Results 91 to 100 of about 143 (124)
Some of the next articles are maybe not open access.

Free core nutation and geomagnetic jerks

Journal of Geodynamics, 2013
Abstract Variations in free core nutation (FCN) are associated with different processes in the Earth's fluid core and core–mantle coupling. The same processes are generally caused the variations in the geomagnetic field (GMF) particularly the geomagnetic jerks (GMJs), which are rapid changes in GMF secular variations.
Zinovy Malkin
exaly   +2 more sources

Localized analysis of polar geomagnetic jerks

Tectonophysics, 2013
Abstract A new method is introduced to find the relatively sudden temporal changes or jerks of the geomagnetic field over the polar regions. Geomagnetic jerk events during the 20th century have mostly been identified from direct measurements at mid-latitude geomagnetic observatories.
Hyung Rae Kim, Ralph R B Von Frese
exaly   +2 more sources

Geomagnetic Jerks: Rapid Core Field Variations and Core Dynamics

Space Science Reviews, 2010
The secular variation of the core field is generally characterized by smooth variations, sometimes interrupted by abrupt changes, named geomagnetic jerks. The origin of these events, observed and investigated for over three decades, is still not fully understood.
Giuliana Verbanac   +2 more
exaly   +6 more sources

On the Spectrum of Geomagnetic Variations Accompanying Jerks

Izvestiya, Physics of the Solid Earth
Based on the data of several spaced magnetic stations, the spectrum of geomagnetic variations is studied in the range of periods from two to 40 years. Special attention is paid to spectral features in the supposed range of action of intraterrestrial processes that cause geomagnetic jerks.
S A Riabova, S L Shalimov, Riabova S A
exaly   +3 more sources

The geomagnetic jerk of 1969 and the DGRFs

Physics of the Earth and Planetary Interiors, 1987
Abstract Cubic spline fits to the DGRF/IGRF series indicate agreement with other analyses showing the 1969–1970 magnetic jerk in the h 1 2 and g 0 2 secular change coefficients, and agreement that the h 1 1 term showed no sharp change.
Delaine Thompson, Joseph C. Cain
openaire   +1 more source

On the geomagnetic jerk of 1969

Journal of Geophysical Research: Solid Earth, 1985
French and British scientists have published reports describing a sudden change in the geomagnetic secular acceleration which took place around 1969. They claimed that this change, called an impulse or jerk, took place in a period of a year or two and that the sources for the jerk were internal.
openaire   +1 more source

A geomagnetic jerk for the end of the 20th century?

Earth and Planetary Science Letters, 2000
Abstract The series of magnetic measurements at some European observatories give some hint of a new geomagnetic jerk around 1999. The geomagnetic impulses would present the remarkable and intriguing property to occur with a frequency of one per decade, in the last third of the 20th century.
Mioara Mandea   +2 more
openaire   +1 more source

Automatic quality control for geomagnetic observatories and fast detection of geomagnetic jerks

2023
MOSFiT (Magnetic Observatories and Stations Filtering Tool) is a python package to visualize and filter data from magnetic observatories and magnetometer stations. The purpose of MOSFiT is to automatically isolate and analyze the secular variation (SV) information contained in geomagnetic observatories data.
Siqueira Da Silva, M.   +3 more
openaire   +2 more sources

More on the alleged 1970 geomagnetic jerk

Physics of the Earth and Planetary Interiors, 1985
Abstract French and United Kingdom workers have published reports describing a sudden change in the secular acceleration, called an impulse or a jerk, which took place around 1970. They claim that this change took place in a period of a year or two and that the sources of the alleged jerk are internal. An earlier paper by this author questioned their
openaire   +1 more source

Was the 1970 geomagnetic jerk of internal or external origin?

Nature, 1982
Annual mean data from worldwide magnetic observatories show that there was a jerk1 (step-change in the second time derivative) in the geomagnetic field, which took place over an interval of
S. R. C. Malin, B. M. Hodder
openaire   +1 more source

Home - About - Disclaimer - Privacy