article · Journal of Geophysical Research Atmospheres · 1998
A mechanism for layer formation in stratified geophysical flows
Josep Lluís Pelegrí, Pablo Sangrà
Cited by 31Abstract and details only
Abstract
We discuss the possibility that steplike structures are formed in subcritical regions of vertically stratified shear flow. The mechanism we propose essentially consists of localized intense mixing in highly stratified and sheared flows, probably following frontogenesis. Its main assumption is that the vertical density flux increases monotonically with decreasing gradient Richardson numbers, which corresponds to enhanced stratification and/or diapycnal shear. This differs from Phillips' [1972] mechanism, which we argue may not apply to vertically stratified shear flow. An essential condition for the formation of constant density steps is the incorporation of a Langevin type equation which takes into account that turbulence must last for some finite characteristic time. We present numerical computations for the case of approximately constant diapycnal shear which lead to the formation of a staircase depth‐density structure.
Cite this paper
Pelegrí, J. L., & Sangrà, P. (1998). A mechanism for layer formation in stratified geophysical flows. Journal of Geophysical Research Atmospheres, 103(C13), 30679–30693. https://doi.org/10.1029/98jc01627
Pelegrí, Josep Lluís, and Pablo Sangrà. “A mechanism for layer formation in stratified geophysical flows.” Journal of Geophysical Research Atmospheres, vol. 103, no. C13, 1998, pp. 30679–93, https://doi.org/10.1029/98jc01627.
Pelegrí, Josep Lluís, and Pablo Sangrà. 1998. “A mechanism for layer formation in stratified geophysical flows.” Journal of Geophysical Research Atmospheres 103 (C13): 30679–93. https://doi.org/10.1029/98jc01627.
Pelegrí, J.L. and Sangrà, P. (1998) ‘A mechanism for layer formation in stratified geophysical flows’, Journal of Geophysical Research Atmospheres, 103(C13), pp. 30679–30693. Available at: https://doi.org/10.1029/98jc01627.
@article{pelegri1998mechanism,
title = {{A mechanism for layer formation in stratified geophysical flows}},
author = {Pelegrí, Josep Lluís and Sangrà, Pablo},
journal = {Journal of Geophysical Research Atmospheres},
volume = {103},
number = {C13},
pages = {30679--30693},
year = {1998},
doi = {10.1029/98jc01627}
}Made from the index record. Check names, capitalisation and page numbers against the paper. Need another style? AI for Research has over 10,000.
Related papers
Turbulent disruption of density staircases in stratified shear flows
Nicolaos Petropoulos, Ali Mashayek, Colm-cille P. Caulfield · Journal of Fluid Mechanics · 2023
Cited by 6Open access
Experiments on high Richardson number instability of a rotating stratified shear flow
Jack Calman · Dynamics of Atmospheres and Oceans · 1977
Cited by 22
Laboratory Modeling of the Transformation of Linearly Stratified Fluid into Steplike Stratified Fluid under Vertically Uniform Turbulent Stirring
V. V. Gerasimov, Andrey Georgievich Zatsepin · Oceanology · 2025
Cited by 1
The instability of stratified flows at large Richardson numbers
Andrew J. Madja, Michael G. Shefter · Proceedings of the National Academy of Sciences · 1998
Cited by 16Open access
Long-time evolution of density layers and interfaces in forced stably-stratified flows
Cocciaglia, Niccolo, Bonaccorso, Fabio, Alessandra Sabina Lanotte et al. · arXiv (Cornell University) · 2025
Cited by 1Open access
Modeling of shear-induced diapycnal mixing in frontal systems
Josep Lluís Pelegrí, Ángel Rodríguez-Santana, Pablo Sangrà et al. · Applied Scientific Research · 1997
Cited by 6
Mixing in a stably stratified shear layer: two- and three-dimensional numerical experiments
Chantal Staquet · Fluid Dynamics Research · 2000
Cited by 81Open access