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  • English  (2,166)
  • Swedish  (8)
  • Finnish
  • 1965-1969  (1,502)
  • 1955-1959  (674)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 6743 ; M 93.0085/4
    In: Methods in geochemistry and geophysics
    Type of Medium: Monograph available for loan
    Pages: XII, 258 S. : Ill.
    Series Statement: Methods in geochemistry and geophysics 4
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York : Reinhold
    Call number: M 93.0129
    Type of Medium: Monograph available for loan
    Pages: VIII, 226 S.
    Language: English
    Location: Upper compact magazine
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  • 3
    Call number: M 93.0140
    In: NASA SP
    Type of Medium: Monograph available for loan
    Pages: IX, 256 S. : überw. Ill.
    Series Statement: NASA SP 129
    Language: English
    Location: Upper compact magazine
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  • 4
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0069/1
    In: Geochemistry and mineralgy of rare elements and genetic types of their deposits
    Type of Medium: Monograph available for loan
    Pages: XIII, 688 S. : graph. Darst.
    Uniform Title: Geokhimiya redkikh elementov
    Language: English
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  • 5
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    London [u.a.]: Academic Press
    Associated volumes
    Call number: 93.0079
    In: Chemical oceanography
    Language: English
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/2 ; 10/G 5218/2/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
    Location: Upper compact magazine
    Location: Reading room
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  • 7
    Monograph available for loan
    Monograph available for loan
    Chicago : Rand McNally
    Call number: M 97.0183
    Type of Medium: Monograph available for loan
    Pages: XIII, 381 S.
    Classification:
    Tectonics
    Language: English
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  • 8
    Monograph available for loan
    Monograph available for loan
    New Brunswick [u.a.] : Rutgers Univ.
    Call number: AWI P8-08-0038
    Type of Medium: Monograph available for loan
    Pages: 126 S. : Ill.
    Edition: Final Report
    Language: English
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  • 9
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    New York : Geological Soc. of America
    Associated volumes
    Call number: 97.0498/2
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
    Pages: Part 1-3
    Classification:
    Regional Geology
    Language: English
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  • 10
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    New York : Geological Soc. of America
    Associated volumes
    Call number: 97.0498/1
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
    Pages: ix, 250 S.
    Classification:
    Regional Geology
    Language: English
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  • 11
    Monograph available for loan
    Monograph available for loan
    Aachen : Meteorologisches Observatorium des Deutschen Wetterdienstes
    Call number: MOP 42741 / Mitte ; MOP 23653
    Type of Medium: Monograph available for loan
    Pages: 158 Seiten , Illustrationen
    Language: English
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 12
    Call number: MOP 24916
    In: Geofysikální sbornik
    Type of Medium: Monograph available for loan
    Pages: 17 S. : Ill., graph. Darst.
    Series Statement: Geofysikální sbornik 96
    Language: English
    Location: MOP - must be ordered
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  • 13
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    Delft ; 1.1969-76.2010
    Call number: S 90.0083
    ISSN: 0165-1706
    Language: English
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  • 14
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
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  • 15
    Call number: MR 17.91138
    Type of Medium: Monograph available for loan
    Pages: [167 S.]
    Language: English
    Note: 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.) , 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.)
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  • 16
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : Belknap Press of Harvard University
    Call number: IASS 16.90614
    Type of Medium: Monograph available for loan
    Pages: 323 S.
    ISBN: 0674794850 , 9780674794856
    Language: English
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  • 17
    Call number: AWI S1-18-91339
    Type of Medium: Monograph available for loan
    Pages: 608 S.
    Edition: 4. ed., repr.
    Language: English
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  • 18
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-21
    In: Research report / Cold Regions Research and Engineering Laboratory, 21
    Description / Table of Contents: Limited studies of white-outs on the Greenland Ice Cap indicate that five major types of low visibility have been reported as white-out. They are: 1.) Overcast white-out, caused by a continuous cloud cover. 2.) Water-fog white-out, produced by supercooled water droplets in the air. 3.) Ice-fog white-out, produced by ice crystals suspended in the air. 4.) Blowing snow white-out, produced by wind-driven, wind-eroded snow. 5.) Precipitation white-out, produced by falling snow. The first three types are interrelated and appear to be produced by upslope, convective lifting of warm maritime air and the advective transport of the cooled saturated air over the cold snow field. Radiation heat losses from the snow surface may contribute to more rapid formation of the white-out. The fact that there is a shift in the prevailing wind direction prior to the development of a white-out indicates that certain changes in upper air circulation may be associated with white-out formation and duration. There is reason to believe that upper air and surface observations might make it possible to forecast white-outs on the Greenland Ice Cap with some degree of reliability.
    Type of Medium: Series available for loan
    Pages: iv, 12 Seiten , Illustrationen , 27 cm
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 21
    Language: English
    Note: CONTENTS Preface Summary Introduction Results at Site 2 Discussion References
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  • 19
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-26
    In: Research report / Cold Regions Research and Engineering Laboratory, 26
    Description / Table of Contents: Summary: The results of temperature, density, ram-hardness and grain-size measurements at 118 test sites along a 300-mi. traverse, ranging in elevation from 2000 to 8000 ft, are reported in detail, and their meteorological and climatic implications are discussed. Four types of diagenetically produced facies were recognized: ablation facies, extending from the snout of the glacier to the firn line; soaked facies, extending from the firn line to the saturation line; percolation facies, extending from the saturation line to the dry-snow line; and dry-snow facies, extending across the glacier above the dry-snow line. The well defined saturation line shows marked discontinuities in temperature, density, and ram hardness, while the dry-snow line is a transition 1 zone 10-20 mi. wide. The recognition of facies allows greater resolution of glacier characteristics than Ahlmann's classification, permitting quantitative subdivision of all types of large glaciers. Regional precipitation (entirely from cyclonic storms) is about 5 times greater than at Thule; and the prevailing katabatic winds control the vertical component of the temperature gradient in the snow and firn. The depth density curve of the firn at elevations where melt is negligible is invariant with time, as in Sorge's law, so that the densification can be treated as a steady-state situation with load as the only significant variable.
    Type of Medium: Series available for loan
    Pages: vii, 62, A4, B2, C2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 26
    Language: English
    Note: CONTENTS Preface Summary Chapter I. Introduction Greenland Glaciers and stratigraphy The Greenland ice sheet - a rock formation Region of investigation Chapter II. Methods of investigation Stratigraphy Accumulation measurements Work program at pit stations General description of pits Temperature Hardness Density, stratigraphy, and grain size Accuracy of density measurements Photography Core drilling Air permeability and mechanical tests Elevation measurements Barometric altimetry Transit leveling Chapter III. Basic concepts and definitions Summer melt Soaking Complete soaking Localized percolation Stability Diagenetic facies Chapter IV. Presentation and discussion of results Grain size and morphology Grain size Morphology Temperature Seasonal variation and mean annual temperature Thermal effect of an open pit Constancy of climate Facies in terms of temperature data Hardness Continuity of strata Effect of wind Increase in R with depth below snow surface Facies in terms of hardness data Density Depth vs density data Depth vs load data Attempts to formulate depth vs density Facies in terms of density data Glacier facies - a classification of glaciers Chapter V. Stratigraphy and accumulation Stratigraphy Stratigraphic interpretation at station 1-0 Correlation between stratigraphic and meteorological records Accumulation Integrated qepth-density curves Measurement of accumulation on surface marker plates Pole-marker measurements Stratigraphic correlation Selection of a reference datum in the annual stratigraphic sequence Correlation across the traverse Effects of topography Chapter VI. Meteorological and climatological implications Winds Precipitation Annual heat exchange References Appendix A: Stratigraphy, meteorology and glaciology Appendix B: Logistics and development of the research program Appendix C: Tables
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  • 20
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-29
    In: Research report / Cold Regions Research and Engineering Laboratory, 29
    Description / Table of Contents: Summary: A microscopic method for the determination of particle-size distributions of pulverized snow was worked out. The method gives satisfactory distribution curves, presenting the number of particles as a function of their cross-sectional "areas". The measurements were made by means of a filar micrometer eyepiece, the snow particles being placed on a ruled glass slide, which was submerged in silicone oil to prevent evaporation. The time for the determination of a distribution can be appreciably shortened by estimating the size of the particles instead of measuring them, though the accuracy is not so high in this case.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 29
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Snow samples Procedure Experimental results Fraction 150-300 µ Fraction 0-150 µ Mixture of fractions Conclusions
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  • 21
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-27
    In: Research report / Cold Regions Research and Engineering Laboratory, 27
    Description / Table of Contents: Summary: The results of a study on the feasibility of mapping selected snow-cover characteristics for military purposes, taking into account both current synoptic and average conditions, are reported in detail. Problems associated with the construction of isolines for depicting individual or combination of snow-cover conditions are discussed; the need for other statistical parameters in addition to the means is stressed; and the adaptation of frequency and variability indices is suggested. The use of a regional technique, which identified areas somewhat homogenous or substantially different from adjacent areas, is investigated. Problems in mapping snow density are also considered as well as the possibility of estimating snow density from meteorological data. Three sets of codes for the systematic recording and transmission of data are proposed, including a code for ground observers, a simplified code for use where no instruments or trained personnel are available, and a code for aerial observations.
    Type of Medium: Series available for loan
    Pages: vi, 92 Seiten , Illustrationen , 27 cm
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 27
    Language: English
    Note: TABLE OF CONTENTS PREFACE LIST OF TABLES LIST OF ILLUSTRATIONS INTRODUCTION Chapter I. APPLICATION OF ISOLINES FOR DEPICTING ASPECTS OF THE SNOW COVER Visual Problems Use of a simplified base map Other solutions Substantive Problems Observational errors Sampling errors Bias error Effect of reliability of data on isolines Conclusion The ''reasoned distribution'' Effects of substantive problems Conclusion II. DEVELOPMENT OF OTHER MEASURES, INDICES, AND METHODS FOR DEPICTING SNOW COVER CONDITIONS Examples of Possible Normal Indices of Snow Cover Average snow depth at end of the maximum month Average monthly snow depths by superimposed or located line graphs Time aspects Snowfall Selected Statistical Parameters of a Particular Value Extreme values Frequency values Measures of variability Conclusion III. SNOW REGIONS: AN APPROACH TO MAPPING SNOW COVER Snow Region Concept Descriptions of Snow Regions 1. Pacific Coast and Coastal Valley Region 2. The Mountain Zone 3. Great Plains Region 4. The Mackenzie-Manitoba Region 5. Upper Ontario Region 6. Northern Great Lakes-St. Lawrence Region 7. Labrador Region 8. The Northern Arctic Region 9. Ungava-Baffinland Region Conclusions IV. CURRENT SNOW DATA MAPS Introduction Ground Observer's Code Suggested code for "Ground Observer's Snow Report" Comments Symbols for a comprehensive station model Air Observation Code Comments Station Model for Aircraft Snow Observations A Simplified Snow Observation Report . Introduction Proposed code and symbols for station model based on Simplified Snow Observation Report Conclusion Chapter V. MAPPING SNOW DENSITY Introduction Limitations of Data for Mapping Available data Reliability of the data Natural variations in density Snow Density Maps of Eastern Canada Statistical Investigation of Density: Eastern Canada Test for area differences Estimating regional trends in density: Orthogonal polynomials Regional density changes during the winter Conclusions: Statistical investigations Estimating Snow Density from Meteorological Data Relation of density to wind speed and temperature Application of Dmitrieva's equation Conclusion VI. CONCLUSION Snow Cover Maps: Small Scale Compilations of Various Aspects of Their Parameters Preparation of Synoptic Current Snow Data Maps Snow Density Research Investigation of Drift and Erosional Surfaces Initiation of Systematic Collection and Recording of Snow Data Internationally Research Reports Based on Existing Literature .
