences of removing the frozen margin of glacial ice could be serious and more temperature measurements are needed to exactly locate the subglacial water. Petrographic studies of a few ice cores revealed a strongly oriented crystal fabric and an appreciable surface accumulation of superimposed ice.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen, Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 318
    URL: http://www.worldcat.org/oclc/1035634454
    Language: English
    Branch Library: AWI Library
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