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  • 1
    Call number: A1 12 ; MOP A1 44957 ; MOP A1 44957 (2. Ex.)
    In: Atlas climático de América del Sur
    Type of Medium: Monograph available for loan
    Pages: 28 Kt.
    Classification:
    E.6.
    Language: English , Spanish , French , Portuguese
    Note: In span., engl., franz. und port. Sprache
    Location: Upper compact magazine
    Location: MOP - must be ordered
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik
    Associated volumes
    Call number: MOP Per 581(3/40) ; ZSP-319/C-40 ; ZSP-319/C-40(2.Ex.)
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Heft 40
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 40
    Language: German , Russian
    Note: Inhaltsverzeichnis Summary, Rezjume 1. Einleitung 2. Das Bewegungsverhalten von Eismassen, seine Untersuchung und Modellierung 2.1. Zum Modellbegriff 2.2. Typische Eismassen und ihr Bewegungsverhalten 2.2.1. Zur Theorie der Eisbewegung 2.2.2. Gletscher 2.2.3. Schelfeis und Eiskappe 2.3. Die Ermittlung von Eisbewegungen durch geodätische Verfahren 2.3.1. Die Vorplanung der Messungen 2.3.2. Die Durchführung der Messungen 2.3.3. Reduktion der Beobachtungen 2.3.4. Berechnung der Eisbewegungen 2.4. Das trendbehaftete vektorielle Zufallsfeld - Modell zur Beschreibung des Geschwindigkeitsfeldes einer Eismasse - in der Theorie stochastischer Prozesse 2.4.1. Definition des Vektorfeldes 2.4.2. Das Geschwindigkeitsfeld einer Eismasse - trendbehaftetes vektorielles Zufallsfeld 2.4.3. Definition eines vektoriellen Zufallsfeldes 2.4.4. Wahrscheinlichkeitsdichte und Verteilungsfunktion 2.4.5. Die Momente und die Korrelationsfunktionen 2.4.6. Vektorielle Zufallsfelder mit Hormalverteilungsgesetz 2.4.7. Homogene und isotrope vektorielle Zufallsfelder 2.4.8. Das Ergodenproblem 3. Das Konzept der Kollokation und seine Anwendung auf die Bearbeitung von Eisbewegungsmessungen 3.1. Zur Theorie der Kollokation 3.1.1. Das Kollokationsmodell von Moritz [40] 3.1.2. Nichtlineare Prädiktion nach Grafarend [12] 3.1.3. Kollokation von Vektorgrößen 3.2. Analyse und Bearbeitung des Datenmaterials 3.2.1. Die Trendbestimmung 3.2.2. Die Analyse des Zufallsfeldes 3.3. Das Kollokationsmodell bei der Bearbeitung von Eisbewegungsmessungen 3.3.1. Zuordnung und Interpretation der Größen 3.3.2. Zur zeitlichen Variation des Geschwindigkeitsfeldes einer Eismasse 3.3.3. Kollokation mit den ursprünglichen reduzierten Beobachtungen 4. Praktische Untersuchungen 4.1. Geschwindigkeitsquerprofile des Fedtschenko-Gletschers (Pamir) 4.2. Geschwindigkeitslängsprofil des Kongsvegen-Gletschers (Spitzbergen) 4.3. Geschwindigkeitslängsprofil des Hays-Gletschers (Antarktika) 4.4. Geschwindigkeitsquerprofil des Ross-Schelfeises (Antarktika) 4.5. Vergleich mit früheren Untersuchungen zur Abschätzung von Geschwindigkeitskorrelationen natürlicher Eismassen 5. Zusammenfassung 6. Literaturverzeichnis , Zusammenfassung in englischer und russischer Sprache
    Location: MOP - must be ordered
    Location: AWI Archive
    Location: AWI Archive
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  • 3
    Monograph available for loan
    Monograph available for loan
    Orsay, France : Les editions de physique
    Call number: M 94.0516
    Type of Medium: Monograph available for loan
    Pages: VIII, 705 S.
    ISBN: 2902731167
    Classification:
    C.3.8.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 94.0014/2
    In: Der Chemielaborant
    Type of Medium: Monograph available for loan
    Pages: 256 S.
    ISBN: 3441910540
    Classification:
    C.4.1.
