On the inadequacies of Long's model for steady two-dimensional stratified flows

DOI10.1080/03091920310001630001zbMath1206.86018OpenAlexW2101386961MaRDI QIDQ3080158

Bhimsen K. Shivamoggi, David K. Rollins

Publication date: 5 March 2011

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091920310001630001

zbMATH Keywords

topographyupstream influenceLong's model

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Stratification effects in inviscid fluids (76B70)

Related Items (1)

On symmetric intrusions in a linearly stratified ambient: a revisit of Benjamin's steady-state propagation results

Cites Work

• On steady laminar flow with closed streamlines at large Reynolds number
• Exact solutions for steady two-dimensional flow of a stratified fluid
• Selective withdrawal from stratified streams
• A study of the motion of a cavity in a rotating liquid
• A free-streamline solution for stratified flow into a line sink
• The time-dependent motion due to a cylinder moving in an unbounded rotating or stratified fluid
• Steady two-dimensional flow of fluid of variable density over an obstacle
• On wakes in stratified fluids
• The two-dimensional flow of a stratified fluid over an obstacle
• Upstream influence
• On Long's hypothesis of no upstream influence in uniformly stratified or rotating flow
• Rotating and stratified fluid flow
• A study of motions in a rotating liquid

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