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-77
    In: Research report / Cold Regions Research and Engineering Laboratory, 77
    Description / Table of Contents: Abstract: A deep rotary core drilling project in 1957 at Site 2 on the Greenland ice sheet (76°59'N, 56°04'W provided ice core to a depth of 411 m. The vertical variation in bulk density, macroscopic structure, oxygen isotope ratios, ionic constituents, and extraterrestrial dust (black spherules) were analyzed using both field and laboratory techniques . These data permit the direct estimate of annual accumulation layers in the core. Continuous stratigraphic measurements and observations were made over the upper 110 m of the profile and detailed physical and chemical analyses were made on continuous lo 3 to 3.9-m core increments at 100, 200, 300 and 411-m depths. The average total ionic concentration in the ice sheet ranges between 0.65 and 1.35 mg/liter. The annual global mass deposit of black spherules as calculated from these studies varies from 2.10 x 10^5 metric tons in 700 year old ice to 6.57 x 10^5 metric tons in 12 year old firn. The oxygen isotope ratio variation provides the best means of estimating accumulation at depth. Results of the investigations indicate rates of net snow accumulation of 42.3, 34.2, 37.4, 41.1 and 41.6 g/cm^2 -yr at the surface, A.D. c. 1773, c. 1513, c. 1233 and c. 934 respectively. Accumulation data and other physical and chemical evidence allow climatological inferences to be made over the 10-century profile. The ice core record shows that snow accumulation and temperature in A. D. 934 were similar to today, followed by a gradual decrease in accumulation to a minimum around the late 18th century and an increase in both accumulation and temperature from A. D. 1773 to 1957 and following.
    Type of Medium: Series available for loan
    Pages: vi, 130 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 77
    Language: English
    Note: CONTENTS Preface Summary 1. lntroduction General background Previous work The Greenland Ice sheet Present work Ice core studies ll. Field procedures General background Subsurface snow laboratory Core reference datum Core handling and processing Ill. Macroscopic stratigraphy General background Polar stratigraphy General observations and results Discussion of results and conclusions above 100 m IV. Detailed stratigraphic studies General background Macroscopic stratigraphy at 100 m Results of analysis and discussion Summary and conclusions V. Oxygen isotope studies General background Previous work Deep ice core 0-isotope stratigraphy Results of analyses Summary and conclusions Vl. Chemical composition studies General background Previous work Factors influencing the chemistry of glaciers Deep core stratigraphy using chemical variations Results of analyses and discussion Summary and interpretation of the 300 m results Geochemistry of the ice sheet Results of analyses and discussion Summary and conclusions Vll. Cosmic dust studies General background Previous work Origin of extraterrestrial dust Deep ice core and near surface studies Results of analyses Discussion of results Summary and conclusions VIII. Climatological implications General background Recent history of the inland ice Past history from the deep core Summary and conclusions- IX. Summary and conclusions Discussion Post Site l deep drilling programs Selected bibliography Appendix A. Sorge's law Appendix B. Thinning of layers Appendix C. Statistical terms Appendix D. Average density determinations for meter increments from the surface to 411.21 meters , Site 2, Greenland
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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-106
    In: Research report / Cold Regions Research and Engineering Laboratory, 106
    Description / Table of Contents: From the Preface: This paper presents a method for determining the extent of heat transfer due to vapor transfer in snow with air flowing through it, which could be useful in connection with studies concerning the changes of physical and mechanical properties of a snow cover caused by temperature gradients and wind currents.
    Type of Medium: Series available for loan
    Pages: iv, 8, A2, B2, C4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 106
    Language: English
    Note: CONTENTS Summary Introduction Theory Experimental apparatus apd procedures Results and discussion References Appendix A: Evaluation of d^2Ps/dx^2, dps/dx Appendix B: Sample calculations of β0, β, and De Appendix C: Experimental results and calculated data
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  • 24
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-42
    In: Research report / Cold Regions Research and Engineering Laboratory, 42
    Description / Table of Contents: Summary: The results of petrofabric studies in the laboratory on five samples of high-density snow collected in 1954 and 1955 at depths of 8.0, 15.5, 23.0, 34.2, and 46.3 m in a pit at Site 2 are reported. The porosity of the samples, the number of grains/cm^2, the mean number of adjacent grains per grain, the mean grain cross section, the size distribution of grain cross sections, and the orientation of c-axes were determined from enlarged photomicrographs of thin sections, using reflected light and transmitted polarized light. The number of adjacent grains per grain, the ratio of free to occupied grain surface, and the sphericity clearly depended on porosity and on each other. There was no strong relation between these data and the number of grains/cm^2. Hence, the structure of high density snow can be satisfactorily described by the porosity and the number of grains/cm^2 . Conclusions from a two-dimensional thin section can be applied to a spatial sample only if the sample is isotropic by strata.
    Type of Medium: Series available for loan
    Pages: iv, 24 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 42
    Language: English
    Note: CONTENTS Page Preface Summary Introduction Methods of preparation Measurements of structural properties Measurements on homogeneity and isotropy Results Structure data Orientation of c-axes Analysis of the distribution of the orientation of c-axes Preferred directions of the fabric Distribution of grain cross sections Size and shape of the counting areas Interrelations of the structure, data Conclusions Recommendations for further studies References
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  • 25
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-43
    In: Research report / Cold Regions Research and Engineering Laboratory, 43
    Description / Table of Contents: Summary: Charts of mean annual air temperature and precipitation over the ice cap are constructed on the basis of snow-profile studies at 8 locations, data collected for several years after 1953 at two U.S. Air Force weather stations, and records from expeditions since 1930. The warming trend in the Arctic appears to have occurred to a lesser degree on the ice cap, possibly because of the effect of the snow cover. The lowest mean annual temperature in South Greenland is estimated to occur within the area bounded by the 2500 m contour and the -18°C isotherm; mean annual temperature at 2700 is estimated as -20.9°C. In North Greenland, the mean annual temperature at 1700 m is estimated at -22°C. The presence of ice glands in the snow and daily max summer temperatures, estimated from records of coastal stations, indicate a potentially high incidence of melting at about 1300 m elevation and some melting at 1700 m in North Greenland, and melting up to 2700 m in the South. Annual accumulation is 2-3 times as great at 2500 m on the west side of the ice cap as at the crest. South of 66°N, precipitation may be about twice as great on the east side of the crest as in the west.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 43
    Language: English
    Note: CONTENTS Preface Summary Introduction Derivation of mean annual air temperature data Annual accumulation References
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  • 26
    Monograph available for loan
    Monograph available for loan
    New York : McGraw-Hill
    Call number: 6286
    Type of Medium: Monograph available for loan
    Pages: XIV, 280 Seiten , Illustrationen
    Series Statement: International series in pure and applied physics
    Language: English
    Location: Upper compact magazine
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  • 27
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-52
    In: Research report / Cold Regions Research and Engineering Laboratory, 52
    Description / Table of Contents: Summary: The results of studies on the physical properties of fog whiteout, as it occurred at Site 2 on the Greenland Ice Cap in the summers of 1956 and 1957, are reported and compared with the results of other studies; the instruments, methods of measurement, and data-reduction techniques used are described; and attempts at dissipating whiteout by AgI (silver iodide) seeding are discussed briefly. Emphasis was given to measurements of fog-particle size distribution, liquid-water content, relative humidity, visibility, and atmospheric nuclei. The data are tabulated. The synoptic situations for 2 selected cases of fog whiteout at relative humidities of less than 100% (possibly because of the presence of salt solutions) are described; and the balance between the rate at which water is made available in the air as it is lifted over the Ice Cap and the rate of water flux to the snow surface is computed using various equations. Efforts at fog dispersal by AgI seeding from the ground were inconclusive.
    Type of Medium: Series available for loan
    Pages: iv, 18, A1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 52
    Language: English
    Note: CONTENTS Preface Summary Introduction Definition of whiteout Scope of this study Instrumentation and observations Location of project: Fog particle measurements Atmospheric humidity measurements Visibility measurements Air temperature measurements Radiation measurements Atmospheric nuclei Observations of fog whiteout Conditions prior to onset of whiteout Conditions at time of arrival and during whiteout Micro-structure of fog whiteout Analysis of moisture balance during two selected cases Synoptic situation for case 1 Synoptic situation for case 2 Computations Attempts at fog whiteout dispersal References Appendix A - Freezing nuclei observations Appendix B - Absolute humidity gradient data
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  • 28
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-56
    In: Research report / Cold Regions Research and Engineering Laboratory, 56
    Description / Table of Contents: Summary: The results of laboratory creep tests in a shear apparatus at -5°C on 2 x2 x 3/8 in. samples of commercial ice, artificial single crystals, and 6 types of ice from the Greenland Ice Cap, at shear stresses of about 0.5-3 kg/cm^2 are reported. Some uniaxial tests were made at stresses from 6-28 kg/cm^2 to supplement the shear tests. Creep data could usually be represented approximately by one or more linear sections on a log-deformation vs log-time plot. The linear sections of the double logarithmic curve imply a creep curve of the form ε=ct^m where ε is the strain. For all samples tested, except single crystals sheared in easy glide, m averaged 0. 5 for shear deformations up to about 1%, and approached unity for more deformation. For single ice crystals oriented for easy glide, m averaged 1.7, implying a strain softening. Single crystals oriented for hard glide behaved similarly to polycrystals, indicating a rate-controlling process such as dislocation climb. For all but single easy-glide crystals, the minimum creep rate was tangent to the deformation curve at the end of the experiment. Creep rates for single easy-glide crystals were several hundred times larger than for the other crystals, the flow laws being similar.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 56
    Language: English
    Note: CONTENTS Preface Summary Introduction Types of ice Experiments Results Creep curves Flow law References
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  • 29
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-55
    In: Research report / Cold Regions Research and Engineering Laboratory, 55
    Description / Table of Contents: Summary: Experiments were performed to investigate the processes involved in the formation of sorted patterns which occur naturally in unconsolidated sandy gravel deposits covering the edge of the ice cap southeast of Thule, northwest Greenland. Four different glacier ice surfaces were covered with various thicknesses of sandy gravel in order to observe the effect of differential melting on the formation of sorted patterns. The different stages of pattern formation were recorded by photographs taken at 7-day intervals. A thin gravel cover of 2 in. allowed more rapid melting than did a cover of 6 in., with the result that depressions and mounds were formed. Coarse particles were segregated in the depressions by natural sorting of the various particle sizes when set in motion by differential melting and resulting uneven collapse of the gravel cover. The sorting produced well-developed stone rings in three of the areas, caused directly by the differential insulation provided by the gravel cover. In the fourth area a uniform gravel cover over a smooth ice surface produced no sorted nets, although a poorly developed stone stripe was formed in a melt-stream channel. A stone stripe was also formed in a stream channel cut into the ice along the edge of the test area. This stripe was composed of coarse particles which rolled down from the better insulated heights of the test area. It is therefore possible that sorted nets and stripes occurring naturally in the moraine deposits on the edge of the ice cap could have been formed by mechanical sorting induced by differential melting of the ice under a non-uniform layer of sandy gravel.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 55
    Language: English
    Note: CONTENTS Preface Summary Introduction Procedure Preparation of test plots Measurements of ice and gravel surfaces Composition of the gravel covering Results Sorting in a smooth layer of sandy gravel over an uneven ice surface Sorting in a uniform layer of sandy gravel over depressions in the ice surface Sorting in a uniform layer of sandy gravel over a uniform ice surface Sorting in a non-uniform layer of sandy gravel over a uniform ice surface Discussion and recommendations Conclusions References
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  • 30
    Call number: 21/SR 90.0917(1-3)
    Type of Medium: Series available for loan
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde 1, 2, 3
    Language: English
    Note: Nr. 1 Untersuchung der Polarisation und anderer Eigenschaften der langperiodischen Mikroseismik von Uwe Walzer (1969) , Nr. 2 Durchführung spezieller geophysikalischer Analogieexperimente und ihre Deutung von Horst Hänsel und Hans-Joachim Wilke (1969) , Nr. 3 Zur Einwirkung der Stativelastizität auf Amplituden und Phasen von Schwerependeln von Claus Elstner (1969)
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  • 31
    Call number: MOP Per 800(620)
    In: WMO, 620
    In: Technical note, 180
    Type of Medium: Monograph available for loan
    Pages: 99 S.