    Language: German
    Location: Upper compact magazine
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  • 5
    Monograph available for loan
    Monograph available for loan
    New York : Academic Press
    Associated volumes
    Call number: AWI A6-94-0044
    In: Advances in geophysics, Volume 21
    Type of Medium: Monograph available for loan
    Pages: Seiten 87-230 , Illustrationen
    Series Statement: Advances in geophysics Volume 21
    Language: English
    Note: Contents 1. An Introduction to Mountain Effects 2. The Flow over Hills and the Generation of Mountain Waves 2.1 Buoyancy Forces 2.2 The Theory of Two- Dimensional Mountain Waves 2.3 Observations of Mountain Waves 2.4 The Three-Dimensional Flow over Isolated Hills 2.5 Large-Amplitude Mountains and Blocking 2.6 The Observed Barrier Effect of Mountains-The Fohn and Bora 2. 7 The Influence of the Boundary Layer on Mountain Flows 2.8 Slope Winds and Mountain and Valley Winds 3. The Flow near Mesoscale and Synoptic-Scale Mountains 3.1 Quasi-geostrophic Flow over a Mountain 3.2 The Effect of Inertia on the Flow over Mesoscale Mountains 3.3 Theories of Lee Cyclogenesis 4. Orographic Control of Precipitation 4.1 Observations of Rainfall Distribution 4.2 The Mechanism of Upslope Rain 4.3 The Redistribution of Rainfall by Small Hills 4.4 Orographic-Convective Precipitation 5. Planetary-Scale Mountain Waves 5.1 A Vertically Integrated Model of Topographically Forced Planetary Waves 5.2 The Vertical Structure of Planetary Waves on a ,8-Plane between Bounding Latitudes 5.3 Models of Stationary Planetary Waves Allowing Meridional Propagation and Lateral Variation in the Background Wind References
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  • 6
    Call number: AWI G7-81-0027 ; AWI G5-86-0505
    Type of Medium: Monograph available for loan
    Pages: VIII, 172 S.
    Language: English
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 7
    Series available for loan
    Series available for loan
    Boulder : The Geological Society of America
    Associated volumes
    Call number: S 90.0095(158)
    In: Special paper
    Type of Medium: Series available for loan
    Pages: 82 S.
    ISBN: 081372158X
    Series Statement: Special paper / Geological Society of America 158
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 8
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Pergamon Press
    Call number: AWI A6-01-0208
    Type of Medium: Monograph available for loan
    Pages: XVI, 241 S. , graph. Darst.
    Edition: 1. Aufl.
    ISBN: 0080216153
    Series Statement: Pergamon international library of science, technology, engineering and social studies
    Language: English
    Note: Contents: Preface. - List of Symbols Commonly Used in the Text. - Acknowledgements. - 1 Introduction. - 2 Properties of Sea Water Relevant to Physical Oceanography. - Introduction. - Density. - Measurement of density, temperature and salinity. - Relative density, sigma-t and specific volume. - Tables for density and specific volume as functions of temperature, salinity and pressure. - Sources of data. - 3 The Basic Physical Laws Used in Oceanography and Classifications of Forces and Motions in the Sea. - Basic laws. - Classification of forces and motion. - 4 The Equation of Continuity of Volume. - The concept of continuity of volume. - The derivation of the equation of continuity of volume. - An application of the equation of continuity. - 5 Stability and Double Diffusion. - Static stabiIity. - Criterion for static stability (E). - Numerical values for stability. - Double diffusion. - Dynamic stability. - 6 The Equation of Motion in Oceanography. - The form of the equation of motion. - Obtaining solutions to the equations, including boundary conditions. - The derivation of the terms in the equation of motion. - The pressure term. - Transforming from axes fixed in space to axes fixed in the rotating earth. - Gravitation and gravity. - The Coriolis terms. - Other accelerations. - Coordinate systems. - 7 The Role of the Non-Linear Terms in the Equations of Motion. - The non-linear terms in the equation of motion. - The friction term for the instantaneous velocity. - What is the source of the difficulty?. - Scaling and the Reynolds Number. - Reynolds stresses. - Equations for the mean or average motion. - Reynolds stresses and eddy viscosity. - Scaling the equations of motion. - Dynamic stabiIity. - The effect of density variations on dynamic stability. - Effects of rotation. - 8 Currents Without Friction: Geostrophic Flow. - Hydrostatic equiIibrium. - Inertial flow. - GeopotentiaI. - Geopotential surfaces and isobaric surfaces. - The geostrophic equation. - Why worry about the geostrophic equation?. - The geostrophic method for calculating relative velocities. - An example of the calculation of a geostrophic velocity profile. - An alternative derivation of the geostrophic equation. - The 'thermal wind' equations. - Absolute velocities. - Relations between isobaric and level surfaces. - Relations between isobaric and isopycnal surfaces. - Comments on the geostrophic equation. - Justification for using the geostrophic approach to obtain the speeds of strong currents. - 9 Currents With Friction. - Wind-driven circulations - introduction. - Nansen's qualitative argument. - The equations of motion with friction included. - Ekman's solution to the equations of motion with friction present. - Comments on the above experimental