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  • Books  (608)
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  • 1
    Call number: AWI E2-11-0018 ; AWI PY-1955-13
    Type of Medium: Monograph available for loan
    Pages: VII, 630 S. : Ill., Kt. , 2 Kt.
    Language: English
    Note: Kt. u.d.T.: Part of Franz Josef Archipelago surveyed by the Ziegler Polar Expedition 1903-4-5 〈1 : 600.000〉 ; Map of Franz Josef Archipelago compiled from surveys of the Ziegler Polar Expeditions 1901--02, 1903-5, and from information published by Payer (1872-74), Leigh Smith (1880-81), Jackson (1894-97), Nansen (1895-96), Wellman (1898-99), the Duke of the Abruzzi (1899-1900) 〈1 : 750.000〉 , Contents: Introduction by Anthony Fiala. - Section A - Magnetic Observations and Reductions. - Section B - Notes and Sketches of the Auroræ Borealis. - Section C - Meteorological Observations and Compilations. - Section D - Tidal Observations and Reductions. - Section E - Astronomic Observations and Reductions. - Section F - Map construction and survey work
    Location: AWI Reading room
    Location: AWI Archive
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 2
    Monograph non-lending collection
    Monograph non-lending collection
    Berlin : Prometter
    Call number: AWI G8-90-0187
    Type of Medium: Monograph non-lending collection
    Pages: 116 S. : graph. Darst.
    Note: Zugl.: Berlin, Univ., Diss., 1887 , Inhaltsübersicht: Einleitung. - Ältere Ansichten über das Geoid. - A. Über die gegenwärtigen Deformationen der Erdgestalt und die Methoden zu ihrer Bestimmung. - Verwendung des Barometers. - B. Die Wirkung von Massenumlagerungen auf die Erdgestalt im allgemeinen Einfluß der Gebirgsbildung. - Fluß-Sedimente. - Vulkane. - Wirkung des Eises. - Sichtung der Eismassen. - C. Über die Geoiddeformationen der Eiszeit. - I. Allgemeiner Teil. - Die Wirkungsart von Inlandeismassen. - Die Elemente der Rechnung. - Die Formeln und ihre Anwendbarkeit. - Die Rechnung und die Resultate in tabellarischer Form. - Graphische Darstellung in Kurven. - Behinderung der freien Schwankungen durch Festlandmassen. - Wirkung eines Attraktionscentrums auf eine gleichmäßig mit Wasser bedeckte Kugel. - Die Wirkung der Wasserabsorbtion. - Erscheinungen beim Abschmelzen der Gletscher. - II. Anwendungen der Theorie. - A. Einfluß der Horizontalverschiebung auf die Thätigkeit der Flüsse. - 1. Entstehung von Seen. - 2. Über Stromverlegungen in Norddeutschland. - B. Schwankungen des Meeresspiegels. - 1. Nordamerika und Grönland.- Der Agassiz-See. - Der kanadische Binnensee und die atlantische Küste der Vereinigten Staaten. - Exkurs über eine Stromverlegung in Connecticut. - Fundy-Bay und Küste von Labrador. - Hudsons-Bay. - Die Westküste Grönlands. - 2. Die Küste Norwegens. - 3. Kurzer Überblick über andere Erdräume. - Schottland und Irland. - Südamerika. - Niedriger Wasserstand an der Küste Nordamerikas. - Polynesien. - Zusammenfassende Übersicht und andere Theorieen. - Die Geoisothermen zur Eiszeit.
