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Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
Baroclinic, geostrophic turbulence is random, chaotic flow characterized by significant vertical gradients in density (Bu << 1) in which rotation plays a major role (Ro << 1). In the presence of a large-scale background gradient of...
Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
