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  • 1
    Monograph available for loan
    Monograph available for loan
    Mantle convection : plate tectonics and global dynamics (1989)
    New York [u.a.] : Gordon and Research Science Publ.
    Associated volumes
    Details Availability
    Call number: M 92.0777 ; M 93.0395
    In: Fluid mechanics of astrophysics and geophysics
    Type of Medium: Monograph available for loan
    Pages: VIII, 881 S.
    ISBN: 0677221207
    Series Statement: Fluid mechanics of astrophysics and geophysics
    Classification:
    Geodynamics
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    The forward problem; I. (1985)
    Associated volumes
    Details Availability
    Call number: O 6065
    In: Glacial-isostatic adjustment
    Type of Medium: Monograph available for loan
    Pages: S. 605-646
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    The inverse problem; II. (1985)
    Associated volumes
    Details Availability
    Call number: O 6066
    In: Glacial-isostatic adjustment
    Type of Medium: Monograph available for loan
    Pages: S. 669-706
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Electronic Resource
    Electronic Resource
    Mantle Convection and Viscoelasticity (1985)
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Fluid Mechanics 17 (1985), S. 561-608 
    Details
    ISSN: 0066-4189
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1146/annurev.fl.17.010185.003021
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  • 5
    Electronic Resource
    Electronic Resource
    Ice Age Geodynamics (1981)
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 9 (1981), S. 199-225 
    Details
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1146/annurev.ea.09.050181.001215
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  • 6
    Electronic Resource
    Electronic Resource
    Oceanic bathymetry profiles flattened by radiogenic heating in a convecting mantle (1980)
    [s.l.] : Nature Publishing Group
    Nature 285 (1980), S. 649-651 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Ignoring horizontal conduction and assuming isostatic compensation at the base of the lithospheric plate, Parsons and McKenzie2 derived the following energy balance equation for a column through the plate: - (?m - ?w) Cp/a D/t+ qu = qb + z H'(z)dz (1) where ?m is the mantle density (below the ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/285649a0
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  • 7
    Electronic Resource
    Electronic Resource
    New constraints on transient lower mantle rheology and internal mantle buoyancy from glacial rebound data (1985)
    [s.l.] : Nature Publishing Group
    Nature 318 (1985), S. 614-617 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A model of mantle rheology which has an explicit transient component of its relaxation spectrum is shown to reconcile two apparently conflicting inferences of lower mantle viscosity. If recent analyses of isostatic geoid anomalies are correct in requiring a large increase of viscosity with depth, ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/318614a0
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  • 8
    Electronic Resource
    Electronic Resource
    Constraint on deep mantle viscosity from Lageos acceleration data (1983)
    [s.l.] : Nature Publishing Group
    Nature 304 (1983), S. 434-436 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The question as to the value of the Earth's viscosity beneath a depth of 670 km remains an important issue. This depth is marked by the presence of a solid-solid phase transition from the low-pressure phase spinel to the high-pressure mixture of the minerals perovskite and magnesiowustite1. Because ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/304434a0
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  • 9
    Electronic Resource
    Electronic Resource
    Quasi-geostrophic simulations of the 1979 stratospheric major warming: The importance of middle-atmospheric drag (1986)
    Springer
    Pure and applied geophysics 124 (1986), S. 1051-1085 
    Details
    ISSN: 1420-9136
    Keywords: Quasi-geostrophic model ; stratospheric major warming ; middle-atmospheric drag
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A detailed test of a simple nonlinear quasi-geostrophic model of stratospheric sudden warming has been performed. The model is of Matsuno's type, which includes only the interaction between a single planetary wave and the zonal mean flow. Given this limitation, the 1979 major stratospheric sudden warming has been employed to test the ability of the model to simulate an actual warming event. This event proved to be an especially appropriate testing ground for the model, since its main assumptions were reasonably well satisfied by the observational evidence. Results from the model simulations demonstrate (a) that such simple quasi-geostrophic dynamics are completely capable of providing a rather detailed simulation of the 1979 major warming event and (b) that the ability of the model to simulate successfully the observed evolution of the warming is extremely sensitive to the magnitude and form of the dissipation mechanism that is assumed to operate in the middle atmosphere.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00879931
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  • 10
    Electronic Resource
    Electronic Resource
    Sensitivity experiments with a quasi-geostrophic model of stratospheric sudden warming (1985)
    Springer
    Pure and applied geophysics 123 (1985), S. 99-140 
    Details
    ISSN: 1420-9136
    Keywords: Quasi-geostropic model ; Statospheric sudden warming
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract We describe a series of sensitivity experiments with a quasi-geostrophic model of the interaction of stationary planetary waves with the mean zonal flow in the stratosphere and mesosphere. The model is of the Matsuno type, which neglects wave-wave interaction and includes only a single zonal harmonic of the planetary wave spectrum in each simulation. We employed the model to investigate the source of the double-layer structure previously obtained by several authors for the stratospheric sudden warming with wavenumber one. Our results suggest that this characteristic of the model-produced warming is a property only of models without damping. When reasonable dissipation is included in the model, the double-layer structure disappears. This implies the importance of the drag parameterization in properly simulating warming events and, since the actual drag very probably is effected by breaking internal waves, it suggests that future analysis should include a specific representation of this effect. We also investigated the dependence of stratospheric warming on the structure of the zonal wind field. Our analyses show in particular that substantial reduction of the height of the polar night jet mitigates strongly against the occurrence of a sudden warming event.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00877052
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