2020
DOI: 10.1016/j.pepi.2020.106589
|View full text |Cite
|
Sign up to set email alerts
|

Magnetic boundary layers in numerical dynamos with heterogeneous outer boundary heat flux

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
4
1

Relationship

1
4

Authors

Journals

citations
Cited by 5 publications
(1 citation statement)
references
References 94 publications
(158 reference statements)
0
1
0
Order By: Relevance
“…For instance, MagIC was used to study the "top-heavy" regime of double-diffusive convection, when thermal and compositional background gradients are destabilizing (Tassin et al, 2021). In a recent paper, MagIC has been used to study magnetic boundary layers with heterogeneous outer boundary heat flux, with results suggesting a significant deviation from classical estimates of the diffusion time and the magnetic Reynold number (Terra-Nova and Amit, 2020). In another paper, the dynamics of a possible stable stratification layer atop Earth's core was explored (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…For instance, MagIC was used to study the "top-heavy" regime of double-diffusive convection, when thermal and compositional background gradients are destabilizing (Tassin et al, 2021). In a recent paper, MagIC has been used to study magnetic boundary layers with heterogeneous outer boundary heat flux, with results suggesting a significant deviation from classical estimates of the diffusion time and the magnetic Reynold number (Terra-Nova and Amit, 2020). In another paper, the dynamics of a possible stable stratification layer atop Earth's core was explored (e.g.…”
Section: Introductionmentioning
confidence: 99%