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A phenomenological study of the Dst storm variation

✍ Scribed by A.S. Potapov; T.N. Polyushkina

Publisher
Elsevier Science
Year
1992
Tongue
English
Weight
983 KB
Volume
40
Category
Article
ISSN
0032-0633

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## Abstract Since both observations and theory indicate weak dissipation, a frictionless one‐dimensional model elucidates the dynamics of the surge and is used to hindcast and forecast. Wind over the shallow northern Adriatic dominates the forcing. The relative phases of the astronomical tide, the