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  • English  (1,127)
  • 1955-1959  (670)
  • 1950-1954  (438)
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  • 1
    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
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  • 2
    Series available for loan
    Series available for loan
    Frankfurt a.M. : Kramer
    Call number: MOP 15176
    Type of Medium: Series available for loan
    Pages: 354 S. : zahlr. Ill.
    Series Statement: Senckenberg-Buch / Senckenbergische Naturforschende Gesellschaft 23
    Language: English
    Location: MOP - must be ordered
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  • 3
    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
    Location: MOP - must be ordered
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  • 4
    Series available for loan
    Series available for loan
    Washington : Department of Meteorology and Climatology, Univ.
    Associated volumes
    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
    Language: English
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  • 5
    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
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  • 6
    Monograph available for loan
    Monograph available for loan
    Toronto
    Call number: PIK N 456-17-90911
    Type of Medium: Monograph available for loan
    Pages: 90 S. , graph. Darst., Kt. , 28 cm
    Language: English
    Location: A 18 - must be ordered
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  • 7
    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
    Location: MOP - must be ordered
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  • 8
    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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  • 9
    facet.materialart.13
    facet.materialart.13
    [Philadelphia] : American Meteor Society
    Call number: MOP S 7075
    In: Meteoritics
    Type of Medium: 13
    Pages: Seite 247-279 , Tabellen
    Edition: Sonderdruck reprinted from Meteoritics Vol. 1, No. 2, 1954
    Series Statement: Meteoritics Vol. 1, No. 2
    Language: English
    Location: MOP - must be ordered
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  • 10
    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-202-18
    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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  • 11
    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-202-17
    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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  • 12
    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-202-20
    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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  • 13
    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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  • 14
    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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  • 15
    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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  • 16
    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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  • 17
    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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  • 18
    Call number: AWI PY-1899-13,1
    In: British Polar Year Expedition, Vol. 1
    Type of Medium: Monograph non-lending collection
    Pages: XIII, 336 S. , Ill.
    Language: English
    Note: Table of Contents: GENERAL INTRODUCTION. - Figures. - North Arm of Great Slave Lake, showing positions of present and former Fort Rae sites. - Site plan of station. - METEOROLOGY. - Introduction. - PART 1. - TEMPERATURE. - 1. Instruments, exposures, and methods. - 2. Annual variation of temperature. - 3. Diurnal variation of temperature. - 4. The effect of cloud and wind upon temperature. - 5. Temperature and wind direction. - 6. Non-periodic temperature changes. - PART 2. - PRESSURE. - 1. Instruments and methods. - 2. Annual variation of pressure. - 3. Diurnal variation of pressure. - 4. Non-periodic pressure changes. - 5. Pressure waves. - 6. Pressure surges. - PART 3. - SURFACE WIND. - 1. Instruments, exposures, and methods. - 2. Annual variation of wind velocity. - 3. Diurnal variation of wind velocity. - 4. Frequency of winds of different velocities. - 5. Frequency of winds of different directions and of calms. - 6. SE. and NW. wind at Fort Rae. - 7. Velocity of winds from different directions. - 8. Distribution of wind velocities from different directions. - 9. Highest instantaneous wind speeds and extreme hourly winds. - 10. The effect of the NW. and SE. wind upon the meteorological elements. - 11. The resultant winds. - 12. Diurnal inequalitites of N. and E. components of resultant winds. - PART 4. - UPPER WINDS. - 1. General remarks. - 2. Monthly and seasonal mean wind velocities at different heights. - 3. Frequency of wind from various directions in the upper atmosphere. - 4. Distribution oof wind at different levels irrespective of direction. - 5. Mean wind velocities from different directions at different levels. - 6. Resultant winds in the upper atmosphere. - 7. The direction of the wind in the upper atmosphere when the wind at the surface is from stated directions. - PART 5. - UPPER AIR TEMPERATURE AND PRESSURE. - PART 6. - CLOUDS. - 1. General. - 2. Percentage frequency of different could forms. - 3. Cloud amount: percentage frequency of each cloud amount. - 4. Annual variation of cloud. - 5. Diurnal variation of cloud. - PART 7. - PRECIPITATION. - 1. Instruments and methods. - 2. Annual variation of precipitation. - 3. Snow crystals. - PART 8. - RELATIVE HUMIDITY OF THE AIR. - 1. General. - 2. Mean monthly values of humidity during the winter months. - 3. Annual variation of the relative humidity. - 4. Diurnal variation of the relative humidity. - PART 9. - SUNSHINE AND RADIATION. - PART 10. - HALO PHENOMENA. - PART 11. - VISIBILITY. - PART 12. - THE METEOGRAPH DIAGRAMS. - TERRESTRIAL MAGNETISM