Blob Instability In Rotating Compositional Convection
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Blob instability in rotating compositional convection
Blob instability in rotating compositional convection Sabine ClaBen and Moritz Heimpel I and Ulrich Christensen Institut fiir C. eophysik, C. eorg-August Universitiit, C. Sttingen, C. ermany Abstract. The onset and structure of compositional con- vection in a rotating system are investigated experimen- tally.
The anisotropy of local turbulence in the Earth s core
Earth Planets Space, 51, 277 286, 1999 The anisotropy of local turbulence in the Earth s core Masaki Matsushima∗, Takahiro Nakajima∗∗, and Paul H. Roberts Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, U.S.A.
One of the distinguishing features of mixing in the ocean is
Such a compositional gradient hampers large-scale convection that turns into double-diffusive convection, yielding an inner thermal profile that departs from the Oscillatory double diffusive convection (oddc) is a double diffusive instability that occurs in fluids that are unstably stratified in temperature and stably stratified