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Open-File Report 2015–1055

Effects of Proposed Sediment Borrow Pits on Nearshore Wave Climate and Longshore Sediment Transport Rate Along Breton Island, Louisiana

Citation | List of Figures | List of Tables | Conversion Factors | Abbreviations | Abstract | Introduction | Methods | Results | Conclusions | Acknowledgments | References Cited | Appendix 1. Scenarios | Appendix 2. Example Model Input Files | Appendix 3. File Naming Conventions | Digital Data Files


Figure 4. Grid G4 showing grid of 135 crossshore transects.
Figure 4. Portion of G4 showing the 135 cross-shore transects (in black) used in calculating the alongshore flux. Alongshore flux was calculated using wave height and direction at the most offshore point along each transect where the depth-induced wave breaking dissipation exceeded 0.01 watt per square meter. If this threshold was exceeded offshore of the island platform (defined as the 4 m contour, shown in purple), values at the 4 m contour were used instead. [m, meters]

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