    Series Statement: WMO / World Meteorological Organization 620
    Language: English
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  • 32
    Call number: AWI G7-19-92221
    Type of Medium: Series available for loan
    Pages: Seiten 437 - 505 , Illustrationen
    Series Statement: Philosophical transactions of the Royal Society : Series A, Mathematical and physical sciences 265.1969,1166
    Language: English
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  • 33
    Monograph available for loan
    Monograph available for loan
    Paris : Organisation Européenne de Recherches Spatiales
    Call number: MOP 41394 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 55 Seiten , Illustrationen
    Series Statement: European Space Research Organization: Scientific note 54
    Language: English
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  • 34
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-20
    In: Research report / Cold Regions Research and Engineering Laboratory, 20
    Description / Table of Contents: Summary: Investigations on sea ice at Hopedale, Labrador, March 1956, included: small beam tests and in-place cantilever beam tests for flexural strength; ring tensile-strength tests; unconfined compression tests, with stress-strain studies to determine "Young's modulus"; and double shear tests. The results exhibit a great deal of scatter, primarily due to the inhomogeneity of sea ice. Ring tensile strength values range between 3.3 kg/cm^2 and 22.3 kg/cm2 between -2.5°C and -19.1°C. The small beam tests give flexural strength values from 0.5 to 17.3 kg/cm^2 in a similar temperature range. The in-place pull-up cantilever beam tests give flexural strength values of 2.2 to 4.0 kg/cm^2, with much less scatter. Crushing strength values range from 26.3 to more than 107 kg/cm^2 in the range -4.9°C to -18.3°C. Values for Young's modulus obtained from the slope of the straight line portion of the stress-strain curves in compression ranged between 4520 and 10,225 kg/cm^2. There is a temperature dependence, explained by the effect of change in brine content, on sea-ice structure. The double shear tests give values of 7.8 to 34.2 kg/cm^2 in the range -5.5°C to -12.8°C. These are higher than the tensile-strength values. These failures occurred normal to the direction of growth, while the tensile strength was obtained with failure parallel to it.
    Type of Medium: Series available for loan
    Pages: 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 20
    Language: English
    Note: CONTENTS Page Preface Summary Introduction Ring tensile strength Flexural strength of small beams Flexural strength of inplace beams Crushing strength Shear strength Discussion of results References
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  • 35
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-87
    In: Research report / Cold Regions Research and Engineering Laboratory, 87
    Description / Table of Contents: Abstract: A consistent theory of plane plastic deformation of soil is formulated by assuming soil as an ideal material that has constant cohesion and friction angle. Such an ideal soil is an extension of the ideal metal that has, in the terminology of soil mechanics, cohesion only. After a review of the existing theories from which the present theory has emerged, the mathematical expression referred to as the "compression characteristic" is developed. Then the system of differential equations is shown by the theory of characteristic lines. Many mathematical and physical problems remain to be solved before the perfect explanation of the plasticity of ideal soil will be attained.
    Type of Medium: Series available for loan
    Pages: iv, 42 Seiten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 87
    Language: English
    Note: CONTENTS Preface Summary Introduction Review of existing theories The compression characteristic Characteristic directions Conclusions Literature cited Appendix A. Proof of Yamaguchi's principle Appendix B. Strain-rate tensor in the strain-rate characteristic line coordinates Appendix C. Stress, strain-rate relationship Appendix D. Bearing on the. Drucker and Prager three -dimensional deformation Appendix E. Notation
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  • 36
    Monograph available for loan
    Monograph available for loan
    Toronto : Atmospheric Environment Service, Environment Canada
    Call number: MOP 42751 / Mitte
    Type of Medium: Monograph available for loan
    Pages: V, 60, 25 Seiten , Illustrationen
    Series Statement: Canadian meteorological memoirs 25
    Language: English
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  • 37
    Monograph available for loan
    Monograph available for loan
    Amsterdam : Elsevier
    Call number: MOP 43353 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XII, 347 Seiten , Illustrationen , 2 Beilagen , 23 cm
    Language: English
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  • 38
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-59
    In: Research report / Cold Regions Research and Engineering Laboratory, 59
    Description / Table of Contents: Summary: The deflection expression of an infinite plate subjected to a concentrated force is used with the "method of images" to obtain solutions for 6 plates with simply supported edges. The semi-infinite plate, the wedge-shaped plate, and its special case, the rectangular corner plate, are solved in closed form; and the infinite strip, the semi-infinite strip, and the rectangular plate are solved as rapidly convergent series. Behavior under a concentrated force is studied in more detail for the semi-infinite plate and the rectangular corner plate. Relationships for obtaining bending moments, shear forces and reaction distributions as well as derivatives of the kei-function with respect to ? and ? are given in the appendices.
    Type of Medium: Series available for loan
    Pages: iv, 12, [2] Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 59
    Language: English
    Note: CONTENTS Preface Introduction and statement of the problem Solution of the boundary value problems for simply supported boundaries Semi-infinite plate Wedge-shaped plate Rectangular corner plate Infinite strip Semi-infinite strip Rectangular plate Remarks on the problem of arbitrary load distribution References Appendix A Appendix B
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  • 39
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-109
    In: Research report / Cold Regions Research and Engineering Laboratory, 109
    Description / Table of Contents: Summary: The present paper contains a critical study of a number of foundation models suggested by various investigators, as well as a further development of some of the ideas involved. It is found that the model by Pasternak is the most natural extension of the Winkler foundation. It is also shown that the "non-solvability" of the problem of a finite bean or plate resting on a continuous foundation as posed by Wieghardt and further elaborated by Pflanz is not correct, and that problems of this type are solvable for any load distribution permissible in classical plate theory. The paper concludes with derivations of differential equations for plates resting on viscous and viscoelastic foundations, which may be used for solving problems involving compacted snow and permafrost bases.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 109
    Language: English
    Note: CONTENTS Preface Summary Introduction The Hetényi foundation The Filonenko-Borodich foundation The Pasternak foundation Plates on a Pasternak foundation Visco-elastic Pasternak foundation Plates on visco-elastic foundations References Appendix A: Notation
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  • 40
    Call number: ZSP-202-111,2
    In: Research report / Cold Regions Research and Engineering Laboratory, 111,2
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    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 111,2
    Language: English
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  • 41
    Call number: 10.1144/GSL.SP.1967.002.01.01 (e-book)
    In: Special publications / the Geological Society, London, Volume 2
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 827 Seiten)
    Series Statement: Special publications / the Geological Society, London 2
    Language: English
    Note: Table of Contents Introduction Geological Society, London, Special Publications, 2, 1-11, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.01 The symposium meeting Geological Society, London, Special Publications, 2, 13-14, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.02 Part I: Symposium Papers Introduction to Part I Geological Society, London, Special Publications, 2, 15-16, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.03 Life in Pre-Cambrian and early Cambrian times John Watson Cowie Geological Society, London, Special Publications, 2, 17-35, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.04 The significance of certain trace-fossil ranges Roland Goldring Geological Society, London, Special Publications, 2, 37-39, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.05 Fluctuations in the evolution of Palaeozoic intertebrates Michael Robert House Geological Society, London, Special Publications, 2, 41-54, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.06 The origins of some Silurian enteletacean brachiopods Victor Gordon Walmsley Geological Society, London, Special Publications, 2, 55-56, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.07 Permo-Triassic extinction Frank Harold Trevor Rhodes Geological Society, London, Special Publications, 2, 57-76, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.08 Changes in terrestrial vertebrate faunas during the Mesozoic C. B. Cox Geological Society, London, Special Publications, 2, 77-89, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.09 Some Cretaceous-Tertiary marine faunal changes John Michael Hancock Geological Society, London, Special Publications, 2, 91-104, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.10 Major features of the evolution of echinoids Graeme Maxwell Philip Geological Society, London, Special Publications, 2, 105-106, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.11 Plant-insect relationships in Palaeozoic and later time Norman Francis Hughes and John Smart Geological Society, London, Special Publications, 2, 107-117, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.12 Biochemical evolution and the fossil record Lambert Beverly Halstead Tarlo Geological Society, London, Special Publications, 2, 119-132, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.13 Fossil birds and their adaptive radiation James Fisher Geological Society, London, Special Publications, 2, 133-154, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.14 General Discussion Geological Society, London, Special Publications, 2, 155-156, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.15 Part II: Documentation of the Fossil Record Introduction to Part II Geological Society, London, Special Publications, 2, 158-159, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.16 Plantae Plantae N. F. H. Geological Society, London, Special Publications, 2, 162, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.17 Chapter 1 Thallophyta—1 H. P. Banks, K. I. M. Chesters, N. F. Hughes, G. A. L. Johnson, H. M. Johnson and L. R. Moore Geological Society, London, Special Publications, 2, 163-180, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.18 Chapter 2 Thallophyta—2 M. Black, C. Downie, R. Ross and W. A. S. Sarjeant Geological Society, London, Special Publications, 2, 181-209, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.19 Chapter 3 Bryophyta and Charophyta* L. J. Grambast and W. S. Lacey Geological Society, London, Special Publications, 2, 211-217, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.20 Chapter 4 Pteridophyta—1 H. P. Banks, W. G. Chaloner and W. S. Lacey Geological Society, London, Special Publications, 2, 219-231, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.21 Chapter 5 Pteridophyta—2 H. P. Banks, M. G. Collett, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 233-245, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.22 Chapter 6 Gymnospermophyta K.L. Alvin, P. D. W. Barnard, T.M. Harris, N. F. Hughes, R. H. Wagner and A. Wesley Geological Society, London, Special Publications, 2, 247-268, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.23 Chapter 7 Angiospermae K. I. M. Chesters, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 269-288, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.24 Invertebrata Invertebrata M. J. S. R. Geological Society, London, Special Publications, 2, 290, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.25 Chapter 8 Protozoa F. T. Banner, W. J. Clarke, J. L. Cutbill, F. E. Eames, A. J. Lloyd, W. R. Riedel and A. H. Smout Geological Society, London, Special Publications, 2, 291-332, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.26 Chapter 9 Porifera and Archaeocyatha R. M. Finks and D. Hill Geological Society, London, Special Publications, 2, 333-345, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.27 Chapter 10 Coelenterata G. A. L. Johnson, I. D. Sutton, F. M. Taylor and G. Thomas Geological Society, London, Special Publications, 2, 347-378, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.28 Chapter 11 Bryozoa G. P. Larwood, A. W. Medd, D. E. Owen and R. Tavener-Smith Geological Society, London, Special Publications, 2, 379-395, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.29 Chapter 12 Brachiopoda D. V. Ager, P. Copper, G. M. Dunlop, G. F. Elliott, F. A. Middlemiss, A. J. Rowell, A. Williams and A. D. Wright Geological Society, London, Special Publications, 2, 397-421, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.30 Chapter 13 Mollusca: Amphineura, Monoplacophora and Gastropoda D. Curry and N. J. Morris Geological Society, London, Special Publications, 2, 423-430, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.31 Chapter 14 Mollusca: Cephalopoda (Nautiloidea) C.H. Holland Geological Society, London, Special Publications, 2, 431-443, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.32 Chapter 15 Mollusca: Cephalopoda (Ammonoidea) D. T. Donovan, F. Hodson, M. K. Howarth, M. R. House, E. T. Tozer and C. W. Wright Geological Society, London, Special Publications, 2, 445-460, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.33 Chapter 16 Mollusca: Cephalopoda (Coleoidea) D. T. Donovan and J. M. Hancock Geological Society, London, Special Publications, 2, 461-467, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.34 Chapter 17 Mollusca: Scaphopoda and Bivalvia N. J. Morris Geological Society, London, Special Publications, 2, 469-477, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.35 Chapter 18 Arthropoda: Protarthropoda and Trilobitomorpha J. W. Cowie, W. T. Dean, R. Goldring, W. D. I. Rolfe, A. W. A. Rushton, J. T. Temple and R. P. Tripp Geological Society, London, Special Publications, 2, 479-497, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.36
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  • 42
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-37
    In: Research report / Cold Regions Research and Engineering Laboratory, 37
    Description / Table of Contents: Summary: Laboratory experiments on the air permeability of various screened and natural snows are described, and, results are analyzed to determine whether the parameters obtained from the measurements could be used to define a snow type. The permeability of a snow sample of known porosity (calculated from density) was determined over a wide range of air velocities; the sample was then compacted artificially a few mm, its density was determined, and its permeability measured again. The procedure was used to obtain curves for several densities of the same sample. Air flow appeared laminar for velocities less than 5 cm/sec in fine-grained snow (less than 0.8 mm in diam.), 2 cm/sec in medium-grained snow (0.8-1.2 mm diam.), and 1 cm/sec in larger-grained snow. A formula is presented expressing all of the results obtained under laminar-flow conditions in a single relationship, and an equation for estimating grain size from initial permeability and initial porosity is suggested. Snow conversion tables and a discussion of the effect of varying sample porosity on its permeability are appended.
