Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows
We analyze surface waves generated by a translating, oscillating surface disturbance atop a horizontal background flow of arbitrary depth dependence, with a focus on determining the Doppler resonance. For a critical value of the dimensionless frequency τ = ωV/g (ω: oscillation frequency, V: source v...
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ftntnutrondheimi:oai:ntnuopen.ntnu.no:11250/2585675 2023-05-15T14:23:51+02:00 Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows Li, Yan Ellingsen, Simen Andreas Ådnøy 2018 http://hdl.handle.net/11250/2585675 https://doi.org/10.1115/OMAE2018-78560 eng eng ASME ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering - Volume 7B: Ocean Engineering urn:isbn:978-0-7918-5127-2 http://hdl.handle.net/11250/2585675 https://doi.org/10.1115/OMAE2018-78560 cristin:1633605 V07BT06A056-? Chapter 2018 ftntnutrondheimi https://doi.org/10.1115/OMAE2018-78560 2019-09-17T06:54:31Z We analyze surface waves generated by a translating, oscillating surface disturbance atop a horizontal background flow of arbitrary depth dependence, with a focus on determining the Doppler resonance. For a critical value of the dimensionless frequency τ = ωV/g (ω: oscillation frequency, V: source velocity, g: gravitational acceleration) at which generated waves cannot escape. In the absence of shear the resonant value is famously 1/4; the presence of a shear current modifies this. We derive the theoretical and numerical tools for studying this problem, and present the first calculation of the Doppler resonance for a source atop a real, measured shear current to our knowledge. Studying graphical solutions to the (numerically obtained) dispersion relation allows derivation of criteria determining the number of far-field waves that exist in different sectors of propagation directions, from which the criteria for Doppler resonance follow. As example flows we study a typical wind-driven current, and a current measured in the Columbia River estuary. We show that modeling these currents as uniform or with a linear depth dependence based on surface measures may lead to large discrepancies, in particular for long and moderate wavelengths. publishedVersion Copyright © 2018 by ASME Book Part Arctic NTNU Open Archive (Norwegian University of Science and Technology) Volume 7B: Ocean Engineering |
institution |
Open Polar |
collection |
NTNU Open Archive (Norwegian University of Science and Technology) |
op_collection_id |
ftntnutrondheimi |
language |
English |
description |
We analyze surface waves generated by a translating, oscillating surface disturbance atop a horizontal background flow of arbitrary depth dependence, with a focus on determining the Doppler resonance. For a critical value of the dimensionless frequency τ = ωV/g (ω: oscillation frequency, V: source velocity, g: gravitational acceleration) at which generated waves cannot escape. In the absence of shear the resonant value is famously 1/4; the presence of a shear current modifies this. We derive the theoretical and numerical tools for studying this problem, and present the first calculation of the Doppler resonance for a source atop a real, measured shear current to our knowledge. Studying graphical solutions to the (numerically obtained) dispersion relation allows derivation of criteria determining the number of far-field waves that exist in different sectors of propagation directions, from which the criteria for Doppler resonance follow. As example flows we study a typical wind-driven current, and a current measured in the Columbia River estuary. We show that modeling these currents as uniform or with a linear depth dependence based on surface measures may lead to large discrepancies, in particular for long and moderate wavelengths. publishedVersion Copyright © 2018 by ASME |
format |
Book Part |
author |
Li, Yan Ellingsen, Simen Andreas Ådnøy |
spellingShingle |
Li, Yan Ellingsen, Simen Andreas Ådnøy Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
author_facet |
Li, Yan Ellingsen, Simen Andreas Ådnøy |
author_sort |
Li, Yan |
title |
Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
title_short |
Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
title_full |
Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
title_fullStr |
Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
title_full_unstemmed |
Surface Waves Generated by a Translating and Oscillating Source Atop Realistic Shear Flows |
title_sort |
surface waves generated by a translating and oscillating source atop realistic shear flows |
publisher |
ASME |
publishDate |
2018 |
url |
http://hdl.handle.net/11250/2585675 https://doi.org/10.1115/OMAE2018-78560 |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
V07BT06A056-? |
op_relation |
ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering - Volume 7B: Ocean Engineering urn:isbn:978-0-7918-5127-2 http://hdl.handle.net/11250/2585675 https://doi.org/10.1115/OMAE2018-78560 cristin:1633605 |
op_doi |
https://doi.org/10.1115/OMAE2018-78560 |
container_title |
Volume 7B: Ocean Engineering |
_version_ |
1766296323999399936 |