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  • English  (1,498)
  • Swedish  (4)
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  • 1965-1969  (1,502)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs : Prentice-Hall
    Call number: M 93.0220
    Type of Medium: Monograph available for loan
    Pages: VIII, 152 S. : Ill.
    Edition: 4. print.
    Series Statement: Foundations of earth science
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York : Reinhold
    Call number: M 93.0129
    Type of Medium: Monograph available for loan
    Pages: VIII, 226 S.
    Language: English
    Location: Upper compact magazine
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  • 3
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs : Prentice-Hall
    Call number: M 93.0219
    Type of Medium: Monograph available for loan
    Pages: VIII, 149 S. : Ill.
    Edition: 6. print.
    Series Statement: Foundations of earth science
    Language: English
    Location: Upper compact magazine
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  • 4
    Monograph available for loan
    Monograph available for loan
    New York : Harper & Row [u.a.]
    Call number: M 93.0005
    Type of Medium: Monograph available for loan
    Pages: XIII, 450 S.
    Series Statement: A Harper International student reprint
    Language: English
    Location: Upper compact magazine
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  • 5
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs : Prentice-Hall
    Call number: M 93.0095
    Type of Medium: Monograph available for loan
    Pages: X, 115 S.
    Language: English
    Location: Upper compact magazine
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 93.0192
    Type of Medium: Monograph available for loan
    Pages: XXIV, 828 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
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  • 7
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs : Prentice-Hall
    Call number: M 93.0133
    Type of Medium: Monograph available for loan
    Pages: IX, 149 S.
    Language: English
    Location: Upper compact magazine
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  • 8
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 6743 ; M 93.0085/4
    In: Methods in geochemistry and geophysics
    Type of Medium: Monograph available for loan
    Pages: XII, 258 S. : Ill.
    Series Statement: Methods in geochemistry and geophysics 4
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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    Branch Library: GFZ Library
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  • 9
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: G 5066 ; 6743 ; 7763 ; M 93.0085/2
    In: Methods in geochemistry and geophysics
    Type of Medium: Monograph available for loan
    Pages: X, 265 S. : graph. Darst.
    Series Statement: Methods in geochemistry and geophysics 2
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
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    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 10
    Monograph available for loan
    Monograph available for loan
    Oak Ridge
    Call number: M 93.0145
    Type of Medium: Monograph available for loan
    Pages: XVI, 1250 S.
    Language: English
    Location: Upper compact magazine
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  • 11
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0069/3
    In: Geochemistry and mineralgy of rare elements and genetic types of their deposits
    Type of Medium: Monograph available for loan
    Pages: XX, 916 S. : graph. Darst., Kt.
    Uniform Title: Geneticheskie tipy mestorozhdenii redkikh elementov
    Language: English
    Location: Upper compact magazine
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  • 12
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill
    Call number: G 5319
    Type of Medium: Monograph available for loan
    Pages: XIII, 721 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
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  • 13
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs : Prentice-Hall
    Call number: M 93.0218
    Type of Medium: Monograph available for loan
    Pages: VIII, 120 S. : Ill.
    Edition: 4. print.
    Series Statement: Foundations of earth science
    Language: English
    Location: Upper compact magazine
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  • 14
    Call number: M 93.0144
    Type of Medium: Monograph available for loan
    Pages: 253 S.
    Language: English
    Location: Upper compact magazine
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  • 15
    Call number: M 93.0140
    In: NASA SP
    Type of Medium: Monograph available for loan
    Pages: IX, 256 S. : überw. Ill.
    Series Statement: NASA SP 129
    Language: English
    Location: Upper compact magazine
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  • 16
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0069/1
    In: Geochemistry and mineralgy of rare elements and genetic types of their deposits
    Type of Medium: Monograph available for loan
    Pages: XIII, 688 S. : graph. Darst.
    Uniform Title: Geokhimiya redkikh elementov
    Language: English
    Location: Upper compact magazine
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  • 17
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0078/1
    In: Chemical oceanography
    Type of Medium: Monograph available for loan
    Pages: XIX, 712 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
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  • 18
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0069/2
    In: Geochemistry and mineralgy of rare elements and genetic types of their deposits
    Type of Medium: Monograph available for loan
    Pages: XX, 945 S. : graph. Darst.
    Uniform Title: Mineralogiya redkikh elementov
    Language: English
    Location: Upper compact magazine
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  • 19
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0087/3
    In: The sea
    Type of Medium: Monograph available for loan
    Pages: XVI, 963 S. : Ill., graph. Darst., Kt.
    Edition: 2nd print.
    Language: English
    Location: Upper compact magazine
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  • 20
    Call number: 8205 ; M 93.0203
    In: Astrophysics and space science library
    Type of Medium: Monograph available for loan
    Pages: XV, 940 S. : Ill., graph. Darst.
    Series Statement: Astrophysics and space science library 12
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 21
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    Unknown
    London [u.a.]: Academic Press
    Associated volumes
    Call number: 93.0079
    In: Chemical oceanography
    Language: English
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  • 22
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0078/2 ; M 93.0079/2
    In: Chemical oceanography
    Type of Medium: Monograph available for loan
    Pages: XV, 508 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 23
    Series available for loan
    Series available for loan
    Stockholm
    Associated volumes
    Call number: SR 93.0767(45)
    In: Sveriges geologiska undersökning. Serie Ca, Avhandlingar och uppsater
    Type of Medium: Series available for loan
    Pages: 418 S. + 8 Kt.
    Series Statement: Sveriges geologiska undersökning : Ser. Ca, Avhandlingar och uppersatser 45
    Language: Swedish
    Location: Lower compact magazine
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  • 24
    Monograph available for loan
    Monograph available for loan
    New York : Consultants Bureau
    Call number: M 140
    Type of Medium: Monograph available for loan
    Pages: 56 S. : graph. Darst.
    Uniform Title: K Metodike opredelenija okislitelnovosstanovitelnogo potenciala i pH osadochnych porod
    Language: English
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  • 25
    Monograph available for loan
    Monograph available for loan
    New York, NY : Consultants Bureau
    Call number: O 3730
    Type of Medium: Monograph available for loan
    Pages: VII, 68 S.
    Series Statement: Seminars in mathematics 3
    Uniform Title: Nekotorye voprosy teorii potenciala i teorii funkcij dklja oblastej s nereguljarnymi granicami
    Language: English
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  • 26
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: G 5365 ; 13/M 93.0189
    In: Elsevier oceanography series
    Type of Medium: Monograph available for loan
    Pages: XIII, 312 S. : Ill., graph. Darst., Kt.
    Series Statement: Elsevier oceanography series 1
    Language: English
    Location: Upper compact magazine
    Location: Reading room
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  • 27
    Call number: SR 99.0125(157)
    In: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften
    Type of Medium: Series available for loan
    Pages: 28 S.
    Series Statement: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften : Reihe B, Angewandte Geodäsie 157
    Language: English
    Location: Lower compact magazine
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  • 28
    Series available for loan
    Series available for loan
    München : Beck
    Associated volumes
    Call number: SR 99.0044(58)
    In: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften
    Type of Medium: Series available for loan
    Pages: 107 S.
    Series Statement: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften : Reihe A, Höhere Geodäsie 58
    Language: English
    Location: Lower compact magazine
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  • 29
    Series available for loan
    Series available for loan
    Stockholm
    Associated volumes
    Call number: SR 93.0768(613)
    In: Sveriges Geologiska Undersökning
    Type of Medium: Series available for loan
    Pages: 24 S.
    Series Statement: Sveriges geologiska undersökning : Ser. C, Avhandlingar och uppsatser 613
    Language: English
    Location: Lower compact magazine
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  • 30
    Monograph available for loan
    Monograph available for loan
    London : Wykeham Publications
    Associated volumes
    Call number: AWI A5-16-89783
    In: The Wykeham science Series ; 3, 3
    Type of Medium: Monograph available for loan
    Pages: xv, 240 S. , Ill., graph. Darst. , 22 cm
    Edition: Repr.
    ISBN: 0851090400
    Series Statement: The Wykeham science series 3
    Language: English
    Note: Contents: Preface. - Symbols, units and numerical values. - 1. The nature and scope of meteorology. - 1.1. Meteorology in relation to other sciences. - 1.2. Variations in space and time. - 1.3. Applied meteorology. - 2. Physical properties of the atmosphere. - 2.1. Composition of dry air. - 2.1.1. Mean molecular weight. - 2.1.2. Dissociation and ionization. - 2.1.3. Escape to space of component molecules. - 2.2. Pressure, density and temperature. - 2.2.1. Definition of pressure. - 2.2.2. Values near sea level. - 2.2.3. Variations in the vertical. - 2.2.4. Diurnal fluctuations at upper levels. - 2.2.5. Horizontal pressure gradients. - 2.3. Water vapour. - 2.3.1. Humidity mixing ratio. - 2.3.2. Density of moist air. - 2.3.3. Saturation vapour pressure. - 2.3.4. Paths leading to saturation. - 2.3.5. Measurement of vapour pressure. - 2.3.6. Distribution of water vapour. - 3. Heat transfer. - 3.1. Radiation processes. - 3.1.1. Solar radiation: its energy distribution. - 3.1.2. The solar constant. - 3.1.3. Effect of the atmosphere and earth on solar radiation. - 3.1.4. Radiation from the earth and atmosphere. - 3.2. Convection. - 3.2.1. Adiabatic temperature changes. - 3.2.2. Adiabatic equation. - 3.2.3. Potential temperature: dry adiabatic lapse rate. - 3.2.4 Saturated adiabatic lapse rate. - 3.2.5. Stability and instability. - 3.3. Heat transfer in land and sea. - 3.3.1. Heating and cooling of soil. - 3.3.2. Heating and cooling of water. - 4. Condensation and precipitation. - 4.1. Microphysical processes. - 4.1.1 Condensation nuclei. - 4.1.2. Curvature and solute effects. - 4.1.3. Water-droplet clouds. - 4.1.4. Ice nuclei. - 4.1.5. Ice-crystal clouds. - 4.1.6. Precipitation from water clouds. - 4.1.7. Precipitation from mixed clouds. - 4.1.8. Thunderstorm electricity. - 4.2. Larger-scale processes. - 4.2.1. Surface cooling. - 4.2.2. Evaporation. - 4.2.3. Vertical motion. - 4.3. Cloud observations. - 4.3.1. Cloud genera: their heights and composition. - 4.3.2. Cloud recognition and general features. - 4.3.3. Effects of vertical wind shear. - 4.3.4. Cloud classification for forecasting. - 5. The tephigram. - 5.1. Construction of the diagram. - 5.1.1. Coordinates: area and energy. - 5.1.2. Isobars. - 5.1.3. Saturation mixing ratio lines. - 5.1.4. Saturated adiabatics. - 5.1.5. Height variation. - 5.2. Simple graphical computations. - 5.2.1. Height. - 5.2.2. Humidity elements. - 5.2.3. Condensation levels. - 5.2.4. Föhn effects. - 5.3. Precipitable water and precipitation rate. - 5.3.1. Formula and calculation. - 5.3.2. Precipitation rate. - 5.3.3. Water content of convection clouds. - 5.4. The effects of vertical motion on lapse rate. - 5.4.1. Unsaturated or saturated motion. - 5.4.2. Potential (convective) instability. - 5.5. Tephigram analysis. - 5.5.1. Latent instability. - 5.5.2. Air mass characteristics. - 6. Winds. - 6.1. Laws of motion and the earth's rotation. - 6.1.1. Newton's First and Second Laws. - 6.1.2. Nature of the earth's rotation. - 6.1.3. Effects of the earth's rotation: the Coriolis force. - 6.2. Inertial flow and geostrophic winds. - 6.2.1. Nature of inertial flow. - 6.2.2. Nature of geostrophic flow. - 6.2.3. Geostrophic wind equation. - 6.2.4. Wind and pressure near the equator. - 6.3. Gradient winds. - 6.4. Winds in the friction layer. - 6.5. Thermal winds. - 6.5.1. Vertical shear vector. - 6.5.2. Temperature control of the shear vector. - 6.5.3. Thermal wind equation and thickness charts. - 6.5.4. Hodographs and temperature advection. - 6.5.5. Jet streams. - 7. Instruments and observations. - 7.1. Routine surface observations. - 7.1.1. Pressure. - 7.1.2. Temperature and humidity. - 7.1.3. Precipitation and evaporation. - 7.1.4. Wind. - 7.1.5. Clouds and visibility. - 7.1.6. Sunshine and radiation. - 7.1.7. Ship observations. - 7.2. Upper air observations. - 7.2.1. Historical. - 7.2.2. The radiosonde: radar winds. - 7.2.3. Ozone measurements. - 7.3. World Weather Watch. - 7.4. Experiments in observation and interpretation. - 7.4.1. Pressure. - 7.4.2. Temperature and humidity. - 7.4.3. Evaporation and rainfall. - 7.4.4. Wind. - 7.4.5. Radiation. - 7.4.6. Topographical influences. - 8. Synoptic Meteorology. - 8.1. The surface weather map: an introduction. - 8.1.1. The plotting code. - 8.1.2. Pressure systems and features. - 8.1.3. Air masses. - 8.1.4. Fronts. - 8.2. Air mass characteristics. - 8.2.1. Classification. - 8.2.2. Modifications. - 8.2.3. Air masses over the British Isles. - 8.3. Frontal characteristics. - 8.3.1. The stability of a frontal surface. - 8.3.2. Equilibrium slope of a frontal surface. - 8.3.3. Frontal structure. - 8.4. Frontal depressions. - 8.4.1. The life cycle of a frontal depression. - 8.4.2. Cold front waves; depression families. - 8.4.3. Warm front waves. - 8.4.4. Secondaries at points of occlusion. - 8.5. Non-frontal depressions. - 8.5.1. Heat lows. - 8.5.2. Polar lows. - 8.5.3. Orographic lows. - 8.5.4. Tropical cyclones. - 8.5.5. Tornadoes. - 8.6. Anticyclones. - 8.6.1. General characteristics. - 8.6.2. Cold and warm anticyclones. - 8.7 Synoptic development. - 8.7.1. Convergence, divergence and vertical motion. - 8.7.2. Convergence and vorticity. - 8.7.3 Long waves. - 8.7.4. Circulation indices: blocking. - 8.8. Surface analysis. - 8.8.1. General. - 8.8.2. Representativeness of observations. - 8.8.3. METMAPS. - 9. Micrometeorology. - 9.1. The nature of airflow near the ground. - 9.1.1. Wind speeds over a uniform level surface. - 9.1.2. Flow within a fluid boundary layer. - 9.1.3. Shearing stress via the mixing length concept. - 9.1.4. The friction velocity u*. - 9.1.5. Interpretation of the mixing length concept. - 9.1.6. The wind profile equation in complete form. - 9.2. The influence of surface roughness on the wind. - 9.2.1. Roughness in the aerodynamic sense. - 9.2.2. Roughness in relation to shearing stress and mean wind speed. - 9.2.3. The drag coefficient CD. - 9.2.4. CD as a transfer coefficient. - 9.2.5. Effect of a change in surface roughness. - 9.3. Vertical transport by turbulence. - 9.3.1. Flux equations; use of electrical analogy. - 9.3.2. Heat flux and other calculations. - 9.3.3. Vertical temperature gradients in relation to turbulent exchange. - 10. The general circulation. - 10.1. General characteristics. - 10.1.1. Genesis and interactions. - 10.1.2. Time fluctuations. - 10.2. Observations. - 10.2.1. Time- and space-averaging. - 10.2.2. Tracers. - 10.3. Experiment and theory. - 10.3.1. The rotating vessel experiment. - 10.3.2. Conservation principles. - 10.3.3. Cellular models. - 10.4. Climatic zones. - 11. Weather forecasting. - 11.1. Historical survey. - 11.1.1. 1860-1920. - 11.1.2. 1920-1945. - 11.1.3. 1945-1960. - 11.1.4. 1960 onwards. - 11.2. Conventional forecasting. - 11.2.1. Pressure tendency. - 11.2.2. Making the forecast. - 11.3. Long-range forecasting. - 11.3.1. Statistical methods. - 11.3.2. Synoptic methods. - 11.3.3. Analogues. - 11.4. Numerical forecasting. - 11.4.1. The barotropic model. - 11.4.2. Later developments. - 11.5. Predictability and control. - 11.5.1. Short-range predictability. - 11.5.2. Medium-range predictability. - 11.5.3. Long-range predictability: climatic trends. - 11.5.4. Weather and climate modification. - Answers to Problems. - Subject Index. - The Wykeham Series.
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  • 31
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : Belknap Press of Harvard University
    Call number: IASS 16.90614
    Type of Medium: Monograph available for loan
    Pages: 323 S.
    ISBN: 0674794850 , 9780674794856
    Language: English
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  • 32
    Call number: MOP 41158 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 122 Seiten , Illustrationen
    Language: English
    Location: MOP - must be ordered
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  • 33
    Monograph available for loan
    Monograph available for loan
    Paris : Organisation Européenne de Recherches Spatiales
    Call number: MOP 41394 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 55 Seiten , Illustrationen
    Series Statement: European Space Research Organization: Scientific note 54
    Language: English
    Location: MOP - must be ordered
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  • 34
    Call number: MOP 40071 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VII, 50 Seiten , Illustrationen, Karten
    Series Statement: Hydrology papers 15
    Language: English
    Location: MOP - must be ordered
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  • 35
    Monograph available for loan
    Monograph available for loan
    New York : Dover Publications
    Call number: M 15.89026
    Type of Medium: Monograph available for loan
    Pages: xvi, 504 S. , graph. Darst.
    Edition: Repr. of 2. ed. rev. and enl., 1894.
    ISBN: 0-486-60293-1
    Series Statement: Dover classics of science and mathematics
    Language: English
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  • 36
    Monograph available for loan
    Monograph available for loan
    New York : Dover Publications
    Call number: M 15.89027
    Type of Medium: Monograph available for loan
    Pages: XLII, 480 S. , graph. Darst.
    Edition: Repr. of 2. ed. rev. and enl., 1894.
