We propose two ensembles of geomagnetic field models spanning the last three millennia:
COV-ARCH is calculated using all available archeological artefacts and volcanic lava flows; …

Reconstructions of the Holocene geomagnetic field and how it varies on millennial
timescales are important for understanding processes in the core but may also be used to …

Abstract Changes of the Earth's magnetic field have been observed with varying spatial and
temporal resolution since the middle ages by means of compasses, and later by refined …

We propose a global geomagnetic field model for the last 14 thousand years, based on
thermoremanent records. We call the model ArchKalmag14k. ArchKalmag14k is constructed …

A record of relative paleointensity from marine sediments in the equatorial Indian Ocean
spanning the last 4 Ma completes a previous dataset from Ocean Drilling Program (ODP) …

Abstract Characterization of geomagnetic field behaviour on timescales of centuries to
millennia is necessary to understand the mechanisms that sustain the geodynamo and drive …

Several global geomagnetic field models exist for recent decades, but due to limited data
availability models for several centuries to millennia are rare. We present a continuous …

Current millennial‐scale time‐varying global geomagnetic field models suffer from a lack of
intensity data compared to directional data, because only thermoremanently magnetized …

Paleomagnetic measurements of direction and intensity recorded in crustal rocks enable
investigations of Earth's dynamo field, in particular over timescales for which direct …

Study of the late Quaternary geomagnetic field contributes significantly to understanding the
origin of millennial‐scale paleomagnetic secular variations, the structure of geomagnetic …