Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell

Details Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell

Feb 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011gapfd.105...61t&link_type=ejournal

Geophysical & Astrophysical Fluid Dynamics, vol. 105, issue 1, pp. 61-81

Physics

Fluid Dynamics

2

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