    Type of Medium: Series available for loan
    Pages: iv, 19, A2, B6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 37
    Language: English
    Note: CONTENTS Page Preface Summary Introduction Apparatus and method Experimental results and discussion Historical background Range of Darcy's law Effect of porosity on the permeability of snow Bader's equation Conclusion References Appendix I. Snow conversion table: Density to absolute porosity Appendix II. Effect on permeability of varying porosity in the sample Porosity varies with length Porosity varies with cross section
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  • 43
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-39
    In: Research report / Cold Regions Research and Engineering Laboratory, 39
    Description / Table of Contents: Summary: An analysis of snow-cover density, temperature, and hardness data, measured over a period of several years at five stations in Alaska and six stations in the Canadian Arctic, shows the snow cover in the Canadian Archipelago to be colder, denser, and harder than in the interior of Alaska. A series of nomographs were developed to estimate average monthly snow-cover density from mean monthly air temperature and wind velocity. The nomographs are applicable for the months November through March, for the Alaskan and Canadian area north of 62°N latitude, and for elevations below 1500 ft. A comparison of observed snow-cover densities with those derived from the nomographs indicates that the method will provide a reliable regional estimate of snow-cover density. Studies of the relation between snow-cover temperature and air temperature from November through March disclosed the snow to be on the average from 4°C to 9°C warmer than the air at the Alaskan stations and 4.5°C warmer at the Canadian Archipelago stations. An investigation of snow-cover hardness revealed regional variations similar to that for density. Measured snow hardness during the period of no melting was found to be related to densities between 0.15 and 0.36 g/cm^3.
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    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 39
    Language: English
    Note: CONTENTS Preface Summary Introduction Climatic parameters which may affect arctic snow-cover density Results of study Regional variations in snow-cover density Prediction of average monthly snow-cover density in the arctic from air temperature and wind velocity Comparison of observed snow-cover density with density computed from the nomographs Relation between snow-cover temperature and air temperature Relation between hardness and density of the snow cover References
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  • 44
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-41
    In: Research report / Cold Regions Research and Engineering Laboratory, 41
    Description / Table of Contents: Summary: Laboratory experiments on the creep of sifted snow under uniaxial, hydrostatic, and confined-side compressive stresses are described, and the results are discussed on the basis of an additive theory for combined stresses. Stress (4-40 psi) and temperature (-3.6°C to -13.6°C) dependence was investigated for 35 samples (initial density = 0.4 g/cm^3) subjected to uniaxial and hydrostatic stress for 200-sec time increments. Another series of 104 samples (initial densities 0.36-0.63) was subjected to uniaxial, hydrostatic, and confined-side compressive stresses until an arbitrary change in density was reached. In all cases the applied stress ultimately became a shear stress acting between grains, the open structure reacting differently to combined stresses and separate uniaxial stresses. An activation energy of 13,400 cal/mol was obtained from the first group of tests.
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    Pages: iv, 12 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 41
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental General Apparatus Procedure Theoretical relations Additive theory Relationship between tests run for constant change in density and tests for constant time Results and discussion Group I experiments Group II experiments Stress dependence for group II tests Variability Time dependence Activation energy Relations between creep rates under different stress conditions Density dependence Lateral stress for confined-side tests Conclusions References
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  • 45
    Monograph available for loan
    Monograph available for loan
    London : Univ. of London Press
    Call number: PIK N 456-16-90109
    Type of Medium: Monograph available for loan
    Pages: XVI, 223 S. , graph. Darst., Kt.
    Language: English
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  • 46
    Monograph available for loan
    Monograph available for loan
    New York u.a. : McGraw-Hill
    Call number: PIK N 456-16-90110
    Type of Medium: Monograph available for loan
    Pages: X, 540 S.: Ill., graph. Darst., Kt.
    Edition: 3.ed.
    Language: English
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  • 47
    Monograph available for loan
    Monograph available for loan
    Dublin : Department of Transport and Power, Meteorological Service
    Call number: MOP 36777
    Type of Medium: Monograph available for loan
    Pages: 72 Seiten , Illustrationen, Tabellen
    Language: English
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  • 48
    Call number: MOP 40553 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 176 Seiten
    Language: English
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  • 49
    Monograph available for loan
    Monograph available for loan
    Boston : American Meteorological Society
    Call number: MOP 40509 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 347 Seiten , Illustrationen
    Language: English
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  • 50
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 43365 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 338 Seiten , Illustrationen , 3 Karten , 27 cm
    Series Statement: Meždunarodnoe Gidrologičeskoe Desjatiletie / AN SSSR. Institut Geografii
    Language: Russian , English
    Note: In kyrillischer Schrift , Mit Zusammenfassung und Inhaltsverzeichnis in englischer Sprache
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  • 51
    facet.materialart.13
    facet.materialart.13
    [Philadelphia] : American Meteor Society
    Call number: MOP S 7298
    In: Meteoritics
    Type of Medium: 13
    Pages: Seite 366-385 , Tabellen
    Edition: Sonderdruck reprinted from Meteoritics Vol. 1, No. 3, 1955
    Series Statement: Meteoritics Vol. 1, No. 3
    Language: English
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  • 52
    Call number: MOP 41371 / Mitte
    In: WMO / World Meteorological Organization
    Type of Medium: Series available for loan
    Pages: X, 145 Seiten , Illustrationen
    Language: English
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  • 53
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41126 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 1
    Language: English
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  • 54
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41127 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 2
    Language: English
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  • 55
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-18
    In: Research report / Cold Regions Research and Engineering Laboratory, 18
    Description / Table of Contents: Summary: Various strength properties of naturally compacted high-density snows, in the density range of from 0.40 to 0.75 g/cm^3, are reported. Test results are given for: unconfined compression; unconfined and confined double shear; ring, flexural, and centrifugal tensile strength; torsional shear; and work of disaggregation. The work of disaggregation per unit volume was related to crushing, tensile, and shear strength at various lateral pressures, using the same empirical relationship. The results of the various tests measuring the tensile strength of the snow compare favorably with each other. An attempt was made to use the direct shear strength results in Coulomb’s equation for the determination of Mohr’s envelope of rupture for snow. These tests yield higher values than those obtained in unconfined compression tests. However, angles of internal friction obtained considering Mohr’s envelope to be straight line seem to agree with measurements taken on an unconfined compression specimen.
    Type of Medium: Series available for loan
    Pages: 19 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 18
    Language: English
    Note: CONTENTS Page Preface Summary Introduction Temperature correction factors Crushing strength Tensile strength · Shear strength Torsional shear strength Work of disaggregation of snow Angle of internal friction and apparent unit cohesion Discussion of results References
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  • 56
    Series available for loan
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-17
    In: Research report / Cold Regions Research and Engineering Laboratory, 17
    Description / Table of Contents: Summary: The ice-cored moraine which occurs on the margin of the Greenland Ice Cap, east of Thule Air Base, was investigated during the summers of 1954 and 1955. A synthesis of the field data gathered leads to the following conclusions: 1.) The outer zone of the ice margin is composed of stagnant ice which acts as a barrier to movement of mobile ice from the interior. 2.) The mobile ice overrides the barrier zone in a series of high angle imbricate shears. 3.) These shears carry old ground moraine from the subglacial floor toward the surface. 4.) Differential ablation on the surface results in the formation of ice-cored moraine ridges, parallel to the strike of the shear. 5.) Recent stagnation and recession of the ice margin in the Thule area has resulted in the formation of a belt of successive shear moraines. 6.) Geomorphic processes in addition to ablation (particularly wind action) control the surface expression of the shear moraines. 7.) Subglacial topography is the primary control on the trend of both ice edge and moraine ridges. 8.) The complex Thule Ramp shear moraine has resulted from a faster-moving ice mass to the north overriding the Thule Ramp ice. 9.) The prominent ice cliffs are manifestations of erosion by wind and water. 10.) The tunnel in the Thule Ramp ice cliff indicates a former development of shear moraine in the area. 11.) Structural and geomorphic features indicate glacial cycles in the area of both long and short duration. 12.) The shear moraines in the Thule area offer a possible explanation for the mode of ground moraine deposition in some areas of continental glaciation during the late Pleistocene. The work done in 1954 and 1955 was in the nature of a glacial geomorphologic reconnaissance. Intensive study remains to be done, particularly in the Thule Ramp area, on ice structure, movement, and ablation before a complete understanding of both present and past glacial regimes can be reached.
    Type of Medium: Series available for loan
    Pages: vi, 46, [2] Seiten , Illustrationen , 27 cm
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 17
    Language: English
    Note: CONTENTS Introduction I. Physiographic description of study area II. Structure of the marginal zone of the ice cap III. Geomorphologic processes IV. Recent glacial history of the ice margin
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  • 57
    Call number: MOP 41158 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 122 Seiten , Illustrationen
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  • 58
    Call number: AWI G1-19-92268
    In: University of California publications in geological sciences, Volume 85
    Type of Medium: Monograph available for loan
    Pages: V, 101 Seiten , Illustrationen
    Series Statement: University of California publications in geological sciences 85
    Language: English
    Note: Contents: Abstract. - Introduction and Acknowledgements. - Metamorphic basement. - Plutonic rocks. - Review of plutonism in Central America, excluding Honduras. - Plutonic rocks of Honduras. - Mesozoic and eocene rocks. - General statement. - Vallę de Angeles group. - Esquias formation. - Matagalpa Formation. - Subinal redbeds. - Ignimbrites. - The pre-ignimbrite surface. - Thickness of the ignimbrites. - Lithology and mineral composition. - Associated lavas. - Ignimbrite vents. - Fluviatile and lacustrine beds associated with ignimbrites. - Age and correlation. - Chemical composition - major elements. - Origin of ignimbrite magmas. - Dikes. - Borderlands of the Gulf of Fonseca. - The Gracias Formation. - Quaternary Volcanism. - General statement. - Description of individual volcanic fields. - Gulf of Fonseea. - Volcanoes of the central highlands. - The Lake Yojoa volcanic field. - Lavas in the Sula graben. - Utila Island. - Geologic structure of Honduras. - Appendix: Microscopic Petrography. - A. Plutonic rocks. - B. Andesites and basalts of the Matagalpa Formation. - C. Lavas of the Gulf of Fonseca sequence. - D. Dike rocks. - E. Ignimbrites. - F. Quaternary lavas. - Literature cited.
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  • 59
    Monograph available for loan
    Monograph available for loan
    Cambridge : University Press
    Call number: AWI G1-19-92304
    Type of Medium: Monograph available for loan
    Pages: XVI, 420 Seiten , Illustrationen
    Edition: Fourth edition
    Language: English
    Note: Contents: I The mechanical properties of rocks. - II The theory of elastic waves. - III Observational seismology. - IV The theory of the figures of the earth and moon. - V The figures of the earth and moon. Discussion of observations. - VI Stress-differences in the earth. - VII The variation of latitude and the bodily tide. - VIII Tidal friction. - IX The age of the earth. - X The thermal history of the earth. - XI The origin of the earth's surface features. - XII Special problems. - Appendices. - A Critical stress-difference. - B The straining of a uniform sphere. - C Castigliano's principle. - D Cooling of a sphere. - E Long-period tides. - Notes. - Bibliography. - Index.
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  • 60
    Call number: MOP 41085 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIII, 144 Seiten , Illustrationen
    Language: English
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  • 61
    Series available for loan
    Series available for loan
    Hanover, NH : Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-96
    In: Research report / Cold Regions Research and Engineering Laboratory, 96
    Description / Table of Contents: Techniques were established by which quantitative data can be obtained from patterned ground features. The field work was carried out during the summers of 1954 and 1955 near Camp Tuto, Greenland. The investigation site is described, and extensive data are presented. The soil materials composing the patterned ground features were found to be of common mineralogy, grain size distribution, and plasticity. The chemical nature of the soils does not contribute to feature formation; it is the mechanical processes acting on these materials that are important. A sharp rise in the soil water content in the form of ice was consistently noted when passing through the base of the active layer into the present permafrost. A net heave occurred at both feature center and border locations, The magnitude of the heave is about 0.05 ft for the centers and 0.03 ft for the borders. Feature age was estimated to be about 150 yr. Vertical sorting occurs over the entire depth of the active layer but radial sorting is confined to the upper 2 ft. Groundwater flow occurs mostly through the feature borders, and incoming radiation has an important effect on the progression of the frost line. The progression of thaw is very rapid and, by the end of summer, the thaw penetration is greatest under the feature centers.
    Type of Medium: Series available for loan
    Pages: VI, 76 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 96
    Language: English
    Note: CONTENTS Preface Summary Introduction Site of investigation Selection of study area General information about site and vicinity Accumulation and initial evaluation of data Feature 1 - preliminary study (raised center feature) Feature 2 - bench mark excavation - preliminary soils study (depressed center feature) Feature 3 - cobble orientation study Feature 4 - precise movement survey Feature 5 - radial comparison studies Feature 6 - moisture content survey Feature 7 - temperature and heat flow study (depressed center feature) Feature 8 - temperature and heat flow study (raised center feature) Feature 9 - ground water table studies Features 10 and 11 - permafrost table survey (depressed and raised center features) Combined analysis of data Sharp rise in water content at frost table Estimate of heave since deposition Study of heave measurements Consideration of feature formation time Soil grain size distribution within features Conclusions Recommendations for future work in this or similar patterned ground study areas Heave and ground-ice accumulation Solifluction ground flow Incoming radiation and soil albedo References Appendix A: General. study of heat budget of the active layer
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  • 62
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-116
    In: Research report / Cold Regions Research and Engineering Laboratory, 116
    Description / Table of Contents: Abstract: Specimens of snow from the South Pole were tested to investigate air permeability K (cm/sec), ultimate compressive strength σc (g/cm^2 ) and dynamic Young's modulus E (g/cm^2 ) as a function of density. Anisotropy in a single layer of snow (snow between two summer crusts) was found in all three properties. Comparison with data for snow from Site II, Greenland, showed an empirical relation for both areas: σc = 10.42 x 10^-4 E for 0.43 g/cm^3 〈 ρ 〈 0.51 g/cm^3. σc = 5.68 x 10^-4 E for 8.63 x 10^3 g/cm^2 for 0.51 g/cm^3 〈 ρ 〈 0.90 g/cm^3. Air permeabilities are different for the two sites because of time and meteorological effects.
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 116
    Language: English
    Note: CONTENTS Preface Summary Introduction Preparing the snow specimens Air permeability Experimental procedure Results and discussion Viscoelastic properties Principle Experimental method Results and discussion Creep tests Unconfined compressive strength Experimental procedure Results and discussion General discussion Literature cited Appendix A: Test result
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  • 63
    Monograph available for loan
    Monograph available for loan
    Washington D.C. : Environmental Science Services Administration National Aeronautics and Space Administration United States Air Force
    Call number: MOP 40337 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XX, 289 Seiten , Illustrationen
    Language: English
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  • 64
    facet.materialart.12
    facet.materialart.12
    London : Geological Society of London
    Call number: 10.1144/GSL.SP.1969.003.01.01
    Type of Medium: 12
    Pages: 1 Online-Ressource (VIII, 311 Seiten)
    Series Statement: Special publications / the Geological Society, London 3
    Language: English
    Note: Table of Contents Introductory Remarks Displacement within continents Introductory remarks R. M. Shackleton Geological Society, London, Special Publications, 3, 1-7, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.01 Structural Analysis of Orogenic Belts Problems of the relationship between surface structure and deep displacements illustrated by the Zagros Range N. L. Falcon Geological Society, London, Special Publications, 3, 9-21, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.02 Some principles governing interpretation of structure in the Rocky Mountain orogenic belt F. G. Fox Geological Society, London, Special Publications, 3, 23-41, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.03 The measurement of strain and displacement in orogenic belts J. G. Ramsay Geological Society, London, Special Publications, 3, 43-79, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.04 The construction of sections in areas of highly deformed rocks W. E. A. Phillips and J. G. Byrne Geological Society, London, Special Publications, 3, 81-93, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.05 The palaeomagnetic evidence of displacements within continents D. H. Tarling Geological Society, London, Special Publications, 3, 95-113, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.06 Historical Analysis of Orogenic Belts Interpretation of stratigraphical ages in orogenic belts W. B. Harland Geological Society, London, Special Publications, 3, 115-135, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.07 Interpretation of isotopic ages in orogenic belts P. E. Brown and J. A. Miller Geological Society, London, Special Publications, 3, 137-155, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.08 A new approach to radio-isotopic dating in orogenic belts F. J. Fitch, J. A. Miller and J. G. Mitchell Geological Society, London, Special Publications, 3, 157-195, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.09 Other Analyses Orogenic belts and their parts N. Rast Geological Society, London, Special Publications, 3, 197-213, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.10 Sedimentary thicknesses in orogenic belts R. Stoneley Geological Society, London, Special Publications, 3, 215-238, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.11 Rates of change within orogenic belts J. Sutton Geological Society, London, Special Publications, 3, 239-250, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.12 The deep structure of orogenic belts—the root problem E. R. Oxburgh Geological Society, London, Special Publications, 3, 251-273, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.13 Orogeny in relation to crust and upper mantle M. H. P. Bott Geological Society, London, Special Publications, 3, 275-283, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.14 Internal features of some orogenic belts of Africa T. N. Clifford Geological Society, London, Special Publications, 3, 285-287, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.15 Closing Remarks Displacement within continents Kingsley Charles Dunham Geological Society, London, Special Publications, 3, 289-290, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.16 Discussion Geological Society, London, Special Publications, 3, 291-308, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.17
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  • 65
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-30
    In: Research report / Cold Regions Research and Engineering Laboratory, 30
    Description / Table of Contents: Summary: Deformations occurring in a tunnel, two trenches, and a 30 m deep pit excavated in the Greenland névé in the summer of 1954 have been measured over a period of 2 years. The experimental results indicate that closure rates increase with lateral distance from a restraining boundary up to distances of about 1 m. At larger distances, the effect of the boundary is not appreciable. Closure rates for deep excavations are not found to be strongly depth-dependent. This is due to a roughly parallel increase of viscosity and pressure with depth. Vertical compaction results from the pit agree well with those calculated from the depth-density relation using Sorge's Law. A theoretical calculation for the tunnel and pit closure, which is a modification of existing theories for the deformation of an elastic, compressible, thick-walled cylinder, is in fair agreement with the observed deformations. From this agreement it appears that the flow behavior of the névé can be described on the basis of a Newtonian viscosity. The trench closure is described as the-squeezing out of horizontal layers, fixed at some distance from the trench, and modified only slightly by the drag of neighboring layers. Measurements will be continued during future summers.
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    Pages: iv, 14 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 30
    Language: English
    Note: CONTENTS Preface Summary Introduction Measurements and results Tunnel North-south trench East-west trench Deep pit Theoretical development Sorge's Law Deformation of acylindrical tunnel in a viscous compressible medium Discussion Tunnel Trenches Deep pit References Appendix
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  • 66
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-31
    In: Research report / Cold Regions Research and Engineering Laboratory, 31
    Description / Table of Contents: Summary: Studies were conducted on 58 snow-ice beams (7.5 cm wide, 10.0 cm high, and 56.0 cm long) ranging in density from 0.621 - 0.719 g/cm^3 under varying loads, at uniform loading rates (except for 23 beams which were tested with repeated loading), and at a constant temperature of -5 ± 0.5°C. All beams were tested to failure. The modulus of elasticity of the beams increased with density and loading rate. The modulus of elasticity ranged from 1.35 x 10^4 to 2.22x 10^4 kg/cm^2 for densities of 0.621 - 719 g/cm^3 respectively. A variation in the relative time of deflection from 42 - 23 sec/0.0200 cm gave a variation in the modulus of elasticity from 1.22 x 10^4 to 1.42 x 10^4 kg/cm^2. The modulus of rupture was roughly a linear function of density, increasing from 7.79 - 11.54 kg/cm^2 with density. Failure of the beams was sudden, with a conchoidal fracture occurring in the middle third of the span, and appeared to be a combination of shear and flexure.
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    Pages: iv, 9, A4, B10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 31
    Language: English
    Note: CONTENTS Preface Summary Introduction Method Procedure Test results Tests conducted Data and calculations Discussion of results References Appendix A. Drawings of apparatus Appendix B. Load-deflection and time-deflection curves for snow beams of various densities
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  • 67
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    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-32
    In: Research report / Cold Regions Research and Engineering Laboratory, 32
    Description / Table of Contents: Summary: Apparatus was built for deforming ice crystals under hydrostatic pressures up to 350 atmospheres. Single crystals were placed in the mounts in such a way that the deformation occurred by gliding on the basal glide plane. It was found that the shear strain rate increased as the pressure was increased at constant temperature, but that the rate is practically independent of hydrostatic pressure when the difference between the ice temperature and the melting point is kept constant.
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    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 32
    Language: English
    Note: CONTENTS Preface Summary Introduction Test apparatus and experimental procedures Experimental results Conclusions References
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  • 68
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    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-33
    In: Research report / Cold Regions Research and Engineering Laboratory, 33
    Description / Table of Contents: Summary: A series of deformation measurements have been selected for preliminary studies on the plasticity of Greenland glacier ice. The measurements to be reported on were obtained in the Red Rock and TUTO tunnels in Northwest Greenland. Both tunnels were excavated during the summer of 1955 with some additional work done during the summer of 1956. Deformation measurements made up to the end of the 1956 summer season, therefore, are of limited reliability, but certain trends appearing in these data seem worth reporting. The topics discussed are (1) the shearing of an initially vertical peg system at Red Rock, (2) the deformation of core holes at TUTO, and (3) tunnel closure at both sites. These data are analyzed on the basis of laminar flow of the Nye type and certain conclusions are derived.
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    Pages: 6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 33
    Language: English
    Note: CONTENTS Introduction Experimental Analysis The shear of glaciers Tunnel closure Conclusions References
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  • 69
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    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-36
    In: Research report / Cold Regions Research and Engineering Laboratory, 36
    Description / Table of Contents: Summary: Measurements were made with 22 more or less hydrophobic polymers and lacquers at intervals of 5 or 10 min for periods up to 1 hr. All surfaces were carefully cleaned, and some surfaces were baked. Highest initial (time 0) average contact angles ( 106° - 106.6°) were measured for Foster Snell rain repellant wax, Barrett 25-218 water repellant varnish (air-dried), and Cardolite NRL-7241. After 40 min, contact angles for these substances were 95.6°, 90.9°, and 91.0°. The measurement apparatus is illustrated, and data are tabulated.
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    Pages: ii, 11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 36
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Apparatus Materials Procedure Experimental results References
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  • 70
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-34
    In: Research report / Cold Regions Research and Engineering Laboratory, 34
    Description / Table of Contents: Summary: The compressive strength of snow cylinders was investigated as a function of age of snow, snow-particle size, and age of the cylinders. The effect of gases such as carbon dioxide, methane, and ammonia on the strength of snow cylinders has also been studied. The experimental results show that the older the snow from which snow cylinders are made, the smaller the compressive strength. The compressive strength of cylinders decreases with the snow particle size. An equation describing the aging curves for snow cylinders is presented. Whereas carbon dioxide and methane in small quantities have no effect on the compressive strength, ammonia appreciably lowers the compressive strength of snow cylinders. All strength measurements were carried out at -10°C.
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    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 34
    Language: English
    Note: CONTENTS Page Preface Summary Introduction Experimental Materials Apparatus and technique Preparation of snow fractions Experimental results Aging of snow cylinders Compressive strength as a function of particle size Mixture of fractions Influence of gases on the compressive strength of snow Discussion References
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  • 71
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-50
    In: Research report / Cold Regions Research and Engineering Laboratory, 50
    Description / Table of Contents: Summary: Samples of cryoconite from the Nuna ramp area in Northwest Greenland have been analyzed for the mineral and cryptogamic content. The non-mineral content of the blue-black gelatinous, drip-free cryoconite was found to be about 95% of the wet mass. After drying and ashing, the organic matter comprised 13.9 to 20% of the oven-dry sample. The mineral matter was predominately fine-grained, sharp-edged grains from 1 mm or larger to microscopic in size and appeared to have been wind-borne from the adjacent nunataks and moraines. The organic matter was found to be largely algae with inclusion of fungi and a rotifer. Since algae utilize radiation primarily in the blue region between 0.40 μ and 0.65 μ, where ice has the greatest transmissivity, it is possible that the cryoconite holes are at least partly the product of energy released by photosynthetic and metabolic processes rather than by direct absorption of red or heat-wave lengths of solar radiation by the dark cryoconite. The uniformity in the pattern and dimensions of the cryoconite holes supports the assumption that biological processes are dominant in their formation and growth.
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    Pages: iv, 12, A2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 50
    Language: English
    Note: CONTENTS Preface Summary Introduction Observations on the Nuna ramp Sample collection Distribution of the cryoconite holes Observations in the Thule ramp Physical analyses of the cryoconite Biological assay of the cryoconite References Appendix: A study of the bacteria and fungus content of the cryoconite of the Thule area
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  • 72
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    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-46
    In: Research report / Cold Regions Research and Engineering Laboratory, 46
    Description / Table of Contents: Summary: The results of studies in the summer of 1957 on ice samples taken from the ice tunnel at TUTO, core samples obtained by drilling in the ice cap at Site 2, and snow samples, using the transverse vibration method and a new portable meter, are reported. Young's modulus was determined from the resonance frequency of flexural vibrations of samples cut in the form of rectangular bars; the loss factor was measured from damping; and the coefficient of viscosity calculated using the Maxwell model. The modulus of elasticity of samples of a density from 0.917 - 0.90 g/cm^3 (tunnel ice) decreased sharply with slight deviations of the density from that of pure ice. At densities from 0.90 - 0.50 g/cm^3 (deep-pit and drill-core samples) the relation between the modulus of elasticity and density was linear, while in the density range from 0.50-0.25 g/cm^3 (surface snow) the modulus of elasticity decreased exponentially. The viscosity-density relation of the samples was similar to that of elasticity vs density. Young's modulus increased slightly with decreasing temperature, while viscosity increased exponentially. The activation energy was calculated as 18.7 kcal/mol for old ice-cap ice, 13.9 kcal/mol for tunnel ice with elongated bubbles, and 13.5 kcal/mol for super-imposed ice.
    Type of Medium: Series available for loan
    Pages: v, 29, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 46
    Language: English
    Note: CONTENTS Preface Summary Introduction Principle of measuring the visco-elastic nature of snow and ice by the vibration method Experimental method for determination of visco-elastic properties of snow and ice Visco-elastic properties of tunnel ice Elastic properties of snow samples from the deep pit Elastic properties of core samples obtained by drilling Elastic properties of snow near the ice-cap surface Vertical variation of Young's modulus near the surface Wind-packed snow Peter snow Relation between Young's modulus and density of snow Relation between Young's modulus and density over the range from surface snow to ice Supplementary experiments on the elastic nature of snow and ice at Site 2 Anisotropy of Peter snow Age hardening Temperature dependence of Young's modulus of core ice Viscosity measurement of snow and ice in Greenland Further experiments on the elastic nature of tunnel ice Temperature dependence of Young's modulus Frequency dependence of Young's modulus Further experiments on the viscous nature of tunnel ice Temperature dependence of loss factor Activation energy Frequency dependence of loss factor and viscosity Relation between viscosity and density Conclusions References Appendix: Experimental data
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  • 73
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-51
    In: Research report / Cold Regions Research and Engineering Laboratory, 51
    Description / Table of Contents: Summary: The study was made in order to simulate the deformation of a tunnel in glacier ice and compare the results with the theoretical value derived from compression or tension tests. The plastic deformation of commercial polycrystalline ice and manufactured snow-ice was determined by measuring the discharge of oil from the cavity of closed hollow ice cylinders subjected to high external pressure in an oil-filled pressure chamber. The deformation vs time curves were similar to those obtained in compression or tension tests. The relationships between minimum strain rate and applied pressure, or between minimum strain rate and the circumferential stress at the surface of the inner cavity, were found to differ from the power law ϵ ̇= ασⁿ, the value of n being an increasing function of stress. Analysis of time deformation curves indicates that viscoelastic models proposed by former investigators do not apply to the mechanism of the plastic deformation of ice.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 51
    Language: English
    Note: CONTENTS Preface Summary Introduction Apparatus Specimens Experimental procedures and results Analysis of the data Discussion References
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  • 74
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 75
    Monograph available for loan
    Monograph available for loan
    London : Wykeham Publications
    Associated volumes
    Call number: AWI A5-16-89783
    In: The Wykeham science Series ; 3, 3
    Type of Medium: Monograph available for loan
    Pages: xv, 240 S. , Ill., graph. Darst. , 22 cm
    Edition: Repr.
    ISBN: 0851090400
    Series Statement: The Wykeham science series 3
    Language: English
