Book contents
- Frontmatter
- Contents
- Preface
- 1 Introduction
- 2 Geomorphology
- 3 Sand Transport Pathways
- 4 Sand Transport and Sand Bypassing at Selected Inlets
- 5 Empirical Relationships
- 6 Tidal Inlet Hydrodynamics; Excluding Depth Variations with Tidal Stage
- 7 Tidal Inlet Hydrodynamics; Including Depth Variations with Tidal Stage
- 8 Cross-Sectional Stability of a Single Inlet System
- 9 Cross-Sectional Stability of a Double Inlet System, Assuming a Uniformly Varying Basin Water Level
- 10 Cross-Sectional Stability of a Double Inlet System, Assuming a Spatially Varying Basin Water Level
- 11 Morphodynamic Modeling of Tidal Inlets Using a Process-Based Simulation Model
- 12 Morphodynamic Modeling of Tidal Inlets Using an Empirical Model
- 13 River Flow and Entrance Stability
- 14 Engineering of Tidal Inlets
- References
- Index
1 - Introduction
Published online by Cambridge University Press: 04 July 2017
- Frontmatter
- Contents
- Preface
- 1 Introduction
- 2 Geomorphology
- 3 Sand Transport Pathways
- 4 Sand Transport and Sand Bypassing at Selected Inlets
- 5 Empirical Relationships
- 6 Tidal Inlet Hydrodynamics; Excluding Depth Variations with Tidal Stage
- 7 Tidal Inlet Hydrodynamics; Including Depth Variations with Tidal Stage
- 8 Cross-Sectional Stability of a Single Inlet System
- 9 Cross-Sectional Stability of a Double Inlet System, Assuming a Uniformly Varying Basin Water Level
- 10 Cross-Sectional Stability of a Double Inlet System, Assuming a Spatially Varying Basin Water Level
- 11 Morphodynamic Modeling of Tidal Inlets Using a Process-Based Simulation Model
- 12 Morphodynamic Modeling of Tidal Inlets Using an Empirical Model
- 13 River Flow and Entrance Stability
- 14 Engineering of Tidal Inlets
- References
- Index
Summary
In the context of this book, tidal inlets are defined as the relatively short and narrow passages between barrier islands. They are sometimes referred to as passes or cuts. Tidal inlets are a common occurrence as barrier island coasts cover some 10 percent of the world's coasts (Glaeser, 1978). According to Hayes (1979), their presence is limited to coasts where the tidal range is less than 4 m.
The earliest interest in tidal inlets originates from their importance to commercial shipping. The relatively protected back-barrier lagoons were a favorite location for harbors. Later, with the increase in recreational boating, small boat basins and marinas were located in back-barrier lagoons. In addition to these commercial and recreational aspects, tidal inlets are ecologically important. Through the exchange of lagoon and ocean water, they contribute to the increase of water quality in the lagoon. Unfortunately, there is also a downside: tidal inlets interrupt the flow of sand along the coast. They not only interrupt but also capture part of the sand, causing erosion of the downdrift coast. For example, in Florida, with some eighty inlets, much of the beach erosion has been attributed to tidal inlets.
Most natural tidal inlets are less than ideal from a navigational point of view. The many shoals, the strong tidal current and the exposure to ocean waves make entering difficult. In addition, on timescales of years to decades, the morphology shows considerable variation, and maintaining sufficient depth and alignment of the channels requires substantial dredging. To minimize dredging and to improve navigation conditions, many inlets have been modified by adding jetties and breakwaters. As a result, tidal currents, waves and sand transport pathways differ from those at inlets without these structures. Nevertheless, in this book, emphasis is on tidal inlets that have not been modified. The reasoning is that understanding the physical processes governing the behavior of tidal inlets in a natural state is a prerequisite for the proper design of engineering measures. This includes the determination of undesirable side effects such as erosion of the adjacent beaches.
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- Information
- Tidal InletsHydrodynamics and Morphodynamics, pp. 1 - 5Publisher: Cambridge University PressPrint publication year: 2017