Secular variation (SV) of Earth’s internal magnetic field is the sum of two contributions, one resulting from core fluid flow and the other from magnetic diffusion. Based on the millenial diffusive timescale of global-scale structures, magnetic diffusion is widely perceived to be too weak to significantly contribute to decadal SV, and indeed is entirely neglected in the commonly adopted end-member of frozen-flux. Such an argument however lacks consideration of radially fine-scaled magnetic structures in the outermost part of the liquid core, whose diffusive timescale is much shorter. Here we consider the opposite end-member model to frozen flux, that of purely diffusive evolution associated with the total absence of fluid flow. Our work is ...
International audienceInverse geodynamo modelling seeks to estimate the dynamic state of Earth's cor...
Variational data assimilation (4DVar) is a powerful technique for tuning dynamic models to observati...
Detailed knowledge of the long-term spatial configuration and temporal variability of the geomagneti...
Secular variation (SV) of Earth’s internal magnetic field is the sum of two contributions, one resul...
Earth’s internal magnetic field is generated through motion of the electrically conductive iron-allo...
Changes in the magnetic field generated within Earth's core that occur over years to centuries are k...
Earth’s internal magnetic field is generated through motion of the electrically conductive iron-allo...
Improving forecasts of the temporal and spatial changes of the Earth's main magnetic field over peri...
International audienceThe frozen flux assumption consists in neglecting magnetic diffusion in the co...
International audienceWe present core flows constructed from high resolution secular variation (SV) ...
The Earth’s magnetic field is generated by fluid motion of liquid iron in the outer core. Flows at t...
International audienceWe use numerical dynamos to investigate the possible role of magnetic diffusio...
International audienceThe frozen flux assumption consists in neglecting magnetic diffusion in the co...
The secular variation (SV) and secular acceleration (SA) of the Earth’s geomagnetic field, generated...
We describe a new technique for implementing the constraints on magnetic fields arising from two hyp...
International audienceInverse geodynamo modelling seeks to estimate the dynamic state of Earth's cor...
Variational data assimilation (4DVar) is a powerful technique for tuning dynamic models to observati...
Detailed knowledge of the long-term spatial configuration and temporal variability of the geomagneti...
Secular variation (SV) of Earth’s internal magnetic field is the sum of two contributions, one resul...
Earth’s internal magnetic field is generated through motion of the electrically conductive iron-allo...
Changes in the magnetic field generated within Earth's core that occur over years to centuries are k...
Earth’s internal magnetic field is generated through motion of the electrically conductive iron-allo...
Improving forecasts of the temporal and spatial changes of the Earth's main magnetic field over peri...
International audienceThe frozen flux assumption consists in neglecting magnetic diffusion in the co...
International audienceWe present core flows constructed from high resolution secular variation (SV) ...
The Earth’s magnetic field is generated by fluid motion of liquid iron in the outer core. Flows at t...
International audienceWe use numerical dynamos to investigate the possible role of magnetic diffusio...
International audienceThe frozen flux assumption consists in neglecting magnetic diffusion in the co...
The secular variation (SV) and secular acceleration (SA) of the Earth’s geomagnetic field, generated...
We describe a new technique for implementing the constraints on magnetic fields arising from two hyp...
International audienceInverse geodynamo modelling seeks to estimate the dynamic state of Earth's cor...
Variational data assimilation (4DVar) is a powerful technique for tuning dynamic models to observati...
Detailed knowledge of the long-term spatial configuration and temporal variability of the geomagneti...