    ISBN: 0-486-60292-3
    Series Statement: Dover classics of science and mathematics
    Language: English
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  • 37
    Monograph available for loan
    Monograph available for loan
    Lahaina, Hawaii : Ross-Hargreaves
    Call number: PIK N 630-15-89560
    Type of Medium: Monograph available for loan
    Pages: 64 S. , zahlr. Ill.
    Language: English
    Location: A 18 - must be ordered
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  • 38
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : U.S. Dept. of Commerce
    Call number: PIK N 456-16-90161/1 ; PIK N 456-16-90161/2
    Type of Medium: Monograph available for loan
    Pages: 621 S. : graph. Darst., Kt. , gebundene Kopie in 2 Bänden
    Edition: 2nd print.
    Uniform Title: Chung-kuo chi-hou 〈engl.〉
    Language: English
    Location: A 18 - must be ordered
    Location: A 18 - must be ordered
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    Branch Library: PIK Library
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  • 39
    Call number: AWI S1-18-91339
    Type of Medium: Monograph available for loan
    Pages: 608 S.
    Edition: 4. ed., repr.
    Language: English
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  • 40
    Monograph available for loan
    Monograph available for loan
    Dublin : Department of Transport and Power, Meteorological Service
    Call number: MOP 36777
    Type of Medium: Monograph available for loan
    Pages: 72 Seiten , Illustrationen, Tabellen
    Language: English
    Location: MOP - must be ordered
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  • 41
    Call number: AWI G7-19-92221
    Type of Medium: Series available for loan
    Pages: Seiten 437 - 505 , Illustrationen
    Series Statement: Philosophical transactions of the Royal Society : Series A, Mathematical and physical sciences 265.1969,1166
    Language: English
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  • 42
    Monograph available for loan
    Monograph available for loan
    Boston : American Meteorological Society
    Call number: MOP 40509 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 347 Seiten , Illustrationen
    Language: English
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  • 43
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 43365 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 338 Seiten , Illustrationen , 3 Karten , 27 cm
    Series Statement: Meždunarodnoe Gidrologičeskoe Desjatiletie / AN SSSR. Institut Geografii
    Language: Russian , English
    Note: In kyrillischer Schrift , Mit Zusammenfassung und Inhaltsverzeichnis in englischer Sprache
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  • 44
    Monograph available for loan
    Monograph available for loan
    New York [u.a] : McGraw-Hill
    Call number: 6293
    Type of Medium: Monograph available for loan
    Pages: x, 244 S. : graph. Darst.
    Series Statement: McGraw-Hill Physical and Quantum Electronics Series
    Language: English
    Location: Upper compact magazine
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  • 45
    Monograph available for loan
    Monograph available for loan
    Haifa : Dep. of Education and Culture
    Call number: PIK N 630-15-89532
    Type of Medium: Monograph available for loan
    Pages: 24 Bl. , zahlr. Ill.
    Language: English , French
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  • 46
    Monograph available for loan
    Monograph available for loan
    Fort Collins : Dept. of Atmospheric Science, Colorado State University
    Call number: MOP 35141
    Type of Medium: Monograph available for loan
    Pages: 54 S. , Ill.
    Language: English
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  • 47
    Call number: MOP 35293
    Type of Medium: Monograph available for loan
    Pages: 80 S. , graph. Darst.
    Series Statement: Atmospheric science paper 107
    Language: English
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  • 48
    Call number: 21/SR 90.0917(1-3)
    Type of Medium: Series available for loan
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde 1, 2, 3
    Language: English
    Note: Nr. 1 Untersuchung der Polarisation und anderer Eigenschaften der langperiodischen Mikroseismik von Uwe Walzer (1969) , Nr. 2 Durchführung spezieller geophysikalischer Analogieexperimente und ihre Deutung von Horst Hänsel und Hans-Joachim Wilke (1969) , Nr. 3 Zur Einwirkung der Stativelastizität auf Amplituden und Phasen von Schwerependeln von Claus Elstner (1969)
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  • 49
    Call number: MR 17.91138
    Type of Medium: Monograph available for loan
    Pages: [167 S.]
    Language: English
    Note: 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.) , 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.)
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  • 50
    Call number: MOP 40553 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 176 Seiten
    Language: English
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  • 51
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-271
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Previous work. - Conduct of the research. - Fundamental properties of snow. - Derived properties of snow. - Environmental effects. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: One of the great deficiencies in snow science is the lack of an analytical framework for much of the snow cycle. Snow research to date has largely consisted of measuring index properties of snow, such as bulk density and snow strength, and correlating them. This is useful, particularly for engineering purposes, but it does not grapple with the basic problem of what fundamental properties of snow determine the magnitude of the index properties and how these properties respond to environmental conditions. This study was an attempt to measure, quantitatively, the fundamental properties of grain size, shape, and fabric (relationship between grains) and relate these to the index or derived properties of bulk density, shear and tensile strength, permeability for air, and the dielectric static permittivity and loss tangent. Despite numerous difficulties in defining fabric and quantifying it, it was possible to show that: 1) snow strength is a function of bond area with a relationship in the low density range that is described by: [Sigma]f = [Sigma]i exp - (0.14nf) where [Sigma]f is failure strength, [Sigma]i is the final strength of ice, and nf is the porosity on the failure surface; and 2) the rate of densification of low density snow can be explained in part by high stress concentrations (on the order of 10^7 dynes /cm^2) at intergranular contacts and by such factors as riming on crystals. The effect of the environmental factors of time, temperature, and gravitational stress is difficult to study in situ because they are not independent variables. However, it appears that their study is simplified when we study the fundamental properties of snow as opposed to index properties.
    Type of Medium: Series available for loan
    Pages: v, 70 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 271
    Language: English
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  • 52
    Series available for loan
    Series available for loan
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Description / Table of Contents: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Type of Medium: Series available for loan
    Pages: IV, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    Language: English
    Note: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
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  • 53
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-264
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Physical properties of ice fog. - Mie scattering computations. - Results. - Literature cited.
