Description: Global spherical harmonic paleomagnetic field model LSMOD.1 describes the magnetic field evolution from 50 to 30 ka BP based on published paleomagnetic sediment records and volcanic data. The time interval includes the Laschamp (~41 ka BP) and Mono Lake (~34 ka BP) excursions. The model is given with Fortran source code to obtain spherical harmonic magnetic field coefficients for individual epochs and to obtain time series of magnetic declination, inclination and field intensity from 49.95 to 30 ka BP for any location on Earth. For details see M. Brown, M. Korte, R. Holme, I. Wardinski and S. Gunnarson (2018): Earth's magnetic field is probably not reversing. PNAS, 115, 5111-5116.
Global identifier:
Doi(
"10.5880/GFZ.2.3.2018.008",
)
Tags: Seen ? Sediment ? Daten ? Zeitreihe ? EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > MAGNETIC FIELD > MAGNETIC DECLINATION ? EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > MAGNETIC FIELD > MAGNETIC INCLINATION ? EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > MAGNETIC FIELD > MAGNETIC INTENSITY ? EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > PALEOMAGNETISM ? EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > REFERENCE FIELDS ? EPOS ? geomagnetic excursion ? multi-scale laboratories ? paleomagnetic and magnetic data ? paleomagnetic field model ? software tools ?
License: cc-by/4.0
Language: Englisch/English
Issued: 2018-01-01
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