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E. M. Tikhomolov 《Astronomische Nachrichten》1998,319(4):245-249
Powerful solar complexes of activity are supposed to result from the excitation of Rossby vortices within a thin layer beneath the convection zone. Numerical simulations demonstrate that Rossby vortices generate large-scale arc-like magnetic structures. It is shown that the most powerful complex of activity observed in June-July 1982 was likely to be a result of the excitation of a Rossby anticyclone rather than a cyclone. 相似文献
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A Rossby vortex was used to simulate the travelling of a large-scale magnetic structure across the equator. This process is reflected in the drift of the longitudinally averaged vertical component of the magnetic field and in the formation of distinct rotation periods of the nonaxisymmetric components in different latitude belts similar to the ones revealed from experimental data. 相似文献
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In the traditional axisymmetric models of the 11-year solar cycle, oscillations of the magnetic fields appear in the background of nonoscillating (over time scale considered) turbulent velocity fields and differential rotation. In this paper, an alternative approach is developed: The excitation of magnetic oscillations with the 22-year period is the consequence of hydrodynamic oscillations with the 11-year period. In the excitation of hydrodynamic oscillations, two processes taking place in high latitudes near the interface between the convective and radiative zones play a key role. One is forcing of the westerly zonal flow, the conditions for which are due to deformation of the interfacial surface. The other process is the excitation of a shear instability of zonal flow as a consequence of a strong radial gradient of angular velocity. The development of a shear instability at some stage brings about the disruption of the forcing of differential rotation. In the first (hydrodynamic) part of the paper, the dynamics of axisymmetric flows near the bottom of the convection zone is numerically simulated. Forcing of differential rotation having velocity shear in latitude and the existence of solutions in the form of torsional waves with the 11-year oscillation period are shown. In the second part the dynamics of the magnetic field is studied. The most pronounced peculiarities of the solutions are the existence of forced oscillations with the 22-year period and the drift of the toroidal magnetic field component from the mid latitudes to the equator. In high and low latitudes after cycle maximum, the toroidal component is of opposite sign in accordance with observations. In the third part, the transport of momentum from the bottom of the convection zone to the outer surface by virtue of diffusivity is considered. The existence of some sources of differential rotation in the convection zone is not implied. A qualitative correspondence of the differential rotation profile in the bulk of the convection zone and on its outer surface to experimental data is shown. The time correspondence between torsional and magnetic oscillations is also in accordance with observations. 相似文献
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E. Tikhomolov 《Solar physics》1995,156(2):205-219
A numerical simulation of the process of generation of the magnetic field by Rossby vortices, whose horizontal scale is comparable to the solar radius, has been carried out. Long-lived vortices form global magnetic structures that drift together with vortices. Differential rotation in latitude leads to a longer lifetime of cyclones and corresponding magnetic structures. The cyclone and the magnetic structure travel in longitude with the velocity close to a corresponding differential rotation velocity and drift slowly poleward. The interaction of cyclones located in close latitudes makes one of them move to higher latitudes and the poloidal component of the magnetic field to intensify during the interaction.The formation of large-scale vortices was simulated, when the initial condition was specified by a grid of small-scale vortices with a random amplitude distribution. Merging of vortices of the same sign leads to the formation of large-scale vortices whose size is determined by the geometry of the problem and by the differential rotation profile. 相似文献
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We study some peculiarities of the time variation of dipole components in the longitudinal field distribution in individual low-latitude belts of the Sun. For analyzing the horizontal dipole rotation and variations of amplitudes we used magnetic and H data.From 1979 to 1981 the rotation of the dipoles of the northern and southern low-latitude belts (0°–30° N and 10°–40° S) occurs with periods of about 26.8 days (N) and 28.2 days (S), in agreement with the results reported by Antonucci, Hoeksema, and Scherrer (1990) and Hoeksema and Scherrer (1987). A uniform rotation of the low-latitude dipoles of these belts continued until the end of 1981. Following the next coincidence of the magnetic poles in longitude the dipoles change in their rotation character. During about 15–20 rotations the low-latitude dipoles co-rotate with a new period close to the Carrington period. This is followed by a rapid (in 3–5 rotations) transition of the poles to a new stable state, also with the Carrington rotation period. The change in rotation and dynamics of the low-latitude dipoles at the end of 1981-beginning of 1982 can be explained either by a mutual penetration of the fields of different hemispheres to the opposite hemisphere or by the onset of the formation of relatively shortlived (15–20 rotations) structures which cover the entire low-latitude belt.Unlike the trajectories of the poles, the dipole amplitudes of the low-latitude belts showed a significant variability. However, simultaneous increases of the amplitudes in both hemispheres correlated with times at which the dipole poles coincide in longitude, and the greatest increase corresponded to the moment of merging of the dipole poles early in 1982. This suggests that sources of large-scale structures of the background field in the low-latitude belts of the Sun or the related fields interacted when the dipole poles coincided. 相似文献
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The evolution of the large‐scale component of the magnetic field generated by an ensemble of Rossby vortices is numerically simulated. The distribution of the Rossby vortices excited at the beginning of each Carrington rotation is determined from the analysis of Kitt Peak synoptic maps. Our model also considers 11‐year hydrodynamic and 22‐year magnetic field oscillations. In the vicinity of the Rossby vortices, the toroidal magnetic field is significantly amplified and the sign of the angle between the rope of the field lines and the equator is in accordance with observations for “normal” sunspots. We also suggest the possibility of the interpretation by our model of “abnormal” sunspot phenomena. We find that an inverse cascade, namely, the merging of Rossby vortices, gives rise to the formation of large‐scale hydrodynamic structures with a life‐time on the order of a solar cycle period. We conclude from this that the formation of such structures can thus explain the appearance of long‐lived, large‐scale component in the distribution of the magnetic field. 相似文献
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