    Description / Table of Contents: Ice-fog crystals consisting of many spherical particles, and some hexagonal plates and columns, were observed at ambient temperatures of about -40°C in the Fairbanks, Alaska area during mid-winter. The concentrations and the size distributions of the ice-fog crystals were measured. The attenuation and backscattering of infrared radiation by ice-fog crystals were computed for optical wavelengths of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My] using the Mie theory. The minimum attenuation coefficients and backscattering functions of ice fog were found to be at 9.7[My] wavelength in the observed wavelengths. Optical attenuation coefficients and volume backscattering functions of water fogs were also computed using the Mie theory. The minimum attenuation coefficients and backscattering functions of water fog were found to be at 10.9[My] wavelength in the region of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My]. Both the attenuation coefficients and backscattering functions of ice fog are within the same order of magnitude as water fog for equivalent fog concentrations and wavelengths.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 264
    Language: English
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  • 54
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-263
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical background. - Experimental apparatus and procedures. - Results and discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: The transition in the mode of heat transfer from conduction to convection in a layer of water formed continuously by melting ice from below has been determined experimentally. This was accomplished by locating the inflection point on the curve relating the water-ice interface (or melting front) and time. Thus, the critical Rayleigh number, Rac, at which convective heat transfer started can be correlated empirically as a function of warm plate temperature, Ts, by Rac= 14,200 exp(-6.64 x 10^-2 Ts). This relation is valid for Ts varying from 7.72 to 25.50°C. The initial ice temperature T0 was varied from -4.8 to -22.00°C. The effect of T0 was found to be insignificant. Homogeneous, bubble-free ice was prepared and used in all the experiments.
    Type of Medium: Series available for loan
    Pages: iv, 12 Seiten , Illustrations
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 263
    Language: English
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  • 55
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
    Language: English
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  • 56
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    Language: English
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  • 57
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-269
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - List of symbols. - Introduction. - Structure of ice and ice sheets. - Ice as a mineral. - Lake and sea ice. - Chemistry and phase relations. - Dislocations,cracks,and stress concentrators. - Direct observation of dislocations. - Crackformation. - Stress concentration. - Theoretical considerations. - Experimental results. - Compressive strength. - Indentation failure. - Tensile strength. - Flexural strength. - Shear strength. - Impact strength. - Scale effects. - Strength deterioration in the spring. - Recommended research. - Summary. - Selected bibliography. - Abstract.
    Description / Table of Contents: The increased activity in cold regions has made a thorough understanding of fracture in lake and sea ice quite desirable, inasmuch as this information has application to a number of problems of geophysical as well as engineering importance. This survey starts with a discussion of the structure of ice I and the macro- and microstructure of sea and lake ice as well as their chemistry and phase relations. Recent work on the direct observation of dislocations as well as the formation of cracks in ice is summarized. Formal ice-brine-air models for analyzing variations in ice strength are also reviewed. The results of the different types of tests are discussed and cornpared (compressive, indentation, direct and ring-tension, small beam flexure and in situ cantilevers and simple beams, shear, and impact). Scale effects are considered as well as the rapid strength deterioration experienced by ice sheets in the spring. Finally, a number of recommendations are made concerning future research in this field.
    Type of Medium: Series available for loan
    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 269
    Language: English
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  • 58
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-266
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Review of dielectric properties of soils and rocks. - Methods and measurements. - Introduction. - Dispersion. - Experimental procedures. - Introduction. - Apparatus. - Correction for stray fields. - Material. - Results. - The dielectric properties of Na-montmorillonite suspensions as a function of concentration. - The dielectric properties of K-montmorillonite water suspension. - Conclusions. - Outlook. - Literature cited.
    Description / Table of Contents: The dielectric properties of Na- and K- montmorillonite suspensions with concentrations varying from 2.5% to 0.10% by weight were measured at 25°C in the frequency range of 50 Hz to 20 kHz. Effects of electrode polarization were minimized by using the same stainless steel electrodes at different interelectrode distances and a correction was applied to compensate for stray fields. This investigation establishes the fact that the high dielectric constants of clay suspensions at audio frequencies are real and not the result of electrode polarization. The polarization that determines the dispersion is an interfacial phenomenon between the ionic atmosphere and the negatively charged clay particle. The results of this study show that clay suspensions have the same dispersion as soil samples, indicating the probability that the dispersion of wet soils in the frequency range from 50 Hz to 20 kHz is similar for most soils. The actual value of the dielectric constant, however, cannot yet be predicted.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 266
    Language: English
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  • 59
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-245
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Snow crystals in Greenland. - Microspherules. - Microspherules in snow and ice-fog crystals. - Concentration and radii of spherules. - Discussion and conclusions. - Literature cited.
    Description / Table of Contents: Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash were studied with an electron microscope using the electron diffraction method. The central part of the residues of 1004 specimens of natural snow crystals from Greenland, the United States, and Japan were examined; 14 spherules 0.1 to 1.5? in radius were found among them. The residues of 658 artificial ice-fog crystals formed from water vapor in flue gases of coal-burning electric power plants at Fairbanks, Alaska, were also examined; nine spherules were found. Spherules similar to those found in ice-fog residues were found in furnace-produced fly ash fallout at Fairbanks, Alaska. Electron and optical microscope examination of spherules found in Greenland snow reveals a size distribution of the form dN/d(log r) = Cr-ß where ß approximately 3. The properties of spherules and the mean mass of snow crystals from Greenland are described. The electron microscope study indicated that less than 0.7% of the 1004 snow crystals contained spherules of possible extraterrestrial origin, and that snow crystals are formed mainly on clay mineral particles by heterogeneous nucleation.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seite , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 245
    Language: English
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  • 60
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    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-267
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Regional variations in density. - Monthly increase in density. - Nomograph to estimate average snow-cover density. - Test and application of the nomograph. - Discussion. - Literature cited. - Appendix A: Observed, weighted snow-cover densities for stations in Table 1.
    Description / Table of Contents: Analysis of snow-cover observations made during November - March at 27 stations in Alaska, Canada and the northern United States for a 2 to 11 year period showed that the average snow density can be classified in four general categories: Category 1 (density 0.20 to 0.23 g/cm^3 ), inland stations reporting light winds; Category 2 (0.24 to 0.27 g/cm^3), stations reporting moderate winds; Category 3 (0.28 to 0.30 g/cm^3), inland and coastal locations with stronger winds; Category 4 (0.32 to 0.36 g/cm^3), cold and windy stations of the Arctic. Skewness coefficients computed for each station showed bias toward lower densities for cat. 1 and 2, and bias toward higher densities for cat. 3 and 4. A nomograph in which the average winter air temperature and wind speed are the independent variables makes it possible to estimate the average snow-cover density for any location in the Arctic, subarctic and North Temperate Zones. A comparison between observed and estimated densities for ten other test stations yielded a correlation coefficient of 0.91 with a standard error of estimate of 0.016 g/cm^3. An average snow density map of North America was drawn and the continent was divided into areas based on the four categories.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 267
    Language: English
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  • 61
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
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  • 62
    facet.materialart.
