Inhaltsbereich
Publications
(Co) Author: Ball, L.
(since 2007) [ All ]
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(2010): The 1991 geomagnetic jerk as seen at the Earth’s surface and the core-mantle boundary. Geophysical Journal International, 183, 2, 659-680.
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(2010): Determining the time-variable part of the toroidal geomagnetic field in the core-mantle boundary zone. Physics of the Earth and Planetary Interiors, 178, 1-2, 56-67.
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(2007): Axial poloidal electromagnetic core-mantle coupling torque: a re-examination for different conductivity and satellite supported geomagnetic field models.. Studia Geophysica et Geodaetica, 51, 4, 491-513.
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(2007): A Simplified, Accurate and Fast Method for Lithium Isotope Analysis of Rocks and Fluids, and 7Li Values of Seawater and Rock Reference Materials. Geostandard Newsletters - The Journal for Geostandards and Geoanalysis, 31, 2, 77-88.
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(2011): Magnetic energy fluctuations on the core-mantle boundary. General Assembly European Geosciences Union (Vienna, Austria 2011).
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(2011): Influence of geometrical settings like flattening and topography of the core-mantle and inner-core boundaries on the gravitational core-mantle coupling. General Assembly European Geosciences Union (Vienna, Austria 2011).| EDOC: 16910 | Abstract |
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(2010): Comparative views of geomagnetic jerks. General Assembly European Geosciences Union (Vienna, Austria 2010).
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(2010): The core-mantle coupling contribution to the excitation of the Earth's rotation variation on decadal time scale. General Assembly European Geosciences Union (Vienna, Austria 2010).| EDOC: 14875 | Abstract |
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(2009): Phase shifts of the secular variation due to an electrically conducting earth mantle. General Assembly European Geosciences Union (Vienna, Austria 2009).
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(2009): Combined electromagnetic and topographic core-mantle coupling and its equivalent excitation function for the time interval 1961 - 2000. AGU 2009 Fall Meeting (San Francisco, USA 2009).| EDOC: 14135 |
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(2009): Combined coupling torques for the electromagnetic and topographic core-mantle coupling and their influence on Earth.. General Assembly European Geophysical Union (Vienna, Austria 2009).
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(2008): Case studies for the 1991 3D-secular variation impulse at the CMB.. General Assembly European Geosciences Union (Vienna, Austria 2008).
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(2008): Determination of the toroidal geomagnetic field in the lower mantle considering a radial electric conductivity profile.. General Assembly European Geosciences Union (Vienna, Austria 2008).
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(2008): Determination of the electromagnetic and topographic core-mantle coupling torques based on geomagnetic observations: Influence of the electric conductivity of the Earth's mantle.. AGU 2008 Fall Meeting (San Francisco, USA 2008).| EDOC: 12397 | Abstract |
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(2008): Influence of electric conductivity profiles of the lower mantle on the electromagnetic core-mantle coupling torque.. General Assembly European Geosciences Union (Vienna, Austria 2008).
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(2007): Gaining insights into space-time scales of the secular variation of the geomagnetic Y component at the core-mantle boundary. General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).
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(2007): 3-D geomagnetic impulses: Synopsis of field components at the CMB.. 24th IUGG 2007 (Perugia, Italy, 2007).| EDOC: 10851 | Abstract |
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(2007): The non-harmonic downward continuation method in deep earth magnetic field studies.. 24th IUGG 2007 (Perugia, Italy, 2007).| EDOC: 10850 | Abstract |
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(2007): Electromagnetic core-mantle coupling torques for different magnetic field models and core velocity fields. 24th IUGG 2007 (Perugia, Italy 2007).| EDOC: 10816 | Abstract |
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(2012): The geomagnetic nonharmonic downward continuation method (NHDC) : basics, details, special cases and some applications. Scientific Technical Report ; 12/08, Deutsches GeoForschungsZentrum GFZ, 70.
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(2012): Core-mantle coupling : Part IV: axial component of the core angular momentum. Scientific Technical Report ; 12/10, Deutsches GeoForschungsZentrum GFZ, 30.
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(2012): Core-mantle coupling : Part III: gravitational coupling torques. Scientific Technical Report ; 12/01, Deutsches GeoForschungsZentrum GFZ, 40.