TY - JOUR
T1 - Lagrangian transport by nonbreaking and breaking deep-water waves at the ocean surface
AU - Pizzo, Nick
AU - Melville, W. Kendall
AU - Deike, Luc
N1 - Funding Information:
UC Santa Barbara, supported by the National Science Foundation under Grant NSF PHY17-48958, where a portion of this research was conducted. L.D. acknowledges support from the Princeton Environmental Institute at Princeton University and the Cooperative Institute for Climate Sciences between NOAA and Princeton University.
Funding Information:
Acknowledgments. This research was conducted under grants to W.K.M. from the Office of Naval Research (Grant N00014-17-1-2171) and the National Science Foundation (Physical Oceanography) (Grants NSF 1434198 and OCE-1634289). We thank the referees for comments that have improved the manuscript. N.P. thanks the Kavli Institute for Theoretical Physics at
Funding Information:
This research was conducted under grants to W.K.M. from the Office of Naval Research (Grant N00014-17-1-2171) and the National Science Foundation (Physical Oceanography) (Grants NSF 1434198 and OCE-1634289). We thank the referees for comments that have improved the manuscript. N.P. thanks the Kavli Institute for Theoretical Physics at UC Santa Barbara, supported by the National Science Foundation under Grant NSF PHY17-48958, where a portion of this research was conducted. L.D. acknowledges support from the Princeton Environmental Institute at Princeton University and the Cooperative Institute for Climate Sciences between NOAA and Princeton University.
Publisher Copyright:
© 2019 American Meteorological Society.
PY - 2019/4/1
Y1 - 2019/4/1
N2 - Using direct numerical simulations (DNS), Deike et al. found that the wave-breaking-induced mass transport, or drift, at the surface for a single breaking wave scales linearly with the slope of a focusing wave packet, and may be up to an order of magnitude larger than the prediction of the classical Stokes drift. This model for the drift due to an individual breaking wave, together with the statistics of wave breaking measured in the field, are used to compute the Lagrangian drift of breaking waves in the ocean. It is found that breaking may contribute up to an additional 30% to the predicted values of the classical Stokes drift of the wave field for the field experiments considered here, which have wind speeds ranging from 1.6 to 16ms-1, significant wave heights in the range of 0.7-4.7 m, and wave ages (defined here as cm/u*, for the spectrally weighted phase velocity cm and the wind friction velocity u*) ranging from 16 to 150. The drift induced by wave breaking becomes increasingly more important with increasing wind friction velocity and increasing significant wave height.
AB - Using direct numerical simulations (DNS), Deike et al. found that the wave-breaking-induced mass transport, or drift, at the surface for a single breaking wave scales linearly with the slope of a focusing wave packet, and may be up to an order of magnitude larger than the prediction of the classical Stokes drift. This model for the drift due to an individual breaking wave, together with the statistics of wave breaking measured in the field, are used to compute the Lagrangian drift of breaking waves in the ocean. It is found that breaking may contribute up to an additional 30% to the predicted values of the classical Stokes drift of the wave field for the field experiments considered here, which have wind speeds ranging from 1.6 to 16ms-1, significant wave heights in the range of 0.7-4.7 m, and wave ages (defined here as cm/u*, for the spectrally weighted phase velocity cm and the wind friction velocity u*) ranging from 16 to 150. The drift induced by wave breaking becomes increasingly more important with increasing wind friction velocity and increasing significant wave height.
KW - Atmosphere-ocean interaction
KW - Currents
KW - Gravity waves
KW - Ocean dynamics
KW - Wave breaking
KW - Wind waves
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U2 - 10.1175/JPO-D-18-0227.1
DO - 10.1175/JPO-D-18-0227.1
M3 - Article
AN - SCOPUS:85064935601
SN - 0022-3670
VL - 49
SP - 983
EP - 992
JO - Journal of Physical Oceanography
JF - Journal of Physical Oceanography
IS - 4
ER -