In order to improve the predictive abilities of weather and climate models, it is essential to understand the behaviour of wind stress at the ocean surface. Wind stress is contingent on small-scale interfacial dynamics typically not directly resolved in numerical models. Although skin friction contributes considerably to the total stress up to moderate wind speeds, it is notoriously challenging to measure and predict using physics-based approaches. This work proposes a supervised machine learning (ML) model that estimates the spatial distribution of the skin-friction drag over wind waves using solely wave elevation and wave age, which are relatively easy to acquire. The input–output pairs are high-resolution wave profiles and their corresponding surface viscous stresses collected from laboratory experiments. The ML model is built upon a convolutional neural network architecture that incorporates the Mish nonlinearity as its activation function. Results show that the model can accurately predict the overall distribution of viscous stresses; it captures the peak of viscous stress at/near the crest and its dramatic drop to almost null just past the crest in cases of intermittent airflow separation. The predicted area-aggregate skin friction is also in excellent agreement with the corresponding measurements. The proposed method offers a practical pathway for estimating both local and area-aggregate skin friction and can be easily integrated into existing numerical models for the study of air–sea interactions.
more »
« less
Data-driven met-ocean model for offshore wind energy applications
In recent years, the global transition towards green energy, driven by environmental concerns and increasing electricity demands, has remarkably reshaped the energy landscape. The transformative potential of marine wind energy is particularly critical in securing a sustainable energy future. To achieve this objective, it is essential to have an accurate understanding of wind dynamics and their interactions with ocean waves for the proper design and operation of offshore wind turbines (OWTs). The accuracy of met-ocean models depends critically on their ability to correctly capture sea-surface drag over the multiscale ocean surface—a quantity typically not directly resolved in numerical models and challenging to acquire using either field or laboratory measurements. Although skin friction drag contributes considerably to the total wind stress, especially at moderate wind speeds, it is notoriously challenging to predict using physics-based approaches. The current work introduces a novel approach based on a convolutional neural network (CNN) model to predict the spatial distributions of skin friction drag over wind-generated surface waves using wave profiles, local wave slopes, local wave phases, and the scaled wind speed. The CNN model is trained using a set of high-resolution laboratory measurements of air-side velocity fields and their respective surface viscous stresses obtained over a range of wind-wave conditions. The results demonstrate the capability of our model to accurately estimate both the instantaneous and area-aggregate viscous stresses for unseen wind-wave regimes. The proposed CNN-based wall-layer model offers a viable pathway for estimating the local and averaged skin friction drag in met-ocean simulations.
more »
« less
- Award ID(s):
- 2404368
- PAR ID:
- 10575931
- Publisher / Repository:
- IOP Publishing
- Date Published:
- Journal Name:
- Journal of Physics: Conference Series
- Volume:
- 2767
- Issue:
- 5
- ISSN:
- 1742-6588
- Page Range / eLocation ID:
- 052005
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
More Like this
-
-
The small-scale physics within the first centimetres above the wavy air–sea interface are the gateway for transfers of momentum and scalars between the atmosphere and the ocean. We present an experimental investigation of the surface wind stress over laboratory wind-generated waves. Measurements were performed at the University of Delaware's large wind-wave-current facility using a recently developed state-of-the-art wind-wave imaging system. The system was deployed at a fetch of 22.7 m, with wind speeds from 2.19 to $$16.63\ \textrm {m}\ \textrm {s}^{-1}$$ . Airflow velocity fields were acquired using particle image velocimetry above the wind waves down to $$100\ \mathrm {\mu }\textrm {m}$$ above the surface, and wave profiles were detected using laser-induced fluorescence. The airflow intermittently separates downwind of wave crests, starting at wind speeds as low as $$2.19\ \textrm {m}\ \textrm {s}^{-1}$$ . Such events are accompanied by a dramatic drop in tangential viscous stress past the wave's crest, and a gradual regeneration of the viscous sublayer upon the following (downwind) crest. This contrasts with non-airflow separating waves, where the surface viscous stress drop is less significant. Airflow separation becomes increasingly dominant with increasing wind speed and wave slope $a k$ (where $$a$$ and $$k$$ are peak wave amplitude and wavenumber, respectively). At the highest wind speed ( $$16.63\ \textrm {m}\ \textrm {s}^{-1}$$ ), airflow separation occurs over nearly 100 % of the wave crests. The total air–water momentum flux is partitioned between viscous stress and form drag at the interface. Viscous stress (respectively form drag) dominates at low (respectively high) wave slopes. Tangential viscous forcing makes a minor contribution ( $${\sim }3\,\%$$ ) to wave growth.more » « less