AND AURORA. - 1. Magnetograph chamber. - 2. Temperature insulation of the magnetograph hut. - 3. Temperature variation within the recording chamber. - 4. Recording instruments. - 5. ILLUMINATION. - 6. TIMING. - 7. CONTROL HUT AND CONTROL INSTRUMENTS USED. - 8. CONTROL OBSERVATIONS OF H. - 9. CONTROL OBSERVATIONS OF D. - 10. AZIMUTH MARK. - 11. CONTROL OBSERVATIONS OF INCLINATION. - 12. PROCEDURE IN CONTROL OBSERVATIONS. - 13. SUMMARISED RESULTS OF CONTROL OBSERVATIONS. - 14. SCALE VALUES OF DECLINATION MAGNETOGRAPHS. - 15. SCALE VALUES OF H AND Z MAGNETOGRAPHS. - 16. EFFECT ON SCALE VALUES OF GREAT SEASONAL RANGE OF HUMIDITY WITHIN THE RECORDING CHAMBER. - 17. TEMPERATURE COEFFICIENTS OF H AND Z VARIOMETERS. - 18. METHODS OF DETERMINING TEMPERATURE COEFFICIENTS OF VARIOMETERS. - 19. ASSIGNMENT OF H BASE LINE VALUES DURING PERIODS OF LARGE TEMPERATURE COEFFICIENT OF VARIOMETER. - 20. ASSIGNMENT OF H BASE LINE VALUES IN GENERAL. - 21. Z BASE LINE VALUES DURING PERIOD OF LARGE TEMPERATURE COEFFICIENT OF VARIOMETER. - 22. Z BASE LINE VALUES IN GENERAL. - 23. USE OF AUXILIARY H AND Z MAGNETOGRAPHS. - 24. D BASE LINE VALUES. - 25. MONTHLY MEAN VALUES: THE ANNUAL VARIATION AND SECULAR CHANGE. - 26. MONTHLY AND SEASONAL VALUES OF N, E, T, I, AND A. - 27. COMPARISON OBSERVATIONS AT 1882-83 (OLD FORT) STATION. - 28. DETERMINATION OF H AT OLD FORT RAE. - 29. DETERMINATION OF D AT OLD FORT RAE. - 30. DETERMINATION OF I AT OLD FORT RAE. - 31. SECULAR CHANGE AT OLD FORT RAE. - 32. LONGITUDE OF OLD FORT RAE SITE. - 33. AZIMUTH OF FIXED MARK AT OLD FORT RAE. - 34. RELATIONSRIPS BETWEEN ALL, QUIET, AND DISTURBED DAY VALUES AT THE MAIN STATION. - 35. NON-CYCLIC CHANGE. - 36. NON-CYCLIC CHANGE ON QUIET DAYS. - 37. EXAMINATION OF THE NEGATIVE NON-CYCLIC CHANGE ON q DAYS. - 38. NON-CYCLIC CHANGE ON DISTURBED DAYS. - 39. OVERLAPPING DAY MEANS. - 40. CHARACTERISTICS OF CURRENT SYSTEM NECESSARY TO PRODUCE H AND Z DEPARTURES FROM MEAN VALUES. - 41. POSITION OF CURRENT SYSTEM AND DIRECTION OF FLOW DEDUCED FROM MEAN H AND Z DEPARTURES AT OTHER STATIONS ON d DAYS. - 42. CONCLUSIONS REGARDING CURRENT CHARACTERISTICS ON DISTURBED DAYS. - 43. CURRENT SYSTEM ON q DAYS. - 44. CONSIDERATIONS UNDERLYING APPLICATION OF NON-CYCLIC CHANGE AND USE OF GREENWICH DAYS IN FORMATION OF DIURNAL INEQUALITIES. - 45. SOME FEATURES OF THE DIURNAL VARIATIONS. - 46. DIURNAL INEQUALITIES FOR SELECTED q AND d DAYS. - 47. MEAN ANNUAL VECTOR DIAGRAMS. - 48. SEASONAL VECTOR. DIAGRAMS. - 49. VECTOR DIAGRAMS ON d' AND q' DAYS. - 50. THE TOTAL FIELD VECTOR T AND ITS POSITIONAL CO-ORDINATES. - 51. SEASONAL MEAN VALUES OF T AND p IN DISTURBANCE. - 52. DIURNAL VARIATION OF T AND p IN DISTURBANCE. - 53. SOME DIURNALLY VARYING CHARACTERISTICS OF THE CURRENT SYSTEM PRODUCING DISTURBANCE. - 54. CHANGE IN POSITION OF DISTURBING CURRENT WITH SEASON. - 55 EFFECT OF INCREASED SCALE OF DISTURBANCE ON THE CURRENT SYSTEM. - 56. T AND p ON QUIET DAYS. - 57 RANGE AND AVERAGE DEPARTURES OF DIURNAL INEQUALITIES. - 58. COMPARISON OF INEQUALITY RANGE AND AVERAGE DEPARTURE AT FORT RAE WITH THOSE AT OTHER STATIONS. - 59. COMPARISON WITH 1882-83 INEQUALITY RANGES. - 60. ESTIMATE OF ELEVATION OF DISTURBING CURRENT SYSTEM FROM IR AND AD. - 61. HARMONIC ANALYSIS OF REGULAR DIURNAL VARIATIONS. - (i) 24-hour component. - (ii) 12-hour component. - (iii) 8-hour wave. - (iv) 6-hour wave. - 62. HARMONIC ANALYSIS OF MEAN INEQUALITIES FOR q' AND d' DAYS. - 63. ABSOLUTE DAILY RANGE: R. - 64. COMPARISON WITH 1882-83 RANGES. - 65. COMPARISON WITH R AT OTHER STATIONS. - 66. RELATION OF DISTURBANCE TO MAGNETIC LATITUDE. - 67. FREQUENCY DISTRIBUTION OF R. - 68. DIURNAL DISTRIBUTION OF TIMES OF INCIDENCE OF MAXIMA AND MINIMA. - 69. DIURNAL INCIDENCE OF EXTREME VALUES IN Z. - 70. INCIDENCE OF EXTREME VALUES IN H AND D. - 71. DAILY RANGE PRODUCTS HRH AND ZRz. - 72. HOURLY RANGES AND RANGE PRODUCTS. - 73. FREQUENCY DISTRIBUTION OF HOURLY RANGES IN REPRESENTATIVE MONTHS. - 74. RELATIONSHIPS AMONG THE HOURLY RANGES. - 75. RELATIVE MAGNITUDE OF PERTURBATIONS IN H AND Z. - 76. THE RATIO p = CR/Cr. - 77. SEASONAL DISTRIBUTION OF Cr AND ITS CONSTITUENTS. - 78. RANK ORDER OF DAYS, ON BASIS OF CR AND Cr: COMPARISON WITH INTERNATIONAL SELECTION OF q AND d DAYS. - 79. EFFECT OF USE OF GREENWICH DAY ON SELECTION OF q AND d DAYS. - 80. DIURNAL VARIATION OF IRREGULAR DISTURBANCE (Di). - 81. RELATION OF Di TO TIME DIFFERENTIALS OF FORCE VECTORS. - 82. CHARACTERISTICS OF D1. - 83. Di ON q' AND d' DAYS. - 84. HARMONIC ANALYSIS OF Di. - 85. LOCAL CHARACTER FIGURES. - 86. RANK ORDER OF MONTHS IN DISTURBANCE BY VARIOUS CRITERIA. - 87. INTERDIURNAL VARIABILITY OF H AND z: MONTHLY U ACTIVITY MEASURES. - 88. INTERDIURNAL VARIABILITY ON q' AND d' DAYS. - 89. COMPARISON OF COMPOSITE RANK ORDER OF MONTHS WITH INTERDIURNAL VARIABILITY MEASURES. - 90. DISTINCTIVE FEATURES OF DISTURBANCE. - 91. N DISTURBANCES. - 92. M DISTURBANCES. - 93. OSCILLATORY DISTURBANCE. - 94. RECOVERY MOVEMENTS. - 95. SEASONAL AND DIURNAL DISTRIBUTION OF N AND M MOVEMENTS. - 96. REPETITION OF ISOLATED PERTURBATIONS. - NON-INSTRUMENTAL AURORAL OBSERVATIONS. - 97. THE SCOPE OF THE OBSERVATIONS. - 98. ESTIMATION OF AURORAL INTENSITY. - 99. AURORAL "ACTIVITY" FIGURES. - 100. THE AURORAL LOG. - 101. SEASONAL DISTRIBUTION OF AURORAL FREQUENCY. - 102. AURORAL ACTIVITY OF THE YEAR: GENERAL NOTE. - 103. QUARTER-HOUR AURORAL INTENSITY FIGURES. - 104. MONTHLY DISTRIBUTION OF BRIGHT AURORA. - 105. DIURNAL
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  • 19
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    Djakarta
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    Call number: MOP 17097
    In: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik, No. 44
    Type of Medium: Series available for loan
    Pages: 22 S. , graph. Darst
    Series Statement: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik 44
    Language: English
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  • 20
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    Djakarta : Repr. Djatop.
    Associated volumes
    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
    Language: English
