Gravity wave generation in balanced sheared flow revisited
نویسندگان
چکیده
Abstract The generation of internal gravity waves from an initially geostrophically balanced flow is diagnosed in nonhydrostatic numerical simulations shear instabilities for varied dynamical regimes. A nonlinear decomposition method up to third order the Rossby number (Ro) used as diagnostic tool a consistent separation and unbalanced motions presence their coupling. Wave emission investigated Eady-like jet-like flow. For case, geostrophic ageostrophic unstable modes are initialize different simulations. Gravity wave general very weak over range values Ro. At sufficiently high Ro, however, when condition symmetric instability satisfied with negative local potential vorticity, significant detected even at lowest order. This related occurrence fast modes, generating wide spectrum waves. Thus, excited mode only if obtain finite growth rates. Significance Statement We aim understand atmosphere ocean field that balanced, i.e., free any To examine this process, we use idealized models identify Our results show prominent mechanism by which can be generated or possibly occurring during frontogenesis. process dissipate energy ocean.
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ژورنال
عنوان ژورنال: Journal of Physical Oceanography
سال: 2022
ISSN: ['1520-0485', '0022-3670']
DOI: https://doi.org/10.1175/jpo-d-21-0115.1