TY - JOUR
T1 - Breaking wave field statistics with a multi-layer model
AU - Wu, Jiarong
AU - Popinet, Stéphane
AU - Deike, Luc
N1 - Funding Information:
This work was supported by the National Science Foundation (Physical Oceanography) under Grant No. 2122042 to L.D., the High Meadows Environmental Institute Energy and Climate Grand Challenge, the NASA Ocean Vector Winds Science Team 22-OVWST22-0012 and the Cooperative Institute for Earth System Modeling between Princeton and the Geophysical Fluid Dynamics Laboratory (GFDL) NOAA. Computations were partially performed using the Extreme Science and Engineering Discovery Environment (XSEDE), which is supported by NSF Grant No. ACI-1053575; and on resources managed and supported by Princeton Research Computing, a consortium of groups including the Princeton Institute for Computational Science and Engineering and the Office of Information Technology's High Performance Computing Center and Visualization Laboratory at Princeton University. J.W. would also like to acknowledge the support of the Mary and Randall Hack ’69 Graduate Award received through the High Meadows Environmental Institute.
Publisher Copyright:
© The Author(s), 2023. Published by Cambridge University Press.
PY - 2023/7/31
Y1 - 2023/7/31
N2 - The statistics of breaking wave fields are characterised within a novel multi-layer framework, which generalises the single-layer Saint-Venant system into a multi-layer and non-hydrostatic formulation of the Navier-Stokes equations. We simulate an ensemble of phase-resolved surface wave fields in physical space, where strong nonlinearities, including directional wave breaking and the subsequent highly rotational flow motion, are modelled, without surface overturning. We extract the kinematics of wave breaking by identifying breaking fronts and their speed, for freely evolving wave fields initialised with typical wind wave spectra. The distribution, defined as the length of breaking fronts (per unit area) moving with speed to following Phillips (J. Fluid Mech., vol. 156, 1985, pp. 505-531), is reported for a broad range of conditions. We recover the scaling without wind forcing for sufficiently steep wave fields. A scaling of based solely on the root-mean-square slope and peak wave phase speed is shown to describe the modelled breaking distributions well. The modelled breaking distributions are in good agreement with field measurements and the proposed scaling can be applied successfully to the observational data sets. The present work paves the way for simulations of the turbulent upper ocean directly coupled to a realistic breaking wave dynamics, including Langmuir turbulence, and other sub-mesoscale processes.
AB - The statistics of breaking wave fields are characterised within a novel multi-layer framework, which generalises the single-layer Saint-Venant system into a multi-layer and non-hydrostatic formulation of the Navier-Stokes equations. We simulate an ensemble of phase-resolved surface wave fields in physical space, where strong nonlinearities, including directional wave breaking and the subsequent highly rotational flow motion, are modelled, without surface overturning. We extract the kinematics of wave breaking by identifying breaking fronts and their speed, for freely evolving wave fields initialised with typical wind wave spectra. The distribution, defined as the length of breaking fronts (per unit area) moving with speed to following Phillips (J. Fluid Mech., vol. 156, 1985, pp. 505-531), is reported for a broad range of conditions. We recover the scaling without wind forcing for sufficiently steep wave fields. A scaling of based solely on the root-mean-square slope and peak wave phase speed is shown to describe the modelled breaking distributions well. The modelled breaking distributions are in good agreement with field measurements and the proposed scaling can be applied successfully to the observational data sets. The present work paves the way for simulations of the turbulent upper ocean directly coupled to a realistic breaking wave dynamics, including Langmuir turbulence, and other sub-mesoscale processes.
KW - air/sea interactions
KW - surface gravity waves
KW - wave breaking
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U2 - 10.1017/jfm.2023.522
DO - 10.1017/jfm.2023.522
M3 - Article
AN - SCOPUS:85167703333
SN - 0022-1120
VL - 968
JO - Journal of Fluid Mechanics
JF - Journal of Fluid Mechanics
M1 - A12
ER -