    Note: Contents: Preface. - Symbols, units and numerical values. - 1. The nature and scope of meteorology. - 1.1. Meteorology in relation to other sciences. - 1.2. Variations in space and time. - 1.3. Applied meteorology. - 2. Physical properties of the atmosphere. - 2.1. Composition of dry air. - 2.1.1. Mean molecular weight. - 2.1.2. Dissociation and ionization. - 2.1.3. Escape to space of component molecules. - 2.2. Pressure, density and temperature. - 2.2.1. Definition of pressure. - 2.2.2. Values near sea level. - 2.2.3. Variations in the vertical. - 2.2.4. Diurnal fluctuations at upper levels. - 2.2.5. Horizontal pressure gradients. - 2.3. Water vapour. - 2.3.1. Humidity mixing ratio. - 2.3.2. Density of moist air. - 2.3.3. Saturation vapour pressure. - 2.3.4. Paths leading to saturation. - 2.3.5. Measurement of vapour pressure. - 2.3.6. Distribution of water vapour. - 3. Heat transfer. - 3.1. Radiation processes. - 3.1.1. Solar radiation: its energy distribution. - 3.1.2. The solar constant. - 3.1.3. Effect of the atmosphere and earth on solar radiation. - 3.1.4. Radiation from the earth and atmosphere. - 3.2. Convection. - 3.2.1. Adiabatic temperature changes. - 3.2.2. Adiabatic equation. - 3.2.3. Potential temperature: dry adiabatic lapse rate. - 3.2.4 Saturated adiabatic lapse rate. - 3.2.5. Stability and instability. - 3.3. Heat transfer in land and sea. - 3.3.1. Heating and cooling of soil. - 3.3.2. Heating and cooling of water. - 4. Condensation and precipitation. - 4.1. Microphysical processes. - 4.1.1 Condensation nuclei. - 4.1.2. Curvature and solute effects. - 4.1.3. Water-droplet clouds. - 4.1.4. Ice nuclei. - 4.1.5. Ice-crystal clouds. - 4.1.6. Precipitation from water clouds. - 4.1.7. Precipitation from mixed clouds. - 4.1.8. Thunderstorm electricity. - 4.2. Larger-scale processes. - 4.2.1. Surface cooling. - 4.2.2. Evaporation. - 4.2.3. Vertical motion. - 4.3. Cloud observations. - 4.3.1. Cloud genera: their heights and composition. - 4.3.2. Cloud recognition and general features. - 4.3.3. Effects of vertical wind shear. - 4.3.4. Cloud classification for forecasting. - 5. The tephigram. - 5.1. Construction of the diagram. - 5.1.1. Coordinates: area and energy. - 5.1.2. Isobars. - 5.1.3. Saturation mixing ratio lines. - 5.1.4. Saturated adiabatics. - 5.1.5. Height variation. - 5.2. Simple graphical computations. - 5.2.1. Height. - 5.2.2. Humidity elements. - 5.2.3. Condensation levels. - 5.2.4. Föhn effects. - 5.3. Precipitable water and precipitation rate. - 5.3.1. Formula and calculation. - 5.3.2. Precipitation rate. - 5.3.3. Water content of convection clouds. - 5.4. The effects of vertical motion on lapse rate. - 5.4.1. Unsaturated or saturated motion. - 5.4.2. Potential (convective) instability. - 5.5. Tephigram analysis. - 5.5.1. Latent instability. - 5.5.2. Air mass characteristics. - 6. Winds. - 6.1. Laws of motion and the earth's rotation. - 6.1.1. Newton's First and Second Laws. - 6.1.2. Nature of the earth's rotation. - 6.1.3. Effects of the earth's rotation: the Coriolis force. - 6.2. Inertial flow and geostrophic winds. - 6.2.1. Nature of inertial flow. - 6.2.2. Nature of geostrophic flow. - 6.2.3. Geostrophic wind equation. - 6.2.4. Wind and pressure near the equator. - 6.3. Gradient winds. - 6.4. Winds in the friction layer. - 6.5. Thermal winds. - 6.5.1. Vertical shear vector. - 6.5.2. Temperature control of the shear vector. - 6.5.3. Thermal wind equation and thickness charts. - 6.5.4. Hodographs and temperature advection. - 6.5.5. Jet streams. - 7. Instruments and observations. - 7.1. Routine surface observations. - 7.1.1. Pressure. - 7.1.2. Temperature and humidity. - 7.1.3. Precipitation and evaporation. - 7.1.4. Wind. - 7.1.5. Clouds and visibility. - 7.1.6. Sunshine and radiation. - 7.1.7. Ship observations. - 7.2. Upper air observations. - 7.2.1. Historical. - 7.2.2. The radiosonde: radar winds. - 7.2.3. Ozone measurements. - 7.3. World Weather Watch. - 7.4. Experiments in observation and interpretation. - 7.4.1. Pressure. - 7.4.2. Temperature and humidity. - 7.4.3. Evaporation and rainfall. - 7.4.4. Wind. - 7.4.5. Radiation. - 7.4.6. Topographical influences. - 8. Synoptic Meteorology. - 8.1. The surface weather map: an introduction. - 8.1.1. The plotting code. - 8.1.2. Pressure systems and features. - 8.1.3. Air masses. - 8.1.4. Fronts. - 8.2. Air mass characteristics. - 8.2.1. Classification. - 8.2.2. Modifications. - 8.2.3. Air masses over the British Isles. - 8.3. Frontal characteristics. - 8.3.1. The stability of a frontal surface. - 8.3.2. Equilibrium slope of a frontal surface. - 8.3.3. Frontal structure. - 8.4. Frontal depressions. - 8.4.1. The life cycle of a frontal depression. - 8.4.2. Cold front waves; depression families. - 8.4.3. Warm front waves. - 8.4.4. Secondaries at points of occlusion. - 8.5. Non-frontal depressions. - 8.5.1. Heat lows. - 8.5.2. Polar lows. - 8.5.3. Orographic lows. - 8.5.4. Tropical cyclones. - 8.5.5. Tornadoes. - 8.6. Anticyclones. - 8.6.1. General characteristics. - 8.6.2. Cold and warm anticyclones. - 8.7 Synoptic development. - 8.7.1. Convergence, divergence and vertical motion. - 8.7.2. Convergence and vorticity. - 8.7.3 Long waves. - 8.7.4. Circulation indices: blocking. - 8.8. Surface analysis. - 8.8.1. General. - 8.8.2. Representativeness of observations. - 8.8.3. METMAPS. - 9. Micrometeorology. - 9.1. The nature of airflow near the ground. - 9.1.1. Wind speeds over a uniform level surface. - 9.1.2. Flow within a fluid boundary layer. - 9.1.3. Shearing stress via the mixing length concept. - 9.1.4. The friction velocity u*. - 9.1.5. Interpretation of the mixing length concept. - 9.1.6. The wind profile equation in complete form. - 9.2. The influence of surface roughness on the wind. - 9.2.1. Roughness in the aerodynamic sense. - 9.2.2. Roughness in relation to shearing stress and mean wind speed. - 9.2.3. The drag coefficient CD. - 9.2.4. CD as a transfer coefficient. - 9.2.5. Effect of a change in surface roughness. - 9.3. Vertical transport by turbulence. - 9.3.1. Flux equations; use of electrical analogy. - 9.3.2. Heat flux and other calculations. - 9.3.3. Vertical temperature gradients in relation to turbulent exchange. - 10. The general circulation. - 10.1. General characteristics. - 10.1.1. Genesis and interactions. - 10.1.2. Time fluctuations. - 10.2. Observations. - 10.2.1. Time- and space-averaging. - 10.2.2. Tracers. - 10.3. Experiment and theory. - 10.3.1. The rotating vessel experiment. - 10.3.2. Conservation principles. - 10.3.3. Cellular models. - 10.4. Climatic zones. - 11. Weather forecasting. - 11.1. Historical survey. - 11.1.1. 1860-1920. - 11.1.2. 1920-1945. - 11.1.3. 1945-1960. - 11.1.4. 1960 onwards. - 11.2. Conventional forecasting. - 11.2.1. Pressure tendency. - 11.2.2. Making the forecast. - 11.3. Long-range forecasting. - 11.3.1. Statistical methods. - 11.3.2. Synoptic methods. - 11.3.3. Analogues. - 11.4. Numerical forecasting. - 11.4.1. The barotropic model. - 11.4.2. Later developments. - 11.5. Predictability and control. - 11.5.1. Short-range predictability. - 11.5.2. Medium-range predictability. - 11.5.3. Long-range predictability: climatic trends. - 11.5.4. Weather and climate modification. - Answers to Problems. - Subject Index. - The Wykeham Series.
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  • 76
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-19
    In: Research report / Cold Regions Research and Engineering Laboratory, 19
    Description / Table of Contents: Abstract: Measurements were made of global and net radiation between 6 July and 7 August 1955 at a site on the Greenland Ice Cap located near 78°N latitude and at an elevation of 6800 ft. Snow-surface temperatures during this period were below 0°C and mean cloudiness was 0.7. Total incident global radiation measured during the 33-day period amounted to 20,628 ?? of which only 3059 ??, or about 15%, were absorbed by the snow cover. Most of the absorbed global radiation was re-emitted as long-wave radiation, so the net gain during the observation period amounted to not more than 7.6 ??/day. Diffuse sky radiation amounted to only 19% of all incoming global radiation measured at the ice-cap research site. In the temperate zone, diffuse sky radiation amounts to 30% or more of the incoming radiation. The small amount of diffuse sky radiation indicates low atmospheric turbidity in this polar climatic zone. Incident global radiation was reduced by 6% in the presence of a 0.5 cloud cover. Under full overcast conditions the snow surface received 65% of the global radiation measured on clear days. In the temperate zone as little as 30% of global radiation reaches the earth under full cloud cover. The large amount of global radiation received in the Arctic under full cloud cover is the primary cause of one form of arctic white-out. Accompanying the small decrease in global radiation caused by cloudiness is a large decrease in effective outgoing long-wave radiation, with an increase in the net radiation balance. This condition contributes to a greater potential ablation of the snow and ice cover during cloudy seasons. The long-wave radiation balance at this site on the ice cap was always negative during the period covered by this study. Errors associated with the measurement of solar radiation at the low sun angles which prevailed at the research site were found to be about -3%. No correction was applied to the basic data, however, since there were insufficient data to establish the consistency of this error over the period of observation. During periods of blowing and drifting snow, 6% more global radiation was measured at 1.25 m above the snow surface than at 5.7 m elevation. The increase may be due to multiple reflection within the layer of blowing snow. The atmospheric transmission coefficient at the ice-cap site was found to be 0.968. This high value was associated with the low atmospheric turbidity. The heat balance of the snow cover as computed from the radiation measurements and a temperature profile in the snow was found to be 7.6 ??/day at the ice-cap site. This is a negligible heat gain when compared with the 400 ??/day gain by a spring snow pack in the Sierra Nevada of California. For the entire season when the sun is above the horizon, the estimated net gain by the ice cap is 1000 ??, no more than a 2-1/2-day heat supply used in melting the snow of the High Sierra. Some measurements made with a silicon solar battery similar to those developed by the Bell Telephone Laboratories indicate that it may have a significantly higher efficiency on the ice cap than in the more temperate zone. Verification of this apparent increase in efficiency and the causes for it require further study of the performance of the p-n junction cells in the Arctic.
    Type of Medium: Series available for loan
    Pages: iv, 20, [2] Seiten , Illustrationen , 27 cm
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 19
    Language: English
    Note: CONTENTS I. Introduction II. Instrumentation Recording of data III. Results Global radiation Albedo of snow Diffuse sky radiation Effect of clouds on radiation Atmospheric and terrestrial radiation Effect of low sun angle on measured radiation Global radiation gradient Atmospheric transmission coefficient Heat balance of snow cover Applied use of solar energy References. Appendix
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  • 77
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-203-116
    In: Special report / Cold Regions Research and Engineering Laboratory, Corps of Engineers, US Army, 116
    Description / Table of Contents: Abstract: Pendulum steering, a new concept of attitude stabilization for thermal probes or coring drills in ice, eliminates instability. The center of support is placed above the center of gravity. A lower and upper hot point produce melt penetration. The ratio of their power levels is the basis for stabilization, which is provided by the automatic control of the heater in the upper hot point. This feature makes possible a single thermal probe design that is suitable for all ice cap temperatures and a wide range of penetration rates (i.e., applied power levels). The simplicity of a thermal probe with pendulum steering suggests availability at modest cost and versatility as a widely applicable tool.
    Type of Medium: Series available for loan
    Pages: iv, 4 Seiten , Illustrationen
    Series Statement: Special report / Cold Regions Research and Engineering Laboratory, Corps of Engineers, US Army 116
    Language: English
    Note: CONTENTS Preface Summary Introduction The principle of pendulum steering Analysis of the power requirements The upper heater control Laboratory tests Summary
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  • 78
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-120
    In: Research report / Cold Regions Research and Engineering Laboratory, 120
    Description / Table of Contents: Abstract: The report is divided into four parts: Parts I and II cover investigations of the reliability of shear stress measurements in soils subjected to vibratory loads for biaxial and triaxial systems, respectively. Part I is a summary only (see USA CRREL Technical Report 90 for detailed treatment). Part III is a study of three-dimensional "principal" stress patterns produced in soil subjected to vibratory loads. Part IV is a theoretical analysis of some aspects of soil wave propagation in stratified soil. From the measurements of five shear stresses and one normal stress, the stress distribution of a triaxial system can be determined. In noncohesive soils triaxial stress fields due to vibratory loads can be determined by recording six independent stress components. Sinusoidal force excitation and impact excitation yield time-distance graphs which can be used to determine reflection and refraction techniques in stratified soils.