    Unknown
    Delft ; 1.1969-76.2010
    Call number: S 90.0083
    ISSN: 0165-1706
    Language: English
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  • 63
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    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-259
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 259
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Previous work. - Study area. - Field procedures. - Results and discussion. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: A modern ice-push ridge on the northwest shore of Gardner Lake in southeastern Connecticut is 0.6 - 1.2 m high and 1.2 - 3.1 m wide. In February and March 1967, the positions of survey stakes placed on the lake ice were measured periodically. During the same period, air and ice temperature and solar radiation intensity were also recorded. Analysis of the data supports the hypothesis that thermal expansion of the lake ice rather than wind action, was the principal cause of ice push. An ice temperature change of approximately 1°C/hr increase for 6 hr was sufficient to induce ice thrust. In a 30-day period, the average net shoreward movement of the surveyed area of the ice surface was 1.0 m. During the 1966-67 winter, approximately 14 m^3 of beach material was reworked and deposited, forming a discontinuous ice-push ridge along 260 m of shoreline.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 259
    Language: English
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  • 64
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-256
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 256
    Description / Table of Contents: The flow of a compressible fluid through a deep layer of a porous medium with non-uniform permeability was analyzed. The volumetric behavior of the fluid was described first by the perfect gas law, then by the van der Waal's equation of state. Darcy's law was assumed to be valid. For illustration, the model of air flowing through a deep bed of naturally compacted snow was used to carry out numerical computation. The permeability of snow was considered as a function of depth. The nonlinear partial differential equation obtained by combining the continuity equation with Darcy's law was solved by finite difference technique. A time dependent exponential decay boundary condition was used which included the step-rise constant boundary condition as a limiting case. Pressure distributions in the porous medium calculated from the assumption of ideal gas and van der Waal's gas were compared. The data were presented in dimensionless variables.
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    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 256
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Computation and results. - Conclusions. - Literature cited.
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  • 65
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-254
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Description of the anemometer. - Temperature effects and their compensation. - Input-output relations. - Vibration isolation and compensation. - Wind tunnel tests. - Conclusions.
    Description / Table of Contents: A triaxial semiconductor strain-gage anemometer measuring wind velocities in three directions and thereby also determining the direction of the wind was designed and subjected to many crucial tests under various conditions. It was found that the measurements were affected by temperature and vibrations. Temperature compensation in two directions was made and wind tunnel tests on an almost vibration-free platform were performed. The results show that this type of instrument can be successfully used to measure large-scale turbulences. Throughout this report, emphasis is placed on the compensation necessary for temperature and vibration effects and the determination of input-output relationships. It is concluded that it is possible to design a practical triaxial strain-gage anemometer with high-frequency response and high sensitivity and to measure wind velocities accurately with this type of instrument when temperature and vibration compensations are properly made.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 254
    Language: English
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  • 66
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-252
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Discussion. - Conclusion. - Literature cited.
    Description / Table of Contents: A diffusion equation is obtained that describes the mechanical dispersion of a dilute mixture of solid particles within an ice matrix that is undergoing deformation. It is shown that within the limits of time intervals and strain rates appropriate to the movement of glaciers and ice sheets the dispersal distance usually is no larger than a distance about one order of magnitude greater than the size of the particles themselves.
    Type of Medium: Series available for loan
    Pages: iv, 6 Seiten , Illistrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 252
    Language: English
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  • 67
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-277
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Nomenclature. - Introduction. - Basic equations. - Constitutive relations. - Elastic region. - Plastic region. - Stability of the differential equation. - Stability of the difference equation. - Literature cited.
    Description / Table of Contents: An analysis is made of the stability of difference approximation to one-dimensional shock wave propagation in elastic-plastic media. The necessary condition for stability is obtained.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 277
    Language: English
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  • 68
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 69
    Call number: SR 90.0001(1260-I,J)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung
    Series Statement: U.S. Geological Survey bulletin 1260-I,J
    Language: English
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  • 70
    Monograph available for loan
    Monograph available for loan
    Chicago : Rand McNally
    Call number: M 97.0183
    Type of Medium: Monograph available for loan
    Pages: XIII, 381 S.
    Classification:
    Tectonics
    Language: English
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  • 71
    Monograph available for loan
    Monograph available for loan
    New Brunswick [u.a.] : Rutgers Univ.
    Call number: AWI P8-08-0038
    Type of Medium: Monograph available for loan
    Pages: 126 S. : Ill.
    Edition: Final Report
    Language: English
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  • 72
    facet.materialart.
    Unknown
    New York : Geological Soc. of America
    Associated volumes
    Call number: 97.0498/1
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
    Pages: ix, 250 S.
    Classification:
    Regional Geology
    Language: English
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  • 73
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    New York : Geological Soc. of America
    Associated volumes
    Call number: 97.0498/3
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
    Pages: Part 1-3
    Classification:
    Regional Geology
    Language: English
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  • 74
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Academic Press
    Call number: MOP B 13421
    Type of Medium: Monograph available for loan
    Pages: IX, 234 S. : graph. Darst.
    Uniform Title: V vedeniye v Kolichestvennyy Ul'tramikroanaliz
    Language: English
    Location: MOP - must be ordered
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  • 75
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Transl.
    Call number: M 97.0501
    Type of Medium: Monograph available for loan
    Pages: X, 614 S.
    Uniform Title: Processy sovremennogo osadkoobrazovanija v Beringovom More
    Classification:
    Regional Geology
    Language: English
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  • 76
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/2 ; 10/G 5218/2/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
    Location: Upper compact magazine
    Location: Reading room
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  • 77
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/1 ; 10/G 5218/1 ; 10/M 93.0251A/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: XIV, 442 S.