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  • 21
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    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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  • 22
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    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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  • 23
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    Monograph available for loan
    New York [u.a.] : McGraw-Hill
    Call number: PIK N 456-16-90116
    Type of Medium: Monograph available for loan
    Pages: X, 392 S. , Ill., graph. Darst., Kt.
    Language: English
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  • 24
    Call number: PIK N 456-16-90137
    Type of Medium: Monograph available for loan
    Pages: getr. Zählung , ill. (some col.) , 24 cm
    Language: English
    Note: Enth.: Introduction -- Pt. 2. Union of South Africa from Olifants River to Mossel Bay. With an appendix on conditions at Saldanha Bay, Cape Town and Simonstown -- Pt. 3. Union of South Africa from Mossel Bay to East London.With an appendix on conditions oat Mossel Bay and Port Elizabeth -- Pt. 4. Union of South Africa from East London to Kosi Bay.With an appendix on conditions at East London and Durban -- Pt. 5. Portuguese East Africa (Mocambique) and Mocambique Channel -- Pt. 5a. Madagascar. With an appendix on conditions at Mayotte, Diégo Suarez, Nossi Bé and Tamatave
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  • 25
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    Monograph available for loan
    Berlin-Treptow
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    Call number: MOP 16145
    In: Mitteilungen der Archenhold-Sternwarte
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    Series Statement: Mitteilungen der Archenhold-Sternwarte 16
    Language: English
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  • 26
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    Monograph available for loan
    [Cambridge]
    Call number: AWI E1-82-0935
    Type of Medium: Monograph available for loan
    Pages: 12 Seiten , Illustrationen
    Language: English
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  • 27
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    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.
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    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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  • 28
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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-202-52
    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.
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    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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  • 29
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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-202-56
    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.
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    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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  • 30
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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-202-30
    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.
    Type of Medium: Series available for loan
    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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  • 31
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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-202-59
    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.
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    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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  • 32
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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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  • 33
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    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.
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    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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  • 34
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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-202-39
    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.
    Type of Medium: Series available for loan
    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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  • 35
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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-202-41
    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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  • 36
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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-202-42
    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.
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    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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  • 37
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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-202-43
    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.
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    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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  • 38
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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-202-19
    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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  • 39
    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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  • 40
    facet.materialart.00 | 00 |
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    Cambridge : Cambridge Univ. Press
    Call number: M 15.89483
    Type of Medium: 00 | 00 |
    Pages: viii, 381 S.
    Edition: 3rd ed.