    Type of Medium: Series available for loan
    Pages: v, 52 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 120
    Language: English
    Note: CONTENTS Preface Summary Part I. Two-dimensional shear stress measurements Part II. Three-dimensional shear stress measurements Introduction Measurements Experimental results Evaluation Compatibility checks Comparison between shear stresses under static and dynamic loads Conclusions Part III. Three-dimensional normal stress measurements Introduction Experimental setup Results Analysis Conclusions Part IV. Soil wave propagation in stratified soil Introduttion Distance-time graphs Results Sinusoidal force excitation Refraction Impact force excitation Selected bibliography Appendix A. Equations for computing stress components in Part II Appendix B. Equations for computer program in Part III
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  • 79
    Call number: MOP 40071 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VII, 50 Seiten , Illustrationen, Karten
    Series Statement: Hydrology papers 15
    Language: English
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  • 80
    Call number: AWI G4-22-94988
    Type of Medium: Monograph available for loan
    Pages: 130 Seiten , Illustrationen , Errata , 28 cm
    Series Statement: Annual progress report / Sanitary Engineering Research Laboratory, University of California 1
    Language: English
    Note: TABLE OF CONTENTS I INTRODUCTION II SUMMARY OF METHODS OF GROUND WATER DETECTION A. Geophysical Methods Gravimetric Method Magnetic Method Seismic Method Electrical Resistivity Method Electrical, Radioactive and Temperature Logging Methods B. Tracer Methods Dyes as Ground Water Tracers Tracers Detected by Chemical Determinations Radioactive Tracers III LABORATORY AND FIELD STUDIES OF GROUND WATER TRACERS Ion Exchange in Soils Lysimeter Studies of Fluorescein, Chloride and Iodine-131 Comparison of Stable and Radioactive Calcium Tritium Studies Injection Well Studies of Fluorescein, Dextrose, and Iodine-131 IV CONCLUSIONS AND RECOMMENDATIONS A. Geophysical Methods B. Tracer Methods V ABSTRACT OF LITERATURE PERTAINING TO GROUND WATER DETECTION A. Geophysical Methods B . Tracer Methods
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  • 81
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    Series available for loan
    Berlin : VEB Deutscher Verlag der Wissenschaften
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    Call number: 7120
    In: Mathematische Forschungsberichte, 23
    Type of Medium: Series available for loan
    Pages: 98 Seiten , Illustrationen
    Series Statement: Mathematische Forschungsberichte 23
    Language: English
    Note: TABLE OF CONTENTS Abstract Introduction Chapter I. The algebras H and L 1. Notation. General conventions 2. Fundamental notions and definitions 3. Geometrical interpretation 4. Summary Chapter II. Monogenic functions 1. Functions which have hypercomplex values 2. Monogenic functions 3. Representatives of monogenic functions in the Banach algebra Lγ 4. Analyticity of monogenic functions Chapter III. Some elementary monogenic functions I. Introduction 2. The inverse function ζ-1 3. The exponential function 4. The components of a power series with real coefficients 5. Trigonometric and hyperbolic functions 6. The logarithmic function 7. The inverse function ζ*-1 8. The singular manifold of (ζ-α*)-1 Chapter IV. Hypercomplex integrals and theorems of Cauchy's type 1. Introduction. Integrals of hypercomplex-valued functions 2. Integrals of monogenic functions over closed curves and surfaces 3. Cauchy's second theorem for monogenic functions of ζ 4. An application of Cauchy's second theorem Chapter V. On some results of Marcel N. Roşuleţ 1. Introduction 2. An algebra associated with Laplace's equation 3. Summary of analysis 4. On the relation between the algebras U and L Appendix. The product of two algebra elements Bibliography
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  • 82
    Call number: O 2075/1964 II
    Type of Medium: Journal available for loan
    ISSN: 0367-6684 , 0568-5249 , 0568-5249
    Former Title: Vorg. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Serija geografičeskaja i geofizičeskaja
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika zemli
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika atmosfery i okeana
    Language: Russian , English
    Note: Teils mit Jg.-Zählung , In kyrill. Schr
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  • 83
    Monograph available for loan
    Monograph available for loan
    Washington : Department of Meteorology and Climatology, Univ.
    Call number: MOP 25529
    Type of Medium: Monograph available for loan
    Pages: VII, 57 S. , graph. Darst., Kt.
    Series Statement: AF contract 19(604) 3063
    Language: English
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  • 84
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    Washington : Department of Meteorology and Climatology, Univ.
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    Call number: MOP 25772
    In: Occasional report / University of Washington, Department of Meteorology and Climatology, No. 8
    Type of Medium: Series available for loan
    Pages: VI, 119 S. , graph. Darst., Kt
    Series Statement: Occasional report / University of Washington, Department of Meteorology and Climatology 8
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  • 85
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    Washington : Dept.of Meteorology and Climatology, Univ.
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    Call number: MOP 25349
    In: Scientific report / Department of Meteorology and Climatology, University of Washington, No. 8
    Type of Medium: Series available for loan
    Pages: VIII, 50 S. , graph. Darst.
    Series Statement: Scientific report / Department of Meteorology and Climatology, University of Washington 8
    Language: English
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  • 86
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    Series available for loan
    Washington : Dept. of Meteorology and Climatology, Univ.
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    Call number: MOP 25773
    In: Occasional report / University of Washington, Department of Meteorology and Climatology, No. 9
    Type of Medium: Series available for loan
    Pages: 64 S. , graph. Darst., Kt
    Series Statement: Occasional report / University of Washington, Department of Meteorology and Climatology 9
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  • 87
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    Series available for loan
    Washington : Department of Meteorology and Climatology, Univ.
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    Call number: MOP 25778
    In: Scientific report / Department of Meteorology and Climatology, University of Washington, No. 5
    Type of Medium: Series available for loan
    Pages: VII, 48 S. , graph. Darst.
    Series Statement: Scientific report / Department of Meteorology and Climatology, University of Washington 5
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  • 88
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    Series available for loan
    Washington : Deptament of Meteorology and Climatology, Univ.
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    Call number: MOP 25768
    In: Scientific report / University of Washington, Department of Meteorology and Climatology, No. 1
    In: Occasional report / University of Washington, Department of Meteorology and Climatology, No. 4
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    Pages: 21 S. , graph. Darst.
    Series Statement: Occasional report / University of Washington, Department of Meteorology and Climatology 4
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  • 89
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    Djakarta : Repr. Djatop.
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    Call number: MOP 21605
    In: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik, No. 48
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    Pages: 14 S. , graph. Darst
    Series Statement: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik 48
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  • 90
    Call number: MOP 28487
    In: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik, Nr. 51
    Type of Medium: Monograph available for loan
    Pages: 4 S.
    Series Statement: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik 51
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  • 91
    Call number: MOP 28488
    In: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik, Nr. 53
    Type of Medium: Monograph available for loan
    Pages: 16 S. , graph. Darst.
    Series Statement: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik 53
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 92
    Monograph available for loan
    Monograph available for loan
    Fort Collins : Dept. of Atmospheric Science, Colorado State University
    Call number: MOP 35141
    Type of Medium: Monograph available for loan
    Pages: 54 S. , Ill.
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 93
    Call number: MOP 35293
    Type of Medium: Monograph available for loan
    Pages: 80 S. , graph. Darst.
    Series Statement: Atmospheric science paper 107
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 94
    Monograph available for loan
    Monograph available for loan
    Haifa : Dep. of Education and Culture
    Call number: PIK N 630-15-89532
    Type of Medium: Monograph available for loan
    Pages: 24 Bl. , zahlr. Ill.
    Language: English , French
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 95
    Call number: PIK N 630-15-89556
    Type of Medium: Monograph available for loan
    Pages: 62 S. , zahlr. Ill.
    Edition: 1. print.
    Language: English
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 96
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : U.S. Dept. of Commerce
    Call number: PIK N 456-16-90161/1 ; PIK N 456-16-90161/2
    Type of Medium: Monograph available for loan
    Pages: 621 S. : graph. Darst., Kt. , gebundene Kopie in 2 Bänden
    Edition: 2nd print.
    Uniform Title: Chung-kuo chi-hou 〈engl.〉
    Language: English
    Location: A 18 - must be ordered
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Branch Library: PIK Library
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  • 97
    Monograph available for loan
    Monograph available for loan
    Wien : Österreichische Geographische Gesellschaft
    Associated volumes
    Call number: M 15.89034
    In: Mitteilungen der Österreichischen Geographischen Gesellschaft
    Type of Medium: Monograph available for loan
    Pages: 481 S. , Kt.
    Series Statement: Mitteilungen der Österreichischen Geographischen Gesellschaft 101, 1
    Language: English
    Note: AUFSÄTZE --- BOBEK HANS: Der Eisrückgang im östlichen Klagenfurter Becken, S. 3 --- BOBEK HANS: Forschungen in Persien 1958/59, S. 381 --- BODZENTA ERICH: Innsbruck. Eine sozial-ökologische Studie, S. 823 --- LECHLEITNER HERWIG: Stadtentwicklung und Stadtplanung in Leoben, S. 202 --- LEITNER WILHELM: Die Verteilung der Bevölkerung nach natürlichen Landschaften in der Steiermark, S. 72 --- LICHTENBERGER ELISABETH: Der Rückzug des Würmgletschers im mittleren Klagenfurter Becken und Krappfeld, S. 63 --- PASCHINGER HERBERT: Studienreise nach Südspanien im März 1959, S. 388 --- RUNGALDIER RANDOLF: Südtirols Sonderstellung im Alpenraum, S. 291 --- SPREITZER HANS: Fußflächen im Kilikischen Ala Dag im Taurus, S. 183 --- SPREITZER HANS: Albrecht Pencks Wirken in Wien, S. 375 --- SUTER KARL: Die Palmgärten des Mzab, S. 63 --- WICHE KONRAD: Geomorphologische Studien in Südostspanien (Provinz Murcia), S. 389 --- WINKLER ERHART: Die Tabakwirtschaft von Samsun, S. 361 --- WISSMANN HERMANN VON: Die rezente und quartäre Vergletscherung des Yülungschan, S. 165 --- BERICHTE UND KLEINE MITTEILUNGEN --- BERNLEITHNER E.: Raumordnungsplan Marchfeld, S. 243 --- HOLZMANN G.: Die japanischen Siedler in Brasilien, S. 401 --- LAUTENSACH H.: Eine Landeskunde der Kanaren, S. 898 --- LENDL E.: Ein unbekannter Humboldtbrief, S. 241 --- MORAWETZ S.: Die Muren des Unwetters vom 12. August 1958 im Murtal zwischen Übelstein und Mixnitz (Steiermark), S. 86 --- MORAWETZ S.: Geomorphologische Bemerkungen zur Unwetterkatastrophe vom August 1958 im Rennfeldgebiet (Steiermark), S. 396 --- SLEZAK F.: Neue geographische Monographie in Südosteuropa, S. 96 --- ZEITLINGER J.: Beobachtungen über unterirdische Erosion in Verwitterungslehm, S. 94 --- SCHULGEOGRAPHIE --- BANNERT B.: Bildauswertung im Geographieunterricht, S. 248 --- BREU J. : Probleme der Schreibung südosteuropäischer Ortsnamen in österreichischen Mittelschulatlanten, S. 97 --- CONSTANTINI O.: Die Elektrizitätsgewinnung im Bereiche der Wolga, S. 123 --- LANGBEIN O.: Zur Ortsnamen-Schreibung, S. 403 --- LANGBEIN O.: Sowjetische Volkszählung 1959, S. 406 --- PRILLINGER F.: Das Geographielehrbuch, sein Inhalt und seine Verwendung, S. 131 --- TRIMMEL H.: Die wirtschaftliche Entwicklung Spaniens im letzten Jahrzehnt, S. 117 --- GEOGRAPHISCHE INFORMATIONEN --- GRÜLL J.: Die Eisenerze am Orinoco, ein Faktor im wirtschaftlichen Strukturwandel Argentiniens, S. 135 --- GRÜLL J.: Afrika auf dem Wege zu politischer Neuordnung, S. 413 --- RIECK W.: Entwicklung und Ausbau des neuen chinesischen Eisenbahnnetzes, S. 266 --- Kurznachrichten, S. 140, 274, 430 --- BUCHBESPRECHUNGEN, S. 153, 282, 430 --- GESELLSCHAFTSNACHRICHTEN, S. 289, 466
    Location: Reading room
    Branch Library: GFZ Library
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  • 98
    Call number: MOP 24644
    Type of Medium: Monograph available for loan
    Pages: XV, 631 S , Ill., graph. Darst
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 99
    Monograph available for loan
    Monograph available for loan
    JERUSALEM : ISRAEL PROGRAM FOR SCIENTIFIC TRANSLATIONS
    Call number: MOP 36587
    Type of Medium: Monograph available for loan
    Pages: IX, 384 S. : Ill.
    Uniform Title: Aerologija
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 100
    Monograph available for loan
    Monograph available for loan
    New York : Dover Publications
    Call number: M 15.89026
    Type of Medium: Monograph available for loan
    Pages: xvi, 504 S. , graph. Darst.
    Edition: Repr. of 2. ed. rev. and enl., 1894.
    ISBN: 0-486-60293-1
    Series Statement: Dover classics of science and mathematics
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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