The geomagnetic field has been decaying at a rate of∼ 5% per century from at least 1840,
with indirect observations suggesting a decay since 1600 or even earlier. This has led to the …

The strength of the geomagnetic field has decreased rapidly over the past two centuries,
coinciding with an increasing field asymmetry due to the growth of the South Atlantic …

Abstract The South Atlantic Anomaly (SAA) is an area of geomagnetic weakness that
represents the most significant anomaly in the present‐day field. Notwithstanding anomalies …

The diminishing strength of the Earth's magnetic dipole over recent millennia is
accompanied by the increasing prominence of the geomagnetic South Atlantic Anomaly …

The geomagnetic field is subject to possible reversals or excursions of polarity during its
temporal evolution. Considering that:(a) in the last 83 million yr the typical average time …

Data-based global paleomagnetic field models provide a more complete view of
geomagnetic excursions than individual records. They allow the temporal and spatial field …

The Laschamp event ended between 8000 and 20000 years ago. In several other parts of
the world, excursions of the Earth's magnetic field have been seen at about this time interval …

The reversed paleomagnetic direction of the Laschamp and Olby flows represents a specific
feature of the geomagnetic field. This is supported by paleomagnetic evidence, showing that …

We report here on a new paleomagnetic (directions and intensities) and coupled K/Ar and
40 Ar/39 Ar analysis of 35 different flows, emplaced in the Chaîne des Puys during the 75 to …

No evidence for a geomagnetic reversal between 30 400 and 13 300 yr ago has been found
in a paleomagnetic study of sediments from Mono Lake, California, with ages controlled by …