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- W2042226677 abstract "This study investigates the reason why the barotropic vorticity structure prevails vertically in response to the enhanced convection associated with the boreal summer intraseasonal oscillation over the central Indian Ocean. The relative vorticity tendency analysis for a 2.5-layer simplified model demonstrates that the barotopic vorticity structure is predominant due to the following two factors: 1) vertical easterly shear on the meridional gradient of barotropic divergence (which induces generation of barotropic vorticity twice larger than that of baroclinic vorticity); and 2) vertical easterly shear on the meridional gradient of baroclinic divergence (which appears only in relation to the generation of barotropic vorticity). The percentage of contribution by each term to barotropic and baroclinic vorticity tendency equations is presented." @default.
- W2042226677 created "2016-06-24" @default.
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- W2042226677 date "2012-06-30" @default.
- W2042226677 modified "2023-09-26" @default.
- W2042226677 title "Vertical Vorticity Structure Associated with the Boreal Summer Intraseasonal Oscillation: Barotropic or Baroclinic?" @default.
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- W2042226677 doi "https://doi.org/10.14191/atmos.2012.22.2.259" @default.
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