    Language: English
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  • 41
    Monograph non-lending collection
    Monograph non-lending collection
    Stockholm : Swedish National Committee for Geodesy and Geophysics
    Call number: AWI PY-1921-13
    Type of Medium: Monograph non-lending collection
    Pages: 77 S. , Ill., Kt., graph. Darst. , 4°
    Language: English
    Note: Table of Contents: GENERAL INTRODUCTION. - Figures. - Map of Spitzbergen. - Site plan of Sveagruvan. - TERRESTRIAL MAGNETISM. - 1. Magnetograph chamber. - 2. Temperature Variations in the magnetograph chamber. - 3. Variometers. - 4. Instruments for absolute measurements. - 5. Absolute observations of the magnetic elements. - 6. Measurements of curves, scale values. Temperature correction. Base values. - 7. Results of curve measurements. Monthly mean values. - 8. Yearly variation and secular change. - 9. Monthly and seasonal mean values of N, E, T, I, and A. - 10. Comparative measurements at the old 1882-83 Polar Year station at Cape Thordsen. - 11. Determination of horizontal force at Cape Thordsen. - 12. Determination of inclination at old station Cape Thordsen. - 13. Determination of declination at Cape Thordsen. - 14. Secular variation at Cape Thordsen. - 15. Relation between all, quiet, and disturbed day values of H, D, and Z at Sveagruvan. - 16. Current system necessary to produce H and Z departures from mean values. - 17. Current system on disturbed days. - 18. Daily variations. - 19. Mean annual vector diagrams. - 20. The total field vector R and its positional co-ordinates. - 21. Diurnal variation of R and ϱ in disturbance. - 22. Some diurnally varying characteristics of the current system producing disturbances. - 23. Harmonic analysis of regular diurnal variations. - . - 24. Absolute daily range. - PLATE 1. - a) Former small storehouse adapted for use as magnetograph hut. - b) Absolute hut in winter. - c) Arrangements inside magnetograph hut. Quick-run magnetograph in the foreground. Standard magnetograph in the background. - d) Arrangement of instruments in the absolute hut. Magnetic theodolite on the central pillar to the left. Dover inclinatorium on the pillar to the right. The oscillation observations were made on the lower pillar. - e) The 1882-83 station at Cape Thordsen. In the foreground the site of the old magnetic variation house. In the background the old observatory building. - f) The magnetic theodolite mounted on the reconstructed pillar used for absolute observations in 1882- 83.
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  • 42
    Series available for loan
    Series available for loan
    Washington : Dept. of Meteorology and Climatology, Univ.
    Associated volumes
    Call number: MOP 25776
    In: Scientific report / Department of Meteorology and Climatology, University of Washington, No. 4
    In: Occasional report / Department of Meteorology and Climatology, University of Washington, No. 12
    Type of Medium: Series available for loan
    Pages: VIII, 52 S. , graph. Darst.
    Series Statement: Scientific report / Department of Meteorology and Climatology, University of Washington 4
    Language: English
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  • 43
    Series available for loan
    Series available for loan
    Washington : Dept. of Meteorology and Climatology, Univ.
    Associated volumes
    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
    Language: English
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  • 44
    Series available for loan
    Series available for loan
    Washington : Department of Meteorology and Climatology, Univ.
    Associated volumes
    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
    Language: English
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  • 45
    Call number: MOP 28488
    In: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik, Nr. 53
    Type of Medium: Monograph available for loan
    Pages: 1 S.
    Series Statement: Verhandelingen / Kementerian Perhubungan Djawatan Meteorologi dan Geofisik 53
    Language: English
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  • 46
    Call number: PIK N 456-17-90919
    Type of Medium: Monograph available for loan
    Pages: IV, 89 S. , graph. Darst., Kt.
    Series Statement: Expéditions polaires françaises 212
    Language: English
    Location: A 18 - must be ordered
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  • 47
    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-202-47
    In: Research report / Cold Regions Research and Engineering Laboratory, 47
    Description / Table of Contents: Summary: Various mechanical properties such as strength, elastic modulus, and density of TUTO tunnel and ramp ice were determined. Results of unconfined compressive strength, ring tensile strength, and flexural strength tests are given. Photographs of included bubbles and grain size and shape are shown for each of six types of ice tested. Petrofabric diagrams for each type of ice are included. No significant differences in strength were found between horizontal and vertical cores in the ice tunnel, although differences between types of ice are noted. Crushing strength values found for tunnel ice generally fit the empirical equation relating crushing strength to density which was found for high-density snows (Butkovich, 1956a). However the values for ramp ice do not fit the equation when the average density values are used, probably due to the layering. The empirical equation relating ring tensile strength to density of high-density snows (ibid.) gives results approximately 20% greater than those obtained for tunnel ice. It appears that grain size influences the results. Ice with large grains consistently gives lower values. Flexural strength of the ramp ice is about half that of the tunnel ice. Comparing these results with the ring tensile values leads to the conclusion that the beams tend to fail in the lowest-density (mostly bubbly) bands. Temperature curves as a function of depth into the wall and along the tunnel length are presented. A 30-day study of deformation in a 100 x 30 ft room at 650 ft. into the tunnel indicated that the room is closing primarily by a block action, with rates of closure being less only very near the walls.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 47
    Language: English
    Note: CONTENTS Preface Summary Introduction Strength Crushing strength Ring tensile strength Flexural strength Static modulus of elasticity Dynamic modulus of elasticity Density of tunnel and ramp ice Tunnel temperature measurements Crystal size, bubble size, and ice fabrics Deformation measurements Discussion of strength test results References
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  • 48
    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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  • 49
    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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  • 50
    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
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  • 51
    Call number: PIK N 630-15-89556
    Type of Medium: Monograph available for loan
    Pages: 62 S. , zahlr. Ill.