observations. - Transport and upwelling. - Upwelling or downwelling away from boundaries. - Bottom friction and shallow water effects. - Limitations of the Ekman theory. - Sverdrup's solution for the wind-driven circulation. - Orders of magnitude of the terms. - Application of the Sverdrup equation. - The general form of the Sverdrup equation. - The mass transport stream function. - Westward intensification - Stommel's contribution. - The planetary wind field. - Munk's solution. - Comments on Munk's solution. - Vorticity. - Relative vorticity. - Planetary vorticity. - Absolute vorticity. - Potential vorticity. - Westward intensification of ocean currents explained using conservation of potential vorticity. - Equatorial undercurrents. - The boundary layer approach. - The use of the boundary layer approach to obtain a solution to Munk's equation. - A simple inertial theory by Stommel. - 10 Thermohaline Effects. - The deep circulation. - Equations for salt and temperature (heat) conservation. - Equations for the average salinity and temperature. - Reynolds fluxes and eddy diffusivity. - Thermoclines and the thermohaline circulation. - The mixed layer of the ocean. - 11 Numerical Models. - Introduction. - Numerical methods. - General approach to numerical modelling of ocean circulations. - Descriptions of some models of individual oceans. - O'Brien's two-dimensional wind-driven model of the North Pacific. - Cox's model of the Indian Ocean. - Holland and Hirschmann's model of the Atlantic Ocean. - Two models of the circulation of the world ocean. - Models of mesoscale eddies. - Comments on the numerical model solutions. - 12 Waves. - Introduction. - Some general characteristics of waves. - Small amplitude waves. - Orbital motion of the water particles. - Refraction and breaking in shallow water; diffraction. - The generation of waves. - Measurement of waves. - ReaI waves. - Wave generation by the wind; semi-empirical relations. - Energy of waves. - Tsunamis or seismic sea waves. - Internal waves. - Effects of rotation. - Modified gravity waves. - Kelvin waves. - Planetary or Rossby waves. - Topographic effects. - 13 Tides. - Introduction. - Tide-producing forces. - Components of the tide-producing forces. - Ocean responses to the tide-producing forces - tidaI theories. - The practical approach to tide prediction. - The measurement of tides. - Types of tides. - Tidal currents. - Tides in bays-resonance. - Storm surges. - 14 Some Presently Active and Future Work. - APPENDIX I Mathematical Review with Some Elementary Fluid Mechanics. - Introduction. - Scalars and vectors. - Derivatives. - The individual or total derivative. - Integrals. - Fields. - Descriptions of fluid flow. - Convergences and divergences. - Hydrostatic pressure. - Slope effects. - CompressibiIity. - Centripetal and centrifugal forces. - APPENDIX 2 Units Used in Physical Oceanography. - Introduction. - Base units. - Derived and temporary units. - Units used in dynamic oceanography and some numerical values. - SUGGESTIONS FOR FURTHER READING AND FOR REFERENCE. - INDEX.
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  • 9
    Call number: M 94.0676
    In: AMD
    Type of Medium: Monograph available for loan
    Pages: v, 215 S.
    Series Statement: AMD Vol. 35
    Classification:
    C.3.6.
    Language: English
    Location: Upper compact magazine
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  • 10
    Monograph available for loan
    Monograph available for loan
    Leipzig : Brockhaus | Moskau : Verlag Progress
    Call number: AWI E2-89-0421
    Description / Table of Contents: Das größte Landraubtier unserer Erde ist der Eisbär - für die Forschung geradezu ein Modellfall für die Anpassungsfähigkeit des Organismus eines Lebewesens an die rauhen Bedingungen der Arktis. Immer wieder werden daher sowjetische Expeditionen entsandt, die die Aufgabe haben, das Verhalten des Eisbären in freier Wildbahn zu beobachten, einzelne Tiere zu wiegen, zu messen und zu markieren, um so tiefer in die Geheimnisse des „Eisbärendaseins" einzudringen. Besonders geeignet für solche Forschungen ist die Wrangel-lnsel vor der Nordostküste Sibiriens, ist sie doch die größte „Wochenstube" für Eisbären, die hier mitten im arktischen Winter ihre Jungen zur Welt bringen. Der weit über die Grenzen seines Heimatlandes hinaus bekannte Zoologe Prof. Dr. S. Uspenski, Teilnehmer vieler Expeditionen zur Wrangel-lnsel, berichtet hier in anschaulicher Weise über seine schwierige, oftmals nicht ungefährliche Arbeit und über die Rätsel, die der Eisbär auch heute noch der Wissenschaft aufgibt. Er mahnt in seinem Buch, mitzuhelfen, daß der Eisbär - diese größte Zierde der Arktis - auch künftigen Generationen der Menschheit erhalten bleibt. Uspenskis Wirken ist es mit zu danken, daß die Sowjetunion strenge Maßnahmen zum Schutz dieses vom Aussterben bedrohten Raubtieres ergriffen hat.
    Type of Medium: Monograph available for loan
    Pages: 203 Seiten , Illustrationen , 21 cm
    Edition: 3. Auflage
    ISBN: 3325001769 , 5-01-001792
    Uniform Title: Rodina belych medvedej 〈dt.〉
    Language: German
    Note: Inhalt Statt einer Einleitung An der Grenze der beiden Hemisphären Ein "Entbindungsheim" für die Eisbären Auf der Wrangel-Insel markiert Ihre Heimat ist das Eis Wohnheime für Vögel Weiße und Blaue Giganten des Eismeeres Schützt auch sie! Bildnachweis , Aus dem Russischen übersetzt
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