Results 161 to 170 of about 1,292 (208)
A case study of the three-dimensional co-seismic ionospheric disturbance evolution. [PDF]
Song R +4 more
europepmc +1 more source
Radio emissions reveal Alfvénic activity and electron acceleration prior to substorm onset. [PDF]
Wu SY +18 more
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GNSS-VTEC prediction based on CNN-GRU neural network model during high solar activities. [PDF]
Yang TY +6 more
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Unexpected major geomagnetic storm caused by faint eruption of a solar trans-equatorial flux rope. [PDF]
Teng W, Su Y, Ji H, Zhang Q.
europepmc +1 more source
Extraction of metadata from solar disk H-alpha observations at Sacramento Peak Observatory. [PDF]
Illarionov EA, Yukui W, Pevtsov AA.
europepmc +1 more source
Real-Time Embedded Smart-Particle Monitoring for Index-Based Evaluation of Asphalt Mixture Compaction Quality. [PDF]
Xiao M +8 more
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Reviews of Geophysics, 1972
The purpose of this review is to outline the definition and method of derivation of the indices of geomagnetic activity that are most commonly used at present. The first part of the review presents the methods of derivation of Kp, ap, AE, and Dst; the second part involves a discussion of the strengths and weaknesses of each index.
exaly +2 more sources
The purpose of this review is to outline the definition and method of derivation of the indices of geomagnetic activity that are most commonly used at present. The first part of the review presents the methods of derivation of Kp, ap, AE, and Dst; the second part involves a discussion of the strengths and weaknesses of each index.
exaly +2 more sources
Indices of geomagnetic pulsations
Planetary and Space Science, 1972Abstract A system of spectral and energetic indices based on pulsations is proposed (taking into account the achievements of hydromagnetic diagnostics). The principle of the proposed system is to ascribe to each index a clear physical meaning.
V.A. Troitskaya +4 more
openaire +1 more source
1996
The predominant part of the geomagnetic field, as observed at the Earth’s surface, originates from sources in the Earth’s core and, to a lesser degree, in the Earth’s crust. Spatial distribution and secular variation of this internal part were described, e.g., by Schmucker (1985).
Walter Dieminger +2 more
openaire +1 more source
The predominant part of the geomagnetic field, as observed at the Earth’s surface, originates from sources in the Earth’s core and, to a lesser degree, in the Earth’s crust. Spatial distribution and secular variation of this internal part were described, e.g., by Schmucker (1985).
Walter Dieminger +2 more
openaire +1 more source

