ملخص
The linear stability of a differentially heated cylindrical annulus, of finite length, containing a dissipationless fluid and rotating uniformly in a nonuniform toroidal magnetic field is studied. The analysis is restricted to the situation where the instabilities are driven by buoyancy. If the end-surfaces are flat, the unstable waves propagate against the basic flow, i.e. westward. When the effect of slight distortions in the end-surfaces on the propagation speeds of these waves are investigated, it is found that these distortions can decrease or increase the propagation speeds depending on a variety of conditions. The application of these results to Hide's (1969) theory on the effects of bumps on the core-mantle interface of the Earth indicates that these topographical features may lead to irregular fluctuations in the westward drift.
اللغة الأصلية | English |
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الصفحات (من إلى) | 75-88 |
عدد الصفحات | 14 |
دورية | Geophysical and Astrophysical Fluid Dynamics |
مستوى الصوت | 9 |
رقم الإصدار | 1 |
المعرِّفات الرقمية للأشياء | |
حالة النشر | Published - يناير 1977 |
منشور خارجيًا | نعم |
ASJC Scopus subject areas
- ???subjectarea.asjc.2200.2206???
- ???subjectarea.asjc.3100.3103???
- ???subjectarea.asjc.1900.1908???
- ???subjectarea.asjc.2200.2211???
- ???subjectarea.asjc.1900.1906???