Storm sudden commencements and polar magnetic substorms

IGY sudden commencements of magnitude greater than 20 gammas simultaneously (±3 min) triggered magnetospheric substorms with a very high probability (∼90%). The magnitude dependence gives rise to a part of the large sunspot cycle variation of the probability of the occurrence of simultaneous events: 49% during the IGY and only 4% during the IQSY. Also, the degree of presubstorm disturbances (measured in terms of ΣKp), types of interplanetary discontinuities, and the direction of interplanetary magnetic field do not appear to be important parameters for ssc-triggered substorms. Therefore, these results may indicate that a sudden compression of the magnetosphere alone, if intense enough, can sometimes trigger substorms.

[1]  L. Burlaga Discontinuities and shock waves in the interplanetary medium and their interaction with the magnetosphere. , 1972 .

[2]  J. Schieldge,et al.  A correlation of the occurrence of simultaneous sudden magnetospheric compressions and geomagnetic bay onsets with selected geophysical indices , 1970 .

[3]  L. Burlaga,et al.  Tangential discontinuities in the solar wind , 1969 .

[4]  H. E. Taylor Sudden commencement associated discontinuities in the interplanetary magnetic field observed by IMP 3 , 1969 .

[5]  G. Rostoker Relationship between the onset of a geomagnetic bay and the configuration of the interplanetary magnetic field , 1968 .

[6]  L. Burlaga,et al.  Macro- and micro-structure of the interplanetary magnetic field , 1968 .

[7]  Edward J. Smith,et al.  Power spectra and discontinuities of the interplanetary magnetic field - Mariner 4. , 1968 .

[8]  C. Fälthammar,et al.  Relationship between changes in the interplanetary magnetic field and variations in the magnetic field at the Earth's surface , 1967 .

[9]  Douglas E. Jones,et al.  The magnetic morphology of solar streams and its relation to geomagnetic storms , 1967 .

[10]  Kenneth H. Schatten,et al.  Response of the geomagnetic activity index Kp to the interplanetary magnetic field , 1967 .

[11]  W. Axford Magnetic storm effects associated with the tail of the magnetosphere , 1967 .

[12]  D. H. Fairfield,et al.  Polar magnetic disturbances and the interplanetary magnetic field. , 1967 .

[13]  J. Wilcox,et al.  Influence of interplanetary magnetic field and plasma on geomagnetic activity during quiet-sun conditions , 1967 .

[14]  L. J. Cahill,et al.  Transition region magnetic field and polar magnetic disturbances. , 1966 .

[15]  J. W. Dungey,et al.  Interactions of solar plasma with the geomagnetic field , 1963 .

[16]  S. Akasofu Large-scale auroral motions and polar magnetic disturbances—II The changing distribution of the aurora during large magnetic storms , 1962 .

[17]  Charles R. Wilson,et al.  Hydromagnetic interpretation of sudden commencements of magnetic storms , 1961 .

[18]  J. Dungey Interplanetary Magnetic Field and the Auroral Zones , 1961 .

[19]  J. Heppner Note on the occurrence of world‐wide S.S.C.'s during the onset of negative bays at College, Alaska , 1955 .