-
Large‐scale offshore wind farms are expected to influence surface waves by modifying local wind forcing through wake effects. We use regional coupled ocean‐atmosphere‐wave model simulations to investigate a realistic large‐scale offshore wind development scenario in the northeastern U.S. during boreal summer. Near‐surface wind speeds are reduced by 10% over lease areas and within downstream wake regions, leading to decreases in significant wave height (3%) and wave‐supported momentum flux (30%). This further leads to reductions in surface roughness length (16%) and near‐surface ocean turbulent kinetic energy (20%). Spectral analysis shows a clear reduction in wind‐sea energy, indicating suppressed local wind‐wave growth near the wind farms. Weaker winds favor the development of longer‐period waves, increasing dominant wave phase speed by 3% and suggesting a transition to an older sea state. Modern bulk flux algorithms often parameterize surface roughness using inverse wave age and/or wave slope. This raises the question of whether wake‐driven reductions in inverse wave age and wave height impact air‐sea momentum exchange. To assess this, we compare fully coupled simulations with an atmosphere‐only run excluding wave coupling. Results show that about one‐third of the reduction in roughness length can be attributed to sea state changes, while two‐thirds result from lower friction velocity due to lower wind speeds. However, the impact of sea state on the drag coefficient and momentum flux is negligible (1%), suggesting that wake‐induced wind speed reductions are the primary driver, with sea state changes playing a secondary role.more » « less
-
This data is large eddy simulation model output of turbulent airflow over misaligned surfaces waves (up to 90 degrees) for strongly forced to weakly forced conditions (wave age up to 10.95) using a wave-following mapped coordinate, for the following manuscript: Manzella, E., Hara, T., Sullivan, P. Reduction of Drag Coefficient due to Misaligned Surface Waves. (Manuscript in preparation) From these data for wind aligned with waves (0 degrees) to wind misaligned with waves (22.5, 45, 67.5, 90 degrees) and wave age (c/u*=1.37, 5.48, 10.95) with corresponding variable names (1x, 4x, 8x) we look at equivalent roughness length and wave growth/decay variables. In addition to the cross-wave component of the velocity (v), we also include the rotated along-wind (U) and cross-wind (V) variables. We look at horizontally averaged vertical profiles of the following: -Wind speed, wind shear, wind speed angle, and wind shear angle -Turbulent kinetic energy -Energy budget (including shear production, transport, and viscous dissipation) -Momentum budget (including pressure stress, turbulent stress, and wave-coherent stress) We also look at phase-averaged flow fields of the following: -Wind speed (horizontal and vertical) -Pressure -Turbulent kinetic energy -Dissipation rate -Vorticity (cross-wind) -Turbulent and wave-coherent stress -Pressure, turbulent tangential stress, and turbulent normal stresses (surface distribution) Finally, we look at cross-wind turbulent instantaneous vorticity fields for the 0 and 90 degrees for the lowest and highest wave agesmore » « less
-
Abstract The quantification of pressure fields in the airflow over water waves is fundamental for understanding the coupling of the atmosphere and the ocean. The relationship between the pressure field, and the water surface slope and velocity, are crucial in setting the fluxes of momentum and energy. However, quantifying these fluxes is hampered by difficulties in measuring pressure fields at the wavy air-water interface. Here we utilise results from laboratory experiments of wind-driven surface waves. The data consist of particle image velocimetry of the airflow combined with laser-induced fluorescence of the water surface. These data were then used to develop a pressure field reconstruction technique based on solving a pressure Poisson equation in the airflow above water waves. The results allow for independent quantification of both the viscous stress and pressure-induced form drag components of the momentum flux. Comparison of these with an independent bulk estimate of the total momentum flux (based on law-of-the-wall theory) shows that the momentum budget is closed to within approximately 5%. In the partitioning of the momentum flux between viscous and pressure drag components, we find a greater influence of form drag at high wind speeds and wave slopes. An analysis of the various approximations and assumptions made in the pressure reconstruction, along with the corresponding sources of error, is also presented.more » « less
An official website of the United States government

