Wave Reflection and Transmission in Channels of Gradually Varying Depth

Prepared Under Contract from Fluid Dynamics Branch Office of Naval Research Department of the Navy , Contract no. Nonr-1841(59)

Bibliographic Details
Main Authors: Ippen, A. T., Alam, A. M. Z., Bourodimos, E. L.
Published: Cambridge, Mass. : Massachusetts Institute of Technology, Hydrodynamics Laboratory, Department of Civil Engineering 2022
Online Access:https://hdl.handle.net/1721.1/143055
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author Ippen, A. T.
Alam, A. M. Z.
Bourodimos, E. L.
author_facet Ippen, A. T.
Alam, A. M. Z.
Bourodimos, E. L.
author_sort Ippen, A. T.
collection MIT
description Prepared Under Contract from Fluid Dynamics Branch Office of Naval Research Department of the Navy , Contract no. Nonr-1841(59)
first_indexed 2024-09-23T13:09:53Z
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institution Massachusetts Institute of Technology
last_indexed 2024-09-23T13:09:53Z
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publisher Cambridge, Mass. : Massachusetts Institute of Technology, Hydrodynamics Laboratory, Department of Civil Engineering
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spelling mit-1721.1/1430552022-06-14T03:22:01Z Wave Reflection and Transmission in Channels of Gradually Varying Depth Ippen, A. T. Alam, A. M. Z. Bourodimos, E. L. Prepared Under Contract from Fluid Dynamics Branch Office of Naval Research Department of the Navy , Contract no. Nonr-1841(59) This report presents the results of a study on the reflection and transmission of water waves in a rectangular channel with transitions of linearly varying depths. Two channel sections of uniform depths are joined by sections of slopes 1:0.58, 1:2.75 and 1:16 in the three sets of experiments. Wave conditions were systematically varied to cover the range of deep-water to shallow-water waves in the deeper approach channel. The pertinent parameters considered for each slope were relative depth (ratio of upstream to downstream depth), ratio of group velocities and wave steepness. Since a comprehensive theory does not exist, the classical small wave amplitude theory for abrupt transitions was employed to correlate the results of the study. Comparisons with other theories developed recently were made where applicable. Some of the important conclusions are: 1. For short and intermediate waves reflection coefficients become generally larger than predicted as the slope of the transition decreases. 2. For short and intermediate waves transmission coefficients generally agree with predictions for group velocity ratios near unity, but tend to lower values for lower ratios of group velocity as the slope of the transition decreases. 3. For short and intermediate waves wave steepness has a relatively small influence on reflection and transmission coefficients. 4. For shallow water waves the reflection coefficients were found independent of relative depth ratios contrary to prediction but decreased markedly with increasing wave steepness for the smallest slope. 5. For shallow water waves the transmission coefficients followed the predicted trend, but became relatively lower for increasing relative depth ratios. Increasing wave steepness had the effect of increasing the transmission coefficients for the smallest slope. 2022-06-13T13:12:49Z 2022-06-13T13:12:49Z 1964-07 72 https://hdl.handle.net/1721.1/143055 13898578 247792 R (Massachusetts Institute of Technology. Department of Civil Engineering) ; 64-31. Report (Massachusetts Institute of Technology. Hydrodynamics Laboratory) ; no. 72. application/pdf Cambridge, Mass. : Massachusetts Institute of Technology, Hydrodynamics Laboratory, Department of Civil Engineering
spellingShingle Ippen, A. T.
Alam, A. M. Z.
Bourodimos, E. L.
Wave Reflection and Transmission in Channels of Gradually Varying Depth
title Wave Reflection and Transmission in Channels of Gradually Varying Depth
title_full Wave Reflection and Transmission in Channels of Gradually Varying Depth
title_fullStr Wave Reflection and Transmission in Channels of Gradually Varying Depth
title_full_unstemmed Wave Reflection and Transmission in Channels of Gradually Varying Depth
title_short Wave Reflection and Transmission in Channels of Gradually Varying Depth
title_sort wave reflection and transmission in channels of gradually varying depth
url https://hdl.handle.net/1721.1/143055
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