Meandering Flows in the Oceanic and Atmospheric Boundary Layers due to Breaking Ocean Waves

https://www.researchgate.net/publication/344482927

Breaking waves generate meandering currents and winds in the oceanic and atmospheric boundary layers (Dommermuth et al., 2014). Meandering flows are revisited here for five types of breaking waