Verification of a 1-dimensional surf prediction model for steep beach conditions
Wave breaking is the only source of energy dissipation in the Battjes and Janssen (1978) wave transformation model, which is parameterized by a breaking wave parameter, Y. The Battjes and Janssen (1978) wave transformation model was calibrated by Battjes and Stive (1985) and the calibration was refi...
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Monterey, California. Naval Postgraduate School
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ndltd-nps.edu-oai-calhoun.nps.edu-10945-59402015-02-04T03:55:39Z Verification of a 1-dimensional surf prediction model for steep beach conditions Cutshaw, Charles Q. Thornton, Edward B. Reniers, Ad Wave breaking is the only source of energy dissipation in the Battjes and Janssen (1978) wave transformation model, which is parameterized by a breaking wave parameter, Y. The Battjes and Janssen (1978) wave transformation model was calibrated by Battjes and Stive (1985) and the calibration was refined by Morris et al. (2001) for waves over shallow sloping beaches. The objective of this study was to further refine the calibration to include steep beaches for a range of wave conditions by analyzing data from a nearshore experiment at Sand City, California. Waves were measured by a cross-shore array of nine pressure sensors. The pressure data were analyzed for Hrms and compared with calculated Hrms by the model. Results were largely inconclusive, which is attributed to wave reflection from the steep beach, something not accounted for in the model. Excluding data collected at low tides and allowing the model to account for reflection would likely reveal a more interesting outcome. 2012-03-14T17:47:15Z 2012-03-14T17:47:15Z 2002-06 Thesis http://hdl.handle.net/10945/5940 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, it may not be copyrighted. Monterey, California. Naval Postgraduate School |
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Wave breaking is the only source of energy dissipation in the Battjes and Janssen (1978) wave transformation model, which is parameterized by a breaking wave parameter, Y. The Battjes and Janssen (1978) wave transformation model was calibrated by Battjes and Stive (1985) and the calibration was refined by Morris et al. (2001) for waves over shallow sloping beaches. The objective of this study was to further refine the calibration to include steep beaches for a range of wave conditions by analyzing data from a nearshore experiment at Sand City, California. Waves were measured by a cross-shore array of nine pressure sensors. The pressure data were analyzed for Hrms and compared with calculated Hrms by the model. Results were largely inconclusive, which is attributed to wave reflection from the steep beach, something not accounted for in the model. Excluding data collected at low tides and allowing the model to account for reflection would likely reveal a more interesting outcome. |
author2 |
Thornton, Edward B. |
author_facet |
Thornton, Edward B. Cutshaw, Charles Q. |
author |
Cutshaw, Charles Q. |
spellingShingle |
Cutshaw, Charles Q. Verification of a 1-dimensional surf prediction model for steep beach conditions |
author_sort |
Cutshaw, Charles Q. |
title |
Verification of a 1-dimensional surf prediction model for steep beach conditions |
title_short |
Verification of a 1-dimensional surf prediction model for steep beach conditions |
title_full |
Verification of a 1-dimensional surf prediction model for steep beach conditions |
title_fullStr |
Verification of a 1-dimensional surf prediction model for steep beach conditions |
title_full_unstemmed |
Verification of a 1-dimensional surf prediction model for steep beach conditions |
title_sort |
verification of a 1-dimensional surf prediction model for steep beach conditions |
publisher |
Monterey, California. Naval Postgraduate School |
publishDate |
2012 |
url |
http://hdl.handle.net/10945/5940 |
work_keys_str_mv |
AT cutshawcharlesq verificationofa1dimensionalsurfpredictionmodelforsteepbeachconditions |
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1716730090889412608 |