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  • 2020-2022  (11,376)
  • 1990-1994  (1,292)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Zürich : Verl. der Fachvereine an den Schweizer. Hochschulen und Techniken
    Call number: AWI A5-05-0005
    Type of Medium: Monograph available for loan
    Pages: 123, [40] S. , Ill., graph. Darst., Kt
    Edition: 5., durchges. Aufl.
    ISBN: 3728118419
    Language: German
    Note: INHALTSVERZEICHNIS: Vorwort. - 1. Einleitung. - 1.1 Abgrenzung zwischen Wetter und Klima. - 1.2 Moderner Mensch und Wetter. - 2. Zusammensetzung und Aufbau der Atmosphäre. - 2.1 Zusammensetzung der Atmosphäre. - 2.2 Aufbau der Atmosphäre. - 2.2.1 Troposphäre. - 2.2.2 Stratosphäre. - 2.2.3 Mesosphäre. - 2.2.4 Thermosphäre. - 2.2.5 Exosphäre. - 2.2.6 Magnetosphäre. - 2.3 Einfluss der Land/Meer·Verteilung auf das Wetter. - 3. Meteorologische Messungen. - 3.1 Messung der Temperatur. - 3.1.1 Definition der Temperatur. - 3.1.2 Quecksilberthermometer. - 3.1.3 Andere Temperaturmessmethoden. - 3.1.4 Temperaturmessungen in der Meteorologie. - 3.1.5 Aufstellung der Temperatur-Messinstrumente. - 3.2 Messung der Feuchtigkeit. - 3.3 Messung des atmosphärischen Druckes. - 3.4 Messung des Windes. - 3.5 Messung des Niederschlages. - 3.6 Beobachtung der Wolken. - 3.7 Messung der Sonnenscheindauer. - 3.8 Messungen mit Radiosonden. - 4. Barometerformel. - 4.1 Barometerformel. - 4.2 Homogene Atmosphäre ρ = ρo = konst. - 4.3 Isotherme Atmosphäre T =konstant. - 4.4 Praktische Anwendung der Barometerformel. - 4.4.1 Druckreduktion auf Meeresniveau. - 4.4.2 Altimeter. - 4.5 Wetterkarten. - 5. Thennodynamik. - 5.1 Erster Hauptsatz der Wännelehre. - 5.1.1 Spezifische Wärme. - 5.2 Adiabatische Vorgänge dQ = 0. - 5.2.1 Potentielle Temperatur. - 5.2.2 Lapse-Rate bei adiabatischen Vorgängen in trockener Luft. - 5.2.3 Graphische Darstellung der adiabatischen Zustandsänderung. - 5.3 Feuchte Luft. - 5.4 Mischungsverhältnis w. - 5.5 Allgemeines über die Kondensation infolge Abkühlung. - 5.5.1 Isobare Abkühlung. - 5.5.2 Mischung von zwei Luftmassen. - 5.5.3 Abkühlung durch adiabatische Expansion. - 5.6 Zustandsänderungen von Wasser. - 5.7 Feuchtadiabatische Vorgänge. - 5.8 Pseudopotentielle Temperatur θe. - 5.9 Verdunstung. - 5.10 Stabilität der Atmosphäre. - 5.10.1 Stabilität unterhalb der Kondensationsbasis. - 5.10.2 Stabilität oberhalb der Kondensationsbasis. - 5.10.3 Wolkenbildung in instabiler Atmosphäre. - 6. Wolken und Niederschlag. - 6.1 Wolken. - 6.2 Niederschläge. - 6.2.1 Formen der Niederschläge. - 6.2.2 Theorie der Gewitterwolken. - 6.2.2.1 Niederschlagsbildung. - 6.3 Hagelbekämpfung. - 6.3.1 Hagelschäden. - 6.3.2 Grassversuche in der Magadinoebene und in Südrussland. - 7. Strahlung. - 7.1 Allgemeines. - 7.2 Allgemeine Gesetze der Strahlung. - 7.3 Streuung. - 7.3.1 Rayleigh-Streuung. - 7.3.2 Mie-Streuung. - 7.4 Intensität der Sonnenstrahlung. - 7.5 Energiegewinn des Systems Erde-Atmosphäre aus der Sonnenstrahlung. - 7.5.1 Die Strahlungsbilanz nach London. - 7.5.2 Abhängigkeit der Strahlungsbilanz von der geographischen Breite. - 7.5.3 Messung der Strahlungsbilanz mit Hilfe von Satelliten. - 8. Windgesetze. - 8.1 Allgemeine Bewegungsgleichung. - 8.2 Druckkraft. - 8.3 Strömungsgleichungen auf der rotierenden Erde. - 8.4 Geostrophischer Wind. - 8.5 Ablenkung des Windes in Bodennähe. - 8.6 Änderung des geostrophischen Windes mit der Höhe. - 9. Allgemeine Zirkulation. - 9.1 Allgemeine Zirkulation. - 9.2 Folgerungen über die allgemeine Zirkulation. - 9.3 Weltweite Klimaverteilung als Funktion der allgemeinen Zirkulation. - 10. Grosswetterlagen in Mitteleuropa. - 10.1 Grundelemente,der synoptischen Meteorologie. - 10.1.1 Druckgebiete. - 10.1.2 Die Luftmassen. - 10.1.3 Fronten. - 10.2 Hauptwetterlagen. - 10.2.1 Hochdrucklage über Mitteleuropa. - 10.2.1.1 Allgemeine Übersicht. - 10.2.1.2 Sommerliches Hochdruckwetter. - 10.2.1.3 Winterliches Hochdruckwetter. - 10.2.2 Tiefdrucklage über Mitteleuropa. - 10.2.2.1 Allgemeine Übersicht. - 10.2.2.2 Winterliche Kaltlufttropfen. - 10.2.2.3 Sommerliche Kaltlufttropfen. - 10.2.3 Nordostlage. - 10.2.3.1 Allgemeine Übersicht. - 10.2.3.2 Winterliche Nordostlage. - 10.2.4 Südlage. - 10.2.4.1 Allgemeine Übersicht. - 10.2.4.2 Entstehung des Föhns. - 10.2.4.3 Föhnlage. - 10.2.5 Westlage. - 10.2.5.1 Allgemeine Übersicht. - 10.2.5.2 Westwindwetter. - 10.2.6 Nordlage. - 10.2.6.1 Allgemeine Übersicht. - 10.2.6.2 Spätfrost bei Nordlage. - 10.2.7 Nordwestlage. - 10.2.7.1 Allgemeine Übersicht. - 10.2.7.2 Lawinensituation bei Nordwestlage. - 10.3 Witterungsverlauf vom 20.12.1970 bis zum 3.2.1971. - 11. Wetterprognose und gobale Atmosphärenforschung. - 11.1 Wetterprognose. - 11.1.1 Einteilung von Wetterprognosen. - 11.1.2 Methode für Wettervorhersage. - 11.1.3 Die Langfristprognose. - 11.2 Globale Atmosphärenforschung.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/12
    In: CRREL Report, 76-12
    Description / Table of Contents: The heat transfer processes associated with melting and refreezing a drill hole 500 m in depth and 0.150 m in initial radius through an ice shelf were approximately analyzed. The results were expressed in graphical form showing the time available for experimentation under the hole as a function of heating duration and heating strength. It was found that the refreezing of the drill hole had a much slower rate than the melting of the hole.
    Type of Medium: Series available for loan
    Pages: vi, 15 Seiten , Illustrationen
    Series Statement: CRREL Report 76-12
    Language: English
    Note: Contents Abstract Preface Summary Nomenclature Introduction Analysis Melting period Freezing period Calculation Conclusion Literature cited Appendix A: Justification of using eq 8 for the calculation of heat transfer coefficient h
    Location: AWI Archive
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  • 3
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/32
    In: CRREL Report, 77-32
    Description / Table of Contents: An experimental study of forced convective heat transfer over a vertical melting plate has been conducted. This study covers water velocities ranging from 1.7 to 9.8 mm/s and bulk water temperatures from 1.11 to 7.50 C. The experimental results are correlated in terms of Nusselt, Prandtl and Reynolds numbers with a moderate correlation coefficient of 0.843. The results are expected to be useful in predicting the heat transfer characteristics of a much larger prototype ice-water heat sink.
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 77-32
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Summary Introduction Problem General review of the subject Experimental apparatus General considerations Water reservoir Test chamber assembly Pumping system Electrical control system Experimental procedure Experimental results Discussion and comparison of results Conclusions Literature cited
    Location: AWI Archive
    Branch Library: AWI Library
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  • 4
    Call number: SR 90.0066(43)
    In: Geologisches Jahrbuch
    Type of Medium: Series available for loan
    Pages: 85 S. + 1 Kt.-Beil.
