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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 59 (1964), S. 100-122 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary A charged particle moves with velocityv in a constant non-uniform magnetic fieldH, spiralling with Larmor radiusR. IfR is small compared with the scale lengthL of the field, the magnetic moment associated with the Larmor motion of the particle is nearly constant. Consequently θ, the (‘pitch’) angle betweenv andH, varies as arcsinH 1/2. Hence θ in such adiabatic motion is approximately the same at points on the path whereH has the same value. But the magnetic moment and the pitch angle may differ materially at two such points, each in the region whereR/L is small, if between them the particle traverses a region whereR/L is not small. This region of non-adiabatic motion ‘scatters’ the pitch angles. Such scattering is investigated for regions of weak field (R large), with and without the presence of a neutral line along whichH=0. Either type of region, it is found, can scatter the pitch angles. This gives support to the theory proposed byAkasofu andChapman to explain why auroral arcs and bands are very thin. The scattering here examined is of interest also in connection with magnetic mirror devices for nuclear energy transformation. It may also have applications to phenomena of solar and stellar atmospheres.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 60 (1965), S. 117-125 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary It is suggested that electrodynamic drifts at right angles to the magnetic field lines in theF2 layer may be replaced by equivalent drifts along the field lines. The suggestion is used in conjunction with a straight field line model of the ionosphere to obtain a qualitative description of the form of an inospheric equilibrium layer formed in absence of production and loss. The layer produced has a latitudinal maximum ofN m , near dip angles of 30°, similar to that of the Appleton anomaly. It is concluded that good agreement would be obtained if electrodynamic drifts were included in attempts to compare theory and experiment above theF2 peak.
    Type of Medium: Electronic Resource
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  • 3
    Title: Vektoranalysis : mit 251 Aufgaben und zahlreichen Beispielen
    Author: Bourne, Donald E.
    Contributer: Kendall, Peter C.
    Uniform Title: Vector analysis and cartesian tensors 〈dt.〉
    Edition: 2., überarb. und erw. Aufl.
    Publisher: Stuttgart :Teubner,
    Year of publication: 1988
    Pages: 260 S. : Ill.
    Series Statement: Teubner-Studienbücher: Physik
    ISBN: 3-519-12044-5
    Type of Medium: Book
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