caa a22 4500 469104902 CHVBK 20180323133054.0 cr unu---uuuuu 170328e19920601xx s 000 0 eng 10.1007/BF01614125 doi (NATIONALLICENCE)springer-10.1007/BF01614125 Boďa Ján Department of Geophysics, Comenius University, Czechoslovakia aut Linear hydromagnetic stability of a differentially rotating non-uniformly stratified fluid layer [Elektronische Daten] [Ján Boďa] Summary: Our discussion is concerned with the common effect of the non-uniformity of layer rotation and stratification. We have assumed a model of differential rotation with the upper part of the layer rotating more slowly, the bottom part more quickly. The upper part of the layer is stratified stably, the bottom part unstably. The thermal instabilities are preferred in the strong differential rotation case and they are the most easily excited by a strong magnetic field (Λ⋍102−103). The direction of its propagation is westward in the uniformly stratified layer and eastward in the non-uniformly stratified layer. Academia, Publishing House of the Czechoslorak Academy of Sciences, 1992 Studia Geophysica et Geodaetica Kluwer Academic Publishers 36/2(1992-06-01), 139-150 0039-3169 36:2<139 1992 36 11200 https://doi.org/10.1007/BF01614125 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF01614125 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Boďa Ján Department of Geophysics, Comenius University, Czechoslovakia aut NATIONALLICENCE 773 0- Studia Geophysica et Geodaetica Kluwer Academic Publishers 36/2(1992-06-01), 139-150 0039-3169 36:2<139 1992 36 11200 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer