Preferred locations of weak surface field in numerical dynamos with heterogeneous core–mantle boundary heat flux: consequences for the South Atlantic Anomaly-Reference-Cited by-同舟云学术

Preferred locations of weak surface field in numerical dynamos with heterogeneous core–mantle boundary heat flux: consequences for the South Atlantic Anomaly

Published:2019-02-04 Issue:2 Volume:217 Page:1179-1199
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Terra-Nova Filipe¹²^ORCID,Amit Hagay²,Choblet Gaël²^ORCID

Affiliation:

1. Departamento de Geofísica, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, Rua do Matão, 1226, Cidade Universitária, 05508-090 São Paulo, Brasil

2. CNRS, Université de Nantes, Nantes Atlantiques Universités, UMR CNRS 6112, Laboratoire de Planétologie et de Géodynamique, 2 rue de la Houssinière, F-44000 Nantes, France

Funder

National Council for Scientific and Technological Development

São Paulo Research Foundation

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/217/2/1179/28087157/ggy519.pdf

Reference79 articles.

1. Can downwelling at the top of the Earth’s core be detected in the geomagnetic secular variation?;Amit;Phys. Earth planet. Inter.,2014

2. Stationary, oscillating or drifting mantle-driven geomagnetic flux patches?;Amit;J. geophys. Res.,2010