    Edition: 1. print.
    Language: English
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  • 52
    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
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  • 53
    Monograph available for loan
    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
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    Pages: 223 S., , Ill.
    Language: English
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  • 54
    Series available for loan
    Series available for loan
    Washington : Deptament of Meteorology and Climatology, Univ.
    Associated volumes
    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
    Type of Medium: Series available for loan
    Pages: 21 S. , graph. Darst.
    Series Statement: Occasional report / University of Washington, Department of Meteorology and Climatology 4
    Language: English
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  • 55
    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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  • 56
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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-202-31
    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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  • 57
    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-202-32
    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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  • 58
    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-202-33
    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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  • 59
    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-202-34
    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.
    Type of Medium: Series available for loan
    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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  • 60
    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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  • 61
    Monograph available for loan
    Monograph available for loan
    London : Methuen
    Call number: M 00.0032 ; G 5651
    Type of Medium: Monograph available for loan
    Pages: xx, 516 S.
    Edition: 4th ed., revised and enl.
    Classification:
    Stratigraphy
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 62
    Series available for loan
    Series available for loan
    Ottawa
    Associated volumes
    Call number: SR 90.0925(18)
    In: Economic geology report
    Type of Medium: Series available for loan
    Pages: VII, 108 S. + 5 Beil.
    Series Statement: Economic geology series 18
    Language: English
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  • 63
    Series available for loan
    Series available for loan
    Ottawa
    Associated volumes
    Call number: SR 90.0925(17)
    In: Economic geology report
    Type of Medium: Series available for loan
    Pages: VII, 251 S. + 2 Kt.-Beil., 8 Beil.
    Series Statement: Economic geology series 17
    Language: English
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  • 64
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0007(16)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: V, 82 S. + 2 pl.
    Series Statement: Bulletin / Geological Survey of Canada 16
    Language: English
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  • 65
    Call number: SR 90.0007(17)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: V, 149 S.
    Series Statement: Bulletin / Geological Survey of Canada 17
    Language: English
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  • 66
    Call number: SR 90.0007(22)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: IV, 113 S. + 2 pl.
    Series Statement: Bulletin / Geological Survey of Canada 22
    Language: English
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  • 67
    Series available for loan
    Series available for loan
    Ottawa : Cloutier
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    Call number: SR 90.0007(37)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: 28 S. + 1 pl.
    Series Statement: Bulletin / Geological Survey of Canada 37
    Language: English
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  • 68
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0007(50)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: VIII, 94 S. + 2 pl.
    Series Statement: Bulletin / Geological Survey of Canada 50
    Language: English
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  • 69
    Call number: SR 90.0006(60)
    In: Memoir
    Type of Medium: Series available for loan
    Pages: IX, 719 S.
    Series Statement: Memoir / Geological Society of America 60
    Language: English
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  • 70
    Call number: SR 90.0007(32)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: 34 S. + 2 pl.
    Series Statement: Bulletin / Geological Survey of Canada 32
    Language: English
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  • 71
    Call number: SR 90.0007(42)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: V, 75 S.
    Series Statement: Bulletin / Geological Survey of Canada 42
    Language: English
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  • 72
    Call number: MOP 25770
    In: Occasional report / Department of Meteorology and Climatology, University of Washington, No. 6
    In: Air motions study, No. 3
    Type of Medium: Series available for loan
    Pages: III, 46 S. , graph. Darst., Kt.
    Series Statement: Occasional report / Department of Meteorology and Climatology, University of Washington 6
    Language: English
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  • 73
    Call number: AWI A5-97-0059 ; MOP 17854
    Type of Medium: Monograph available for loan
    Pages: IX, 1334 S.
    Edition: 2nd print.
