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Carlowen A. Smith, Kevin G. Speer, and Ross W. Griffiths

experiments are strongly influenced by bottom slope in their sense (that the value of the parameter be of order unity) and we note that ocean values are near unity as well. The primitive equation simulations of cooling around an island conducted by Spall (2013) bear a striking resemblance to the geometry of the present work and also show spontaneous generation of azimuthal jets. We also point to many previous laboratory experiments demonstrating qualitative analogs to the planetary β effect in

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