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Simple Mechanism for Reversals of Earth’s Magnetic Field

Simple Mechanism for Reversals of Earth’s Magnetic Field

http://www.wikidata.org/entity/Q56637813

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Chaos as an intermittently forced linear system Mechanisms for magnetic field reversals.Optimized setup for two-dimensional convection experiments in thin liquid films.Dynamical similarity of geomagnetic field reversals.Influence of counter-rotating von Kármán flow on cylindrical Rayleigh-Bénard convection.Chaos driven by interfering memory.Symmetry-breaking Hopf bifurcations to 1-, 2-, and 3-tori in small-aspect-ratio counterrotating Taylor-Couette flow.Dynamics and symmetries of flow reversals in turbulent convection.Evidence for forcing-dependent steady states in a turbulent swirling flow.Magnetic reversals from planetary dynamo waves

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Simple Mechanism for Reversals of Earth’s Magnetic Field

http://www.wikidata.org/entity/Q56637813

description

article publié dans la revue scientifique Physical Review Letters

@fr

im April 2009 veröffentlichter wissenschaftlicher Artikel

@de

scientific article published in Physical Review Letters

@en

wetenschappelijk artikel

@nl

наукова стаття, опублікована у квітні 2009

@uk

name

Simple Mechanism for Reversals of Earth’s Magnetic Field

@en

Simple Mechanism for Reversals of Earth’s Magnetic Field

@nl

type

label

Simple Mechanism for Reversals of Earth’s Magnetic Field

@en

Simple Mechanism for Reversals of Earth’s Magnetic Field

@nl

prefLabel

Simple Mechanism for Reversals of Earth’s Magnetic Field

@en

Simple Mechanism for Reversals of Earth’s Magnetic Field

@nl

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PHYSREVLETT.102.144503

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Physical Review Letters

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Simple mechanism for reversals of earth's magnetic field

@en

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François Pétrélis

http://www.w3.org/2001/XMLSchema#string

Jean-Pierre Valet

http://www.w3.org/2001/XMLSchema#string

Stéphan Fauve

http://www.w3.org/2001/XMLSchema#string

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Dependence of the duration of geomagnetic polarity reversals on site latitude.

Large-scale flow generation in turbulent convection

Geomagnetic dipole strength and reversal rate over the past two million years.

The role of the Earth's mantle in controlling the frequency of geomagnetic reversals

Mantle plumes link magnetic superchrons to phanerozoic mass depletion events

Oscillation or rotation: a comparison of two simple reversal models

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144503

http://www.w3.org/2001/XMLSchema#string

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scholarly article

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10.1103/PHYSREVLETT.102.144503

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P433

14

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102

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2009-04-07T00:00:00Z

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24358260

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19392444

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0806.3756

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