Numerical dynamo models of Uranus' and Neptune's magnetic fields
By S. Stanley, J. Bloxham. 2006
149 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/1dc43cbff3a653b8b62828102227f72fbe9d244b
How researchers see this paper
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In Astronomy and Astrophysics
- Jon Fortney
- N. Nettelmann
- Ronald Redmer
- R. Helled
- J. Anderson
- Gerald Schubert
- M. Podolak
- U. Christensen
In Atmospheric Science
In Molecular Biology
- Jon Fortney
- N. Nettelmann
- Ronald Redmer
- Gerald Schubert
- J. Anderson
- U. Christensen
- Julien Aubert
- Johannes Wicht
Citations in the corpus
- New indication for a dichotomy in the interior structure of Uranus and Neptune from the application of modified shape and rotation data (2012, background): “Magnetic field models of Uranus and Neptune require that 60–70% of the region interior to the ionic water layer, corresponding to 0.42–0.56 Rp (Redmer et al., 2011), is stable to convection (Stanley and Bloxham, 2006).”
- Dynamo Scaling Laws and Applications to the Planets (2010, background): “A thin shell dynamo above a stably stratified conducting core might explain the multipolar nature of the magnetic field (Stanley and Bloxham 2004, 2006), but it could run into the problem of a subcritical magnetic Reynolds number, as mentioned above.”
- INTERIOR MODELS OF URANUS AND NEPTUNE (2010, background): “The magnetic fields of Uranus and Neptune provide additional information about their interiors (Ness et al. 1986, 1989; Stanley & Bloxham 2004, 2006).”