Modelling of the geomagnetic field is a complex challenge, hindered by noisy and incomplete ground and satellite observations, and the extent to which we can separate the contributions of the various field sources in these data. Forecasting of the core field and its time variations (secular variation), an activity of key interest for academic and applied studies of geomagnetism and space weather, is further complicated by an incomplete knowledge of the physics controlling magnetic field generation. Predictive core field models often rely on simple mathematical extrapolation to produce short term (<5 year) forecasts, but this technique can struggle when rapid variations known as geomagnetic jerks cause distinctly non-linear secular variation...
Global geomagnetic field models can be used to study the dynamics of the core, aid satellite operati...
The secular variation (SV) and secular acceleration (SA) of the Earth’s geomagnetic field, generated...
International audienceWe present the geomagnetic field model COV-OBS.x2 that covers the period 1840-...
The secular variation (SV) of the geomagnetic field is difficult to accurately predict with our curr...
The secular variation and secular acceleration of the Earth’s geomagnetic core field pose a difficul...
Improving forecasts of the temporal and spatial changes of the Earth's main magnetic field over peri...
Over the past ten years satellite measurements in combination with data from ground-based observator...
[1] Geomagnetic main field models used for navigation are updated every 5 years and contain a foreca...
Global geomagnetic field models are designed to represent the sources of Earth’s magnetic field and ...
Ground-based data that are contemporary with the Ørsted mission are valuable as an independent data...
Abstract Each International Geomagnetic Reference Field (IGRF) model released under the auspices of ...
International audienceObservational constraints on geomagnetic field changes from interannual to mil...
Accurate forecasting of the change of the Earth's internal magnetic field over short intervals of ti...
Global geomagnetic field models can be used to study the dynamics of the core, aid satellite operati...
The secular variation (SV) and secular acceleration (SA) of the Earth’s geomagnetic field, generated...
International audienceWe present the geomagnetic field model COV-OBS.x2 that covers the period 1840-...
The secular variation (SV) of the geomagnetic field is difficult to accurately predict with our curr...
The secular variation and secular acceleration of the Earth’s geomagnetic core field pose a difficul...
Improving forecasts of the temporal and spatial changes of the Earth's main magnetic field over peri...
Over the past ten years satellite measurements in combination with data from ground-based observator...
[1] Geomagnetic main field models used for navigation are updated every 5 years and contain a foreca...
Global geomagnetic field models are designed to represent the sources of Earth’s magnetic field and ...
Ground-based data that are contemporary with the Ørsted mission are valuable as an independent data...
Abstract Each International Geomagnetic Reference Field (IGRF) model released under the auspices of ...
International audienceObservational constraints on geomagnetic field changes from interannual to mil...
Accurate forecasting of the change of the Earth's internal magnetic field over short intervals of ti...
Global geomagnetic field models can be used to study the dynamics of the core, aid satellite operati...
The secular variation (SV) and secular acceleration (SA) of the Earth’s geomagnetic field, generated...
International audienceWe present the geomagnetic field model COV-OBS.x2 that covers the period 1840-...