Topographic Effects in Stratified FlowsCambridge University Press, 1998 - 500 pages With an emphasis on both theory and experiment, this text describes the behaviour of homogeneous and density-stratified fluids over and around topography. In examining the similarities between the flow of a river over a barrier or weir and the flow of the atmosphere over a mountain range, this book presents a comprehensive synthesis of this topic in terms suitable for scientists, engineers, teachers and students of fluid dynamics. With this book, Professor Baines makes a notable contribution to the fields of fluid mechanics and geophysical fluid dynamics. The text will be a great asset to graduate and advanced undergraduate students, as well as to research professionals. |
Contents
The flow of a homogeneous layer with a free surface | 17 |
Twolayer flows | 93 |
Waves in stratified fluids | 164 |
Stratified flow over twodimensional obstacles | 224 |
flows | 316 |
Stratified flow past threedimensional topography | 344 |
Applications to practical modelling of flow over complex | 448 |
Appendix | 463 |
479 | |
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Common terms and phrases
amplitude approximately Atmos Baines boundary condition Boussinesq approximation columnar constant critical layer critical level curve d₁ decreases denote density depth described in section diagram displacement downstream side drag effects equations finite flow past flow pattern Fluid Mech flux Froude number given gravity waves group velocity height horizontal hydraulic jump hydrostatic flow implies increases infinite-depth interface internal wave inviscid lee waves Long's-model lower boundary maximum mean flow Nh/U non-linear observed obstacle crest obstacle shape obtained occurs perturbation plane potential flow r₁ region Reynolds number shear shown in Figure shows single layer solution stagnation point stationary stratified flow stratified fluid stream streamline subcritical subcritical flow supercritical supercritical flow surface three-dimensional topography turbulent two-dimensional two-layer u₁ uniform unstable upper boundary upstream disturbance upstream side values vertical wake wave drag wave energy wave speeds wavenumber wavetrain Witch of Agnesi zero