Parameters of the Earth's Free Core Nutation from Diurnal Strain Tides. [PDF]
Amoruso A, Crescentini L.
europepmc +1 more source
S U M M A R Y By subtracting computed atmospheric angular momentum from a time-series for length-of-day variations, we obtain a high-resolution time-series that is useful for studying the effects of the core on length-of-day variations.
O De Viron +3 more
core
New perspectives in the study of the Earth's magnetic field and climate connection: The use of transfer entropy. [PDF]
Campuzano SA +4 more
europepmc +1 more source
Archaeointensity results spanning the past 6 kiloyears from eastern China and implications for extreme behaviors of the geomagnetic field. [PDF]
Cai S +6 more
europepmc +1 more source
Geomagnetic jerks: impulses of secular variation in geophysics
Geomagnetic records from some observatories give a strong indication that there was a rapid, impulsive change in geomagnetic secular acceleration around 1990.
De Michelis, P. +2 more
core +1 more source
Reconstructing the Geomagnetic Field in West Africa: First Absolute Intensity Results from Burkina Faso. [PDF]
Kapper L +5 more
europepmc +1 more source
Forecasting secular variation using physics-informed neural networks for IGRF-14. [PDF]
Shakespeare-Rees N +6 more
europepmc +1 more source
A Comprehensive Model of Earth's Magnetic Field Determined From 4 Years of Swarm Satellite Observations. [PDF]
Sabaka TJ +3 more
europepmc +1 more source
Core-surface flows, geomagnetic jerks and short-term predictions of the Earth's magnetic field
Dans ce mémoire nous présentons une série d'études dont le double objectif est de mieux comprendre les phénomènes qui gouvernent l'évolution du champ magnétique principal de la Terre, et d'améliorer notre capacité actuelle à en prédire l'évolution à ...
SILVA, Luís Alexandre, HULOT, Gauthier
core
Could the Mw = 9.3 Sumatra Earthquake Trigger a Geomagnetic Jerk?
The magnetic field observed at the Earth’s surface is not a stationary feature. It is characterized by time variations ranging from milliseconds (micropulsations) to millions of years (the time interval between field reversals).
De Michelis, P. +3 more
core