    Language: English
    Note: Table of Contents: COMPOSITION OF THE ATMOSPHERE. - The Composition of Atmospheric Air / by E. Glueckauf. - RADIATION. - Solar Radiant Energy and Its Modification by the Earth and Its Atmosphere / by Sigmund Fritz. - Long-Wave Radiation / by Fritz Möller. - Actinometric Measurements / by Anders Ångström. - METEOROLOGICAL OPTICS - General Meteorological Optics / by Hans Neuberger. - Polarization of Skylight / by Zdeněk Sekera. - Visibility in Meteorology / by W. E. Knowles Middleton. - ATMOSPHERIC ELECTRICITY. - Universal Aspects of Atmospheric Electricity / by O. H. Gish. - Ions in the Atmosphere / by G. R. Wait and W. D. Parkinson. - Precipitation Electricity / by Ross Gunn. - The Lightning Discharge / by J. H. Hagenguth. - Instruments and Methods for the Measurement of Atmospheric Electricity / by H. Israël. - Radioactivity of the Atmosphere / by H. Israël. - CLOUD PHYSICS. - On the Physics of Clouds and Precipitation / by Henry G. Houghton. - Nuclei of Atmospheric Condensation / by Christian Junge. - The Physics of Ice Clouds and Mixed Clouds / by F. H. Ludlam. - Thermodynamics of Clouds / by Fritz Möller. - The Formation of Ice Crystals / by Ukichiro Nakaya. - Snow and Its Relationship to Experimental Meteorology / by Vincent J. Schaefer. - Relation of Artificial Cloud-Modification to the Production of Precipitation / by Richard D. Coons and Ross Gunn. - THE UPPER ATMOSPHERE. - General Aspects of Upper Atmospheric Physics / by S. K. Mitra. - Photochemical Processes in the Upper Atmosphere and Resultant Composition / by Sidney Chapman. - Ozone in the Atmosphere by F. W. Paul Götz. - Radiative Temperature Changes in the Ozone Layer / by Richard A. Craig. - Temperatures and Pressures in the Upper Atmosphere / by Homer E. Newell, Jr. - Water Vapour in the Upper Air / by G. M. B. Dobson and A. W. Brewer. - Diffusion in the Upper Atmosphere / by Heinz Lettau. - The Ionosphere / by S. L. Seaton. - Night-Sky Radiations from the Upper Atmosphere / by E. O. Hulburt. - Aurorae and Magnetic Storms / by L. Harang. - Meteors as Probes of the Upper Atmosphere / by Fred L. Whipple. - Sound Propagation in the Atmosphere / by B. Gutenberg. - COSMICAL METEOROLOGY. - Solar Energy Variations As a Possible Cause of Anomalous Weather Changes / by Richard A. Craig and H. C. Willett. - The Atmospheres of the Other Planets / by S. L. Hess and H. A. Panofsky. - DYNAMICS OF THE ATMOSPHERE. - The Perturbation Equations in Meteorology / by B. Haurwitz. - The Solution of Nonlinear Meteorological Problems by the Method of Characteristics / by John C. Freeman. - Hydrodynamic Instability / by Jacques M. Van Mieghem. - Stability Properties of Large-Scale Atmospheric Disturbances / by R. Fjørtoft. - The Quantitative Theory of Cyclone Development / by E. T. Eady. - Dynamic Forecasting by Numerical Process / by J. G. Charney. - Energy Equations / by James E. Miller. - Atmospheric Turbulence and Diffusion / by O. G. Sutton. - Atmospheric Tides and Oscillations / by Sydney Chapman. - Application of the Thermodynamics of Open Systems to Meteorology / by Jacques M. Van Mieghem. - THE GENERAL CIRCULATION. - The Physical Basis for the General Circulation / by Victor P. Starr. - Observational Studies of General Circulation Patterns / by Jerome Namias and Philip F. Clapp. - Applications of Energy Principles to the General Circulation / by Victor P. Starr. - MECHANICS OF PRESSURE SYSTEMS. - Extratropical Cyclones / by J. Bjerknes. - The Aerology of Extratropical Disturbances / by E. Palmén. - Anticyclones / by H. Wexler. - Mechanism of Pressure Change / by James M. Austin. - Large-Scale Vertical Velocity and Divergence / by H. A. Panofsky. - The Instability Line / by J. R. Fulks. - LOCAL CIRCULATIONS. - Local Winds / by Friedrich Defant. - Tornadoes and Related Phenomena / by Edward M. Brooks. - Thunderstorms / by Horace R. Byers. - Cumulus Convection and Entrainment / by James M. Austin. - OBSERVATIONS AND ANALYSIS. - World Weather Network / by Athelstan F. Spilhaus. - Models and Techniques of Synoptic Representation / by John C. Bellamy. - Meteorological Analysis in the Middle Latitudes / by V. J. Oliver and M. B. Oliver. - WEATHER FORECASTING. - The Forecast Problem / by H. C. Willett. - Short-Range Weather Forecasting / by Gordon E. Dunn. - A Procedure of Short-Range Weather Forecasting / by Robert C. Bundgaard. - Objective Weather Forecasting / by R. A. Allen and E. M. Vernon. - General Aspects of Extended-Range Forecasting / by Jerome Namias. - Extended-Range Weather Forecasting / by Franz Baur. - Extended-Range Forecasting by Weather Types / by Robert D. Elliott. - Verification of Weather Forecasts / by Glenn W. Brier and Roger A. Allen. - Application of Statistical Methods to Weather Forecasting / by George P. Wadsworth. - TROPICAL METEOROLOGY. - Tropical Meteorology / by C. E. Palmer. - Equatorial Meteorology / by A. Grimes. - Tropical Cyclones / by Gordon E. Dunn. - Aerology of Tropical Storms / by Herbert Riehl. - POLAR METEOROLOGY. - Antarctic Atmospheric Circulation / by Arnold Court. - Arctic Meteorology / by Herbert G. Dorsey, Jr. - Some Climatological Problems of the Arctic and Sub-Arctic / by F. Kenneth Hare. - CLIMATOLOGY. - Climate - The Synthesis of Weather / by C. S. Durst. - Applied Climatology / by Helmut E. Landsberg and Woodrow C. Jacobs. - Microclimatology / by Rudolf Geiger. - Geological and Historical Aspects of Climatic Change / by C. E. P. Brooks. - Climatic Implications of Glacier Research / by Richard Foster Flint. - Tree-Ring Indices of Rainfall, Temperature, and River Flow / by Edmund Schulman. - HYDROMETEOROLOGY. - Hydrometeorology in the United States / by Robert D. Fletcher. - The Hydrologic Cycle and Its Relation to Meteorology - River Forecasting / by Ray K. Linsley. - MARINE METEOROLOGY. - Large-Scale Aspects of Energy Transformation over the Oceans / by Woodrow C. Jacobs. - Evaporation from the Oceans / by H. U. Sverdrup. - Forecasting Ocean Waves / by W. H. Munk and R. S. Arthur. - Ocean Waves as a Meteorological Tool / by W. H. Munk. - BIOLOGICAL AND CHEMICAL METEOROLOGY. - Aerobiology / by Woodrow C. Jacobs. - Physical Aspects of Human Bioclimatology / by Konrad J. K. Buettner. - Some Problems of Atmospheric Chemistry / by H. Cauer. - ATMOSPHERIC POLLUTION. - Atmospheric Pollution / by E. Wendell Hewson. - CLOUDS, FOG, AND AIRCRAFT ICING. - The Classification of Cloud Forms / by Wallace E. Howell. - The Use of Clouds in Forecasting / by Charles F. Brooks. - Fog / by Joseph J. George. - Physical and Operational Aspects of Aircraft Icing / by Lewis A. Rodert. - Meteorological Aspects of Aircraft Icing / by William Lewis. - METEOROLOGICAL INSTRUMENTS. - Instruments and Techniques for Meteorological Measurements / by Michael Ference, Jr. - Aircraft Meteorological Instruments / by Alan C. Bemis. - LABORATORY INVESTIGATIONS. - Experimental Analogies to Atmospheric Motions / by Dave Fultz. - Model Techniques in Meteorological Research / by Hunter Rouse. - Experimental Cloud Formation / by Sir David Brunt. - RADIOMETEOROLOGY. - Radar Storm Observation / by Myron G. H. Ligda. - Theory and Observation of Radar Storm Detection / by Raymond Wexler. - Meteorological Aspects of Propagation Problems / by H. G. Booker. - Sferics / by R. C. Wanta. - MICROSEISMS. - Observations and Theory of Microseisms / by B. Gutenberg. - Practical Application of Microseisms to Forecasting / by James B. Macelwane, S. J. CORRIGENDA. - INDEX.
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  • 74
    Monograph available for loan
    Monograph available for loan
    Seattle, Wash.
    Associated volumes
    Call number: MOP 25774
    In: Occasional report / Department of Meteorology and Climatology, University of Washington, No. 10
    In: Scientific report / Department of Meteorology and Climatology University of Washington, No. 1
    Type of Medium: Monograph available for loan
    Pages: VII, 41 S. , graph. Darst., Kt.
    Series Statement: Occasional report / Department of Meteorology and Climatology, University of Washington 10
    Language: English
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  • 75
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 97.0377/1 / Regal 12
    In: A descriptive petrography of the igneous rocks
    Type of Medium: Monograph available for loan
    Pages: XXIV, 318 S.
    Edition: 2nd ed.
    Classification:
    Petrology, Petrography
    Language: English
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  • 76
    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
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    Location: MOP - must be ordered
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  • 77
    Monograph available for loan
    Monograph available for loan
    Chicago : Univ. of Chicago Press
    Call number: M 93.0054
    Type of Medium: Monograph available for loan
    Pages: XVI, 911 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
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  • 78
    Call number: ZSP-201-10
    In: SIPRE report, 10
    Type of Medium: Series available for loan
    Pages: 97 Seiten
    Series Statement: SIPRE report 10
    Language: English
    Note: Contents Foreword Synopsis Introduction Authority Purpose and scope SIPRE organization and activities Cryological problems and military end points Present state of knowledge General Introduction Terminology and classification Snow and ice Introduction Physical properties and geometry Density and water equivalent Water holding or storage capacity of snow Water transmission through snow Bound water Crystallography and metamorphism Porosity and permeability Mechanical properties Elasto-plastic properties Friction Strength Hardness Electromagnetic properties Dielectric constants Conductivity Magnetic properties Piezoelectric and pyroelectric effects Triboelectricity Freezing potential Thermodynamic properties Thermal properties Radiation Phase relations Engineering problems Snow and ice removal Snow compaction Snow draft control Trafficability Temporary structures Snow melt and runoff Maps Frozen ground and permafrost Introduction Frost action Theory of frost action Cyclic freezing and thawing Manifestations of frost actions Frost heave on freezing Reduction in load-carrying capacity on thawing Soil movements on slopes Ground properties affecting or affected by frost action Composition, grain size, and grain-size distribution Soil-moisture-movement properties Thermal properties Structure of unfrozen ground Structure of frozen ground Strength of frozen ground Freezing point Ground conditions affecting or affected by frost action Density Degree of saturation Interrelation of climate, position, vegetation, and soil Frost phenomena Climate Position Vegetation Engineering problems Excavation and replacement Subsurface drainage Base courses Insulation courses Surface icing and its control Trafficability Building foundations Maps Current related research Introduction Military cryological research in United States and Canada Non-military cryological research in the Western World Research needed Introduction Subjects for fundamental research Subjects for applied research
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  • 79
    Monograph available for loan
    Monograph available for loan
    Bergen : Grieg
    Associated volumes
    Call number: AWI E2-99-0137 (4)
    In: The Norwegian north polar expedition with the "MAUD" 1918 - 1925
    Type of Medium: Monograph available for loan
    Pages: 288 S. : Ill., graph. Darst., Kt.
    Series Statement: The Norwegian north polar expedition with the "MAUD" 1918 - 1925
    Language: English
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  • 80
    Call number: ZSP-553-159,4
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 17 S. : Ill.
    Series Statement: Meddelelser om Grønland 159,4
    Language: English
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  • 81
    Monograph available for loan
    Monograph available for loan
    København : Lunos
    Associated volumes
    Call number: ZSP-553-156,5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Series Statement: Meddelelser om Grønland 156,5
    Language: English
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  • 82
    Call number: ZSP-553-159,2
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 14 S. : Ill.
    Series Statement: Meddelelser om Grønland 159,2
    Language: English
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  • 83
    Call number: M 93.0188
    In: Society of Economic Paleontologists and Mineralogists. Special Publications
    Type of Medium: Monograph available for loan
    Pages: 178 S. : Ill., graph. Darst.
    Series Statement: Society of Economic Paleontologists and Mineralogists. Special Publications 5
    Language: English
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  • 84
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow, Ice and Permafrost Research Establishment
    Associated volumes
    Call number: ZSP-201-11
    In: SIPRE report, 11
    Description / Table of Contents: A commercial deep-freeze unit was modified to serve as a laboratory for growing single crystals, cutting specimens of a given orientation, testing these specimens in compressive creep, and studying thin-sections of the results on a universal stage. A method of growing single crystals of adequate size was developed by adapting the Bridgman method. Fortyone creep tests were made at temperatures ranging from -1° to -18°C. These gave an unexpected form of creep-curve in which the rate of strain continuously increases with time. The mechanism of deformation is dominantly basal translation—consistent with earlier work. The dependence on temperature and stress is expressed empirically.
    Type of Medium: Series available for loan
    Pages: 24 Seiten , Illustrationen
    Series Statement: SIPRE report 11
    Language: English
    Note: Contents Introduction Use of the deep-freeze as a cold laboratory Growing single crystals Creep tests Conclusions References cited
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  • 85
    Call number: ZSP-201-20
    In: SIPRE report, 20
    Description / Table of Contents: Work carried out at the SIPRE Test Site, Site 2, on the Greenland Ice Cap,during the summer 1954, included: (1) Excavation of trenches, a circular tunnel and a deep pit; (2) Instrumentation of excavations for pressure and deformation measurements; (3) Tests on the properties of snow from the deep pit; (4) Construction of a snow house as an experimental structure and to provide a heated shelter for an observer stationed at the site for the winter. Observations and measurements over a period of five years are expected to provide sufficient information for the establishment of satisfactory design criteria for all kinds of surface and subsurface military installations on high polar ice caps.
    Type of Medium: Series available for loan
    Pages: 31 Seiten , Illustrationen
    Series Statement: SIPRE report 20
    Language: English
    Note: Contents I. Introduction, by H. Bader II. Excavation of trenches and tunnels, by R.W. Waterhouse III. Excavation of deep pit, by J.K. Landauer IV. Trench covering, framing, and instrumentation, by R.W. Waterhouse V. The snow house, by R.W. Waterhouse VI. Load measurements in the N-S trench, by R.W. Waterhouse VII. Deformation measurements, by J.K. Landauer VIII. Distance changes on the ice cap, by B.L. Hansen and H. Bader IX. Annual accumulation, by H. Bader X. Snow density and snow load in deep pit, by J.K. Landauer XI. Air permeability of snow from deep pit, by J.A. Bender XII. Viscosity of snow from deep pit, by J.K. Landauer XIII. Crushing strength of snow from deep pit, by T.R. Butkovich XIV. Shear strength of snow from deep pit, by T.R. Butkovich XV. Tensiel strength of snow from deep pit, by T.R. Butkovich XVI. Angle of internal friction of snow from deep pit, by T.R. Butkovich XVII. Snow temperatures, by J.K. Landauer
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  • 86
    Monograph available for loan
    Monograph available for loan
    Chicago : Univ. of Chicago Pr.
    Associated volumes
    Call number: M 97.0377/4 / Regal 12
    In: A descriptive petrography of the igneous rocks
    Type of Medium: Monograph available for loan
    Pages: xvii, 523 S.
    Classification:
    Petrology, Petrography
    Language: English
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  • 87
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(906-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 42 S. + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 906-A
    Language: English
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  • 88
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: SR 90.0001(890-A)
    In: U.S. Geological Survey bulletin
    In: Spirit leveling in South Carolina
    Type of Medium: Series available for loan
    Pages: II, 455 S. + 1 pl.
    Series Statement: 890-A
    Language: English
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  • 89
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(910-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 115-145
    Series Statement: U.S. Geological Survey bulletin 910-B
    Language: English
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  • 90
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(906-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 43-84 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 906-B
    Language: English
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  • 91
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(906-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 85-133 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 906-C
    Language: English
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  • 92
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(906-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 135-188
    Series Statement: U.S. Geological Survey bulletin 906-D
    Language: English
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  • 93
    Call number: SR 90.0001(900-B)
    In: U.S. Geological Survey bulletin
    In: Subsurface geology and oil and gas resources of Osage County, Oklahoma
    Type of Medium: Series available for loan
    Pages: IV S., S. 47-82 + 1 pl.
    Series Statement: 900-B
    Language: English
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  • 94
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(969-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 87-103 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 969-D
    Language: English
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  • 95
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(969-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 105-149 + 17 pl.
    Series Statement: U.S. Geological Survey bulletin 969-E
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 96
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(985)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 394 S.
    Series Statement: U.S. Geological Survey bulletin 985
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 97
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(977)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 273 S.
    Series Statement: U.S. Geological Survey bulletin 977
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 98
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(993)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 104 S. + 5 pl.
    Series Statement: U.S. Geological Survey bulletin 993
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 99
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(988-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 69-87 + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 988-F
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 100
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(989-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 26 S.
    Series Statement: U.S. Geological Survey bulletin 989-A
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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