    Series Statement: Geologisches Jahrbuch : Reihe A 43
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Call number: SR 90.1043(111)
    In: Illinois petroleum
    Type of Medium: Series available for loan
    Pages: 10 S.
    Series Statement: Illinois petroleum 111
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-95
    In: Research report / Cold Regions Research and Engineering Laboratory, 95
    Description / Table of Contents: Summary: An investigation was conducted at Camp Century, Greenland, to study the feasibility of using air wells to cool undersnow structures in the arctic during the summer months. From results obtained during the summers of 1959,and 1960 and late November, 1960, it was found that the air well is a practical and effective means of providing a -20°C air supply at volumetric flow rates of 1200 to 1700 ft^3/min. The extent and rate of warming of the snow beneath the trench floor by heat exchange between the air and the snow foundation was found to depend upon trench air temperature, fan capacity, fan arrangement, and casing length. For example, in a well cased to a depth of 17. 5 ft and equipped with a 5 hp fan drawing in air at a rate of 1700 ft^3/min, the maximum warming was found to be 12.5°C during a 42-day period. Snow temperature differences of about 7°C were found between similar trenches with and without a fan installation. The minimum permissible distance between two adjacent fans to eliminate, overlap in warming up the snow foundation is approximately 80 ft.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 95
    Language: English
    Note: CONTENTS Preface Summary Theoretical background Test method and equipment Test operations Effectiveness of the air well Estimation of fan capacity Natural cooling in winter Change of trench foundation temperature Trench wall warm-up Conclusions and recommendations
    Location: AWI Archive
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-103
    In: Research report / Cold Regions Research and Engineering Laboratory, 103
    Description / Table of Contents: Summary: The effect of air flow on the thermal conductivity of snow was investigated. Steady-state temperature measurements were made along the edge and axis of a cylindrical bed of snow to determine the effective axial thermal conductivity of snow. Unconsolidated snow samples were used, with densities ranging from 0.376 to 0.472 g/cm^3 and corresponding snow particle sizes of 0.065 to 0.219 cm nominal diameter; the mass flow rates employed ranged from approximately 10-40 x 10^-4g/cm^2 sec. Snow density and sample size apparently have opposite effects on the effective thermal conductivity because of the flow of fluid in snow. The test apparatus is described in detail and is illustrated. The results of the experiments are tabulated, and a least square equation is given which represents the results well.
    Type of Medium: Series available for loan
    Pages: iv, 14, A2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 103
    Language: English
    Note: CONTENTS Preface Summary Introduction Theory Apparatus and experimental procedure Results and discussion References Appendix A: Sample calculations of a and ke
    Location: AWI Archive
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  • 8
    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-202-335
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Ňomenclature. - Introduction. - Experimental apparatus and procedure. - Testspecimens. - Bubble frequency and velocity. - Analysis of experimental results. - Discussion. - Summary. - Literature cited.
    Description / Table of Contents: An experimental study of the heat transfer characteristics of a bubble-driven water jet on an ice surface was conducted. Two Lucite columns, one 1.829 m high and 0.286 m in diameter and the other 1.219 m high and 0.140 m in diameter were used. Water levels were maintained at 0.762 and 1.524 m in the large column and 0.840 m in the small column. Hypodermic needles with openings of 0.152, 0.406 and 0.838 mm were used for bubble formation. The air flow rate was varied from 7.39 X 10^-8 to 9.91 X I0^-7 m^3/s. In all, 171 experimental runs were conducted. The results can be correlated by Nu = 0.1735 (Rei)^0.848 with a correlation coefficient of 0.84, in which Nu is defined in terms of average heat transfer coefficient h, sample diameter Ds, and thermal conductivity of water kw. Rei is defined in terms of diameter of the impinging water jet at the ice surface, Di, the centerline arrival water velocity vc and the kinematic viscosity of water uw.
    Type of Medium: Series available for loan
    Pages: vi, 16 S. : graph. Darst.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 335
    Branch Library: AWI Library
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  • 9
    Monograph available for loan
    Monograph available for loan
    Peking
    Call number: G 7295
    Type of Medium: Monograph available for loan
    Pages: 13 S. : Ill.
    Edition: Sonderdr
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 10
    Call number: SR 90.0001(2050)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 22 S.
    Series Statement: U.S. Geological Survey bulletin 2050
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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