Parameterizing Submesoscale Vertical Buoyancy Flux by Simultaneously Considering Baroclinic Instability and Strain‐Induced Frontogenesis
Abstract Oceanic submesoscale processes (submesoscales) with O(1–10) km horizontal scale can generate strong vertical buoyancy flux (VBF) that significantly modulate upper‐ocean stratification. Because submesoscales cannot be resolved by the prevailing ocean models, their VBFs have to be properly pa...
| Prif Awduron: | , , |
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| Fformat: | Erthygl |
| Iaith: | English |
| Cyhoeddwyd: |
Wiley
2023-04-01
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| Cyfres: | Geophysical Research Letters |
| Pynciau: | |
| Mynediad Ar-lein: | https://doi.org/10.1029/2022GL102292 |