    Location: AWI Archive
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  • 3
    Series available for loan
    Series available for loan
    Leipzig : Deutscher Verlag für Grundstoffindustrie
    Associated volumes
    Call number: SR 99.0015(409) ; ZSP-292-409
    In: Freiberger Forschungshefte, 409
    Type of Medium: Series available for loan
    Pages: 54 Seiten , Illustrationen
    Edition: 1. Auflage
    ISBN: 3-342-00920-9
    ISSN: 0071-9409
    Series Statement: Freiberger Forschungshefte : C 409 : Geowissenschaften - Geologie
    Language: German
    Note: Inhaltsverzeichnis Annotation (Annotation, Annotacija) 1. Einführung 1.1. Politische Grundlagen 1.2. Rohstoffspekulationen 2. Grundzüge der Tektonik und Mineragenie der Antarktis 2.1. Geotektonische Epochen 2.2. Tektonisch-minerogenetische Rayonierung 3. Vorkommen fester mineralischer Rohstoffe 3.1. Metallische Rohstoffe 3.1.1. Schwarzmetalle 3.1.1.1. Eisen 3.1.1.2. Mangan 3.1.1.3. Chrom, Nickel, Kobalt, Vanadium, Titan 3.1.1.4. Molybdän, Wolfram 3.1.2. Buntmetalle 3.1.2.1. Kupfer 3.1.2.2. Blei, Zink 3.1.2.3. Zinn 3.1.3. Edelmetalle (Silber, Gold, Platin) 3.1.4. Sonstige Metalle 3.2. Nichtmetallische Rohstoffe 3.2.1. Edel- und Schmucksteine 3.2.2. Glimmer 3.2.3. Feuerfestminerale 3.2.4. Phosphat 3.2.5. Fluorit, Baryt 3.2.6. Graphit. 3.2.7. Schwefel 4. Kohlenvorkommen 5. Kohlenwasserstoff-Vorkommen 6. Geothermische Energie 7. Süßwasser(Eis)-Vorräte 8. Schlußfolgerungen 9. Danksagung . 10. Zusammenfassung (Summary, Rezjume) Literaturverzeichnis Tabellen 1 bis 8
    Location: Lower compact magazine
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    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 4
    Call number: SR 99.0015(335) ; ZSP-292-335
    In: Freiberger Forschungshefte, 335
    Type of Medium: Series available for loan
    Pages: 145 Seiten , Illustrationen
    Edition: 1. Auflage
    Series Statement: Freiberger Forschungshefte : C 335 : Geowissenschaften
    Language: German
    Note: Enthält auch: Methode und Anleitung zur weitgehend objektiven Ermittlung der Varietäten humifizierter Xylite unserer Weichbraunkohlen : Vortrag zum Berg- u. Hüttenmännischen Tag 1976 in Freiberg / von Gerhard Roselt
    Location: Lower compact magazine
    Location: AWI Archive
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 5
    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-202-244
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Summer temperature data. - Station network and history. - Parameters for data reduction. - Analysis of summer temperatures. - Temperature trends. - Summer temperatures in the highlands. - Lapse rates for summer temperatures. - Spatial variation of summer temperatures. - Summary. - Literature cited. - Appendix A. - Appendix B. - Appendix C. - Abstract.
    Description / Table of Contents: Annual degree-day summations over bases of 43°F and 50°F in 15-day periods from May through August are given for the period of record for five interior Alaska climatic stations. Average temperature and precipitation data are included. Patterns of summer temperature in interior Alaska are analyzed in terms of historical, elevational and areal differences. Since 1900, summer temperatures show little long-term change but significant short-term changes. In contrast, winter temperatures show considerable fluctuations, which are reflected in mean annual temperatures to a much greater degree than are summer temperature fluctuations. Average summer lapse rates for the 1600 to 3300 and 3300 to 6600-ft levels were 3.4 and 3.7°F/1000 ft, respectively, based on timberline temperature observations and on upper air data from Fairbanks. Correlation analysis of daily and monthly average July temperatures indicates areas of uniformity with respect to temperature variation. This provides information on lowland climatic stations that are representative of highland locations, especially the Yukon-Tanana Uplands
    Type of Medium: Series available for loan
    Pages: iv, 37 Seiten , Illustrationen, Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 244
    Language: English
    Location: AWI Archive
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  • 6
    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-202-259
    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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  • 7
    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-202-256
    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.
    Type of Medium: Series available for loan
    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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  • 8
    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-202-255
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Previous work on unsteady rectilinear motion of a sphere. - Experiments with a circular path. - Conclusion. - Literature cited. - Appendix A: Comparisons of the measured and calculated forces.
    Description / Table of Contents: Forces on a sphere moving unsteadily along a circular path in a viscous fluid are measured, and it is found that within the experimental range the formula valid for rectilinear motion has to be modified to account for the curvature of the path.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 255
    Language: English
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  • 9
    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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    Branch Library: AWI Library
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  • 10
    Call number: ZSP-202-347
    In: Research report / Cold Regions Research and Engineering Laboratory, 347
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental. - Results and discussion. - Applications. - Literature cited.
    Description / Table of Contents: Chemical analysis of century-old ice from continuous 5 to 7 year intervals of three ice cores from south and central Greenland (Dye 3, Milcent and Crete) show maximum concentrations of Na, Mg,Ca, K, and Al during early spring and minimum concentrations during late summer and early fall. Peak spring values are as much as 10 times greater than fall values. Because of the large seasonal chemical variations, samples used for depth-age or annual deposition rate studies must represent accumulation from exactly one year or whole multiples of a year. The seasonal chemical variations seem promising as a new method of defining annual layers and thus dating old ice cores.
    Type of Medium: Series available for loan
    Pages: iii, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 347
    Language: English
    Location: AWI Archive
    Branch Library: AWI Library
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