Thermohaline interleaving induced by horizontal temperature and salinity gradients from above

نویسندگان

چکیده

In the Ocean, thermohaline intrusions and interleaving layers occur within water mass fronts with horizontal temperature salinity gradients, which provide an important mixing mechanism. Here we report a new type of intrusion is driven by gradients in fluid at adjacent depths due to different double diffusive rates vertical direction. Once established, share similar behaviors as those found gradient regions. Such process generates extra heat fluxes towards cold fresh side, but transfer density anomaly warm salty side. These findings greatly extend circumstance where may be observed.

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ژورنال

عنوان ژورنال: Journal of Fluid Mechanics

سال: 2021

ISSN: ['0022-1120', '1469-7645']

DOI: https://doi.org/10.1017/jfm.2021.753