    Language: English
    Location: Upper compact magazine
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  • 78
    Call number: M 93.0131
    Type of Medium: Monograph available for loan
    Pages: VII, 754 S.
    Uniform Title: Problemy geokhimii
    Language: English
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  • 79
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/2
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 80
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/3
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 81
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/4
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 82
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    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 93.0251/a
    In: Handbook of geochemistry
    Pages: XIV, 442 S.
    Language: English
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  • 83
    Journal available for loan
    Journal available for loan
    Associated volumes
    In: Contributions to Mineralogy and Petrology
    Type of Medium: Journal available for loan
    Pages: 747 S.
    Language: English
    Location: Lower compact magazine
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  • 84
    Monograph available for loan
    Monograph available for loan
    Tokyo : Inst.
    Call number: ZSP-403 ; MOP Per 272/A
    Type of Medium: Monograph available for loan
    ISSN: 0075-3343
    Parallel Title: 438297-3 14=33; 15=35; 16=37; 17=41; 19=46; 20=51 u.a. von ---〉oeJARE data reports
    Parallel Title: 1197205-1 45=1988 u.a. von ---〉oeHF field strength data measured at Syowa Station, Antarctica
    Parallel Title: 437667-5 15=1975; 17=1976; 19=1977; 20=1978; 22=1979; 26=1980; 27=1981 - 49=1991 von ---〉oeRiometer records of 30 MHz cosmic noise at Sy¯owa Station, Antarctica
    Language: English
    Location: MOP - must be ordered
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  • 85
    Monograph available for loan
    Monograph available for loan
    Toronto : Atmospheric Environment Service, Environment Canada
    Call number: MOP 42751 / Mitte
    Type of Medium: Monograph available for loan
    Pages: V, 60, 25 Seiten , Illustrationen
    Series Statement: Canadian meteorological memoirs 25
    Language: English
    Location: MOP - must be ordered
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  • 86
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41126 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 1
    Language: English
    Location: MOP - must be ordered
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  • 87
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41127 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 2
    Language: English
    Location: MOP - must be ordered
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  • 88
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-116
    In: Research report / Cold Regions Research and Engineering Laboratory, 116
    Description / Table of Contents: Abstract: Specimens of snow from the South Pole were tested to investigate air permeability K (cm/sec), ultimate compressive strength σc (g/cm^2 ) and dynamic Young's modulus E (g/cm^2 ) as a function of density. Anisotropy in a single layer of snow (snow between two summer crusts) was found in all three properties. Comparison with data for snow from Site II, Greenland, showed an empirical relation for both areas: σc = 10.42 x 10^-4 E for 0.43 g/cm^3 〈 ρ 〈 0.51 g/cm^3. σc = 5.68 x 10^-4 E for 8.63 x 10^3 g/cm^2 for 0.51 g/cm^3 〈 ρ 〈 0.90 g/cm^3. Air permeabilities are different for the two sites because of time and meteorological effects.
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 116
    Language: English
    Note: CONTENTS Preface Summary Introduction Preparing the snow specimens Air permeability Experimental procedure Results and discussion Viscoelastic properties Principle Experimental method Results and discussion Creep tests Unconfined compressive strength Experimental procedure Results and discussion General discussion Literature cited Appendix A: Test result
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  • 89
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-120
    In: Research report / Cold Regions Research and Engineering Laboratory, 120
    Description / Table of Contents: Abstract: The report is divided into four parts: Parts I and II cover investigations of the reliability of shear stress measurements in soils subjected to vibratory loads for biaxial and triaxial systems, respectively. Part I is a summary only (see USA CRREL Technical Report 90 for detailed treatment). Part III is a study of three-dimensional "principal" stress patterns produced in soil subjected to vibratory loads. Part IV is a theoretical analysis of some aspects of soil wave propagation in stratified soil. From the measurements of five shear stresses and one normal stress, the stress distribution of a triaxial system can be determined. In noncohesive soils triaxial stress fields due to vibratory loads can be determined by recording six independent stress components. Sinusoidal force excitation and impact excitation yield time-distance graphs which can be used to determine reflection and refraction techniques in stratified soils.
    Type of Medium: Series available for loan
    Pages: v, 52 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 120
    Language: English
    Note: CONTENTS Preface Summary Part I. Two-dimensional shear stress measurements Part II. Three-dimensional shear stress measurements Introduction Measurements Experimental results Evaluation Compatibility checks Comparison between shear stresses under static and dynamic loads Conclusions Part III. Three-dimensional normal stress measurements Introduction Experimental setup Results Analysis Conclusions Part IV. Soil wave propagation in stratified soil Introduttion Distance-time graphs Results Sinusoidal force excitation Refraction Impact force excitation Selected bibliography Appendix A. Equations for computing stress components in Part II Appendix B. Equations for computer program in Part III
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  • 90
    Call number: AWI Bio-99-0271
    In: Atlas of seeds and small fruits of Northwest-European plant species 〈Sweden, Norway, Denmark, East Fennoscandia and Iceland〉
    Type of Medium: Monograph available for loan
    Pages: 68 S.
    Language: English
    Note: Contents: Foreword. - Introduction. - Information concerning the Taxonomic Arrangement and the Origin of the Material Examined. - Notes on Keys and Descriptions. - Glossary. - List of Abbreviations. - Key to the Genera. - Cyperus. - Eriophorum. - Scirpus. - Blysmus. - Eleocharis. - Trichophorum. - Schoenus. - Cladium. - Rhynchospora. - Kobresia. - Carex. - References. - Index of Used Specimens. - Index of Species. - Explanation of Plates. - Plates 1—39. - Fold up Map of Simple Systematical Plane Shapes and Colour Chart.
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  • 91
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Translations
    Call number: MOP 35098
    Type of Medium: Monograph available for loan
    Pages: VI, 242 S. : graph. Darst.
    Uniform Title: Ob-ektivnyi analiz meteorologiceskich polej
    Language: English
    Location: MOP - must be ordered
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  • 92
    Call number: AWI E3-93-0322
    Type of Medium: Monograph available for loan
    Pages: 271 Seiten , Illustrationen , 21 cm
    Language: Russian , English
    Note: Contents: From the editor. - The sixth Soviet Antarctic Expedition (1960-1962). - The Pravda Coast. - Unloading the Ob at Mirny. - Operations of expedition parties. - Aerometeorological researches. - Sea and coastal ice researches. - Geophysical researches. - Operations of the aviation group. - Connection with Antarctic expeditions of other countries. - Brief summary of results of researches conducted by the sixth Soviet Antarctic Expedition. - The Seventh Soviet Antarctic Expedition (1961-1963). - Organization and tasks of the expedition. - Routes of expedition ships. - D/s Ob. - M/s Kooperatsia. - First flight: the Soviet Union - Antarctica. - Flight Moscow - Mirny. - Flights in Antarctica. - Home-coming. - The Pravda Coast. - Unloading the ships. - Operations of the expedition parties. - Traverses to the 100th km. - Brief summary of results of researches conducted by the Seventh Soviet Antarctic Expedition. - The Eighth Soviet Antarctic expedition (1962-1964). - Organization and tasks of the expedition. - Routes of expedition ships. - D/s Ob. - M/s Esthonia. - Mirny Observatory. - Tractor-sledge traverses of inland areas of Eastern Antarctica. - Sixth expedition traverses. - Auxiliary traverse along the route Mirny - Komsomolskaya - Mirny. - Transport traverse along the Mirny - Vostok route. - Scientific-research traverse along the route Komosomolskaya - Sovetskaya - Vostok - Komsomolskaya. - Eighth expedition traverse. - Operation of the Antarctic stations. - Vostok. - Komsomolskaya. - Novolazarevskaya. - Enderby Land. - Debarkation and unloading the "Ob". - Operation of expedition parties. - Molodezhnaya. - Atlas of the Antarctic. - International cooperation in the study of Antarctica. - Antarctic treaty. - Second consultative meeting concerning the Antarctic treaty. - Scientific Committee on Antarctic researches. - Abstract. - References. - Appendices. - 1. List of members of the Soviet Antarctic Expeditions. - 2. Main data of the Soviet Antarctic stations. - 3. Calendar of the expedition ships operations. - 4. Personnel of the Soviet Antarctic Expeditions of 1955-1965. - 5. Period of operations of the Soviet Antarctic Expeditions of 1955-1964. - 6. Recommendations of the First Consultative Meeting concerning the Antarctic Treaty. - 7. Recommendations of the Second Consultative Meeting concerning the Antarctic Treaty. , In kyrillischer Schrift , Mit englischer Zusammenfassung
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  • 93
    Monograph available for loan
    Monograph available for loan
    New York : Greystone Press
    Associated volumes
    Call number: M 95.0044/2
    In: The illustrated library of the world and its peoples
    Type of Medium: Monograph available for loan
    Pages: 216 S.
    Classification:
    Geography and Geomorphology
    Language: English
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  • 94
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Acad. Press
    Associated volumes
    Call number: 5/O 3210(10) ; 6193 ; 6584
    In: International geophysics series
    Type of Medium: Monograph available for loan
    Pages: XIV, 202 S. : Ill., graph. Darst.
    Series Statement: International geophysics series 10
    Language: English
    Location: Reading room
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  • 95
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-276
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Test site. - Test procedures. - Equipment. - Unconfined compression tests. - Ring tensile tests. - Test results. - Unconfined compression tests. - Ring tensile tests. - Discussion. - Literature cited. - Appendix A. Calculation of the effect of nonaxial loading of unconfined compression specimens. - Appendix B. Camp Century unconfined compressive strength data at -25C. - Appendix C. Camp Century ring-tensile strength data at -25C. - Appendix D. Unconfined compressive strength of Camp Century vertical snow samples 8.25 in. length, 3.0 in. diam at -25C. - Abstract.
    Description / Table of Contents: The unconfined compressive strengths [Sigma]c and the ring-tensile strengths [Sigma]T of snow and ice specimens from the Inclined Drift at Camp Century, Greenland, were determined. The specimen densities varied over essentially the complete natural density range of polar snow and ice (0.340 to 0.890 g/cm^3). The specimens were loaded rapidly to failure with times varying between 0.2 and 1.4 sec. During loading, head speeds varied between 5.1 and 23.6 cm/min, although during individual tests they were constant. Even the low density specimens failed in the brittle mode. Although a plot of [Sigma]T vs [Gamma] is linear, [Sigma]c vs [Gamma] is clearly nonlinear. This nonlinearity may result from either changes in the level of the internal stress concentrations associated with the voids in the snow or from changes in the ratio (bulk porosity/effective porosity of the failure surface) with density. Both tangent and secant moduli are linear functions of [Gamma]. There is no pronounced change in [Sigma]c with changes in strain rate. A significant increase in [Sigma]T, [Sigma]c and the modulus values was noted at bulk densities greater than 0.830 g/cm^3. This increase is presumably caused by the close-off of the air passages.
    Type of Medium: Series available for loan
    Pages: 35 Seiten , Illustrationen, graphische Darstellungen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 276
    Language: English
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  • 96
    Monograph available for loan
    Monograph available for loan
    Middlesex : Penguin Books
    Call number: M 97.0180
    Type of Medium: Monograph available for loan
    Pages: xii, 237 S.
    Edition: Revised ed.
    Classification:
    Geography and Geomorphology
    Language: English
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  • 97
    Monograph available for loan
    Monograph available for loan
    London : Heinemann
    Call number: M 97.0182
    Type of Medium: Monograph available for loan
    Pages: xi, 404 S.
    Classification:
    Geography and Geomorphology
    Language: English
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  • 98
    Monograph available for loan
    Monograph available for loan
    London : Arnold
    Call number: M 97.0181
    Type of Medium: Monograph available for loan
    Pages: ix, 342 S.
    Classification:
    Geography and Geomorphology
    Language: English
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  • 99
    Call number: ZSP-553-159,12
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 114 S., 38 Taf. : Ill., graph. Darst.
    Series Statement: Meddelelser om Grønland 159,12
    Language: English
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  • 100
    Monograph available for loan
    Monograph available for loan
    København : Lunos
    Associated volumes
    Call number: ZSP-553-170,3
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 26 S. : Ill., graph. Darst.
    Series Statement: Meddelelser om Grønland 170,3
    Language: English
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