Great geomagnetic storm of 9 November 1991: Association with a disappearing solar filament
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Cites background from "Great geomagnetic storm of 9 Novemb..."
...geomagnetic variations or indices (e.g., Li et al. 2006; Cliver et al. 2009)....
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...Other papers have reconstructed solar wind parameters during large storms by using geomagnetic variations or indices (e.g., Li et al. 2006; Cliver et al. 2009)....
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References
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877 citations
"Great geomagnetic storm of 9 Novemb..." refers background in this paper
...…[1964] as a precursor of the general recognition, which came nearly 30 years later, that certain CMEs, rather than the major flares with which they were characteristically, but not always, associated, were the essential element for producing great sporadic storms [Kahler, 1992; Gosling, 1993]....
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...CMEs, rather than the major flares with which they were characteristically, but not always, associated, were the essential element for producing great sporadic storms [Kahler, 1992; Gosling, 1993]....
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802 citations
"Great geomagnetic storm of 9 Novemb..." refers background or methods in this paper
...Because the widely used am and Dst geomagnetic indices [Mayaud, 1980] have different dependencies on these parameters, we can use them to fill data gaps in the following manner: (1) on the basis of experience and intuition, assume solar wind speed and magnetic field data for periods of missing…...
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...[2] Following Newton [1943], and prior to Joselyn and McIntosh [1981], solar flares were widely considered to be the sole source of great sporadic geomagnetic storms....
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...Because the widely used am and Dst geomagnetic indices [Mayaud, 1980] have different dependencies on these parameters, we can use them to fill data gaps in the following manner: (1) on the basis of experience and intuition, assume solar wind speed and magnetic field data for periods of missing data; (2) use these composite profiles (consisting of actual and assumed values) to derive one of the indices (in our case am, via Svalgaard [1977]); (3) adjust the assumed, gap-filling, solar wind parameters as necessary until the observed am is faithfully reproduced by the model; (4) use the various continuous solar wind parameter series obtained by this method (i....
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...Because the widely used am and Dst geomagnetic indices [Mayaud, 1980] have different dependencies on these parameters, we can use them to fill data gaps in the following manner: (1) on the basis of experience and intuition, assume solar wind speed and magnetic field data for periods of missing data; (2) use these composite profiles (consisting of actual and assumed values) to derive one of the indices (in our case am, via Svalgaard [1977]); (3) adjust the assumed, gap-filling, solar wind parameters as necessary until the observed am is faithfully reproduced by the model; (4) use the various continuous solar wind parameter series obtained by this method (i.e., V, BX, BY, BZ, and n (density); with V and BZ shown in Figure 7) to calculate the other index (Dst, via Temerin and Li [2002]) as a test of the method....
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"Great geomagnetic storm of 9 Novemb..." refers background in this paper
...The 17 April event represents an extreme example of a problem storm in that the long segment of chromospheric neutral line over which the eruption occurred was marked only by filament channels (FC) [Martin, 1998] and small and faint filaments....
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