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

Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell (Q5876585)

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scientific article; zbMATH DE number 7648577
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Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell
scientific article; zbMATH DE number 7648577

    Statements

    Retrograde equatorial surface flows generated by thermal convection confined under a stably stratified layer in a rapidly rotating spherical shell (English)
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    1 February 2023
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    mean zonal flows
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    stably stratified layer
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    angular momentum budget
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    viscous diffusion
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