## Topographic Effects in Stratified FlowsWith an emphasis on both theory and experiment, this text describes the behavior of homogeneous and density-stratified fluids over and around topography. The topics include the flow of a homogeneous layer with a free surface--the prototype for conventional hydraulics--the corresponding phenomena in two-layer flows, and a description of the properties of linear waves in stratified fluids in motion. The author applies the aforementioned properties to laboratory and numerical modeling of flow through real complex terrain. |

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### Contents

The flow of a homogeneous layer with a free surface | 17 |

Stratified flow over twodimensional obstacles | 224 |

flows | 316 |

Applications to practical modelling of flow over complex | 448 |

Appendix | 463 |

479 | |

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amplitude applies approximately assume becomes bore boundary cause Chapter complex constant continuous corresponding crest critical curve decreases defined denote density depends depth described direction discussed displacement disturbance downstream drag effects energy equations example experiments expressed field finite flow fluid flux forcing function further given gives height Hence horizontal hydraulic jump hydrostatic implies increases initial instability integral interface internal jump lateral layer limit linear lower maximum mean mode motion moving Nh/U non-linear observed obstacle obtained occurs past pattern perturbation plane possible pressure propagating properties range region relative represented scale separation shape shown in Figure shows side similar situation solution speed stationary steady stratified stream streamline studies supercritical surface theory tion topography two-dimensional uniform upper upstream values varies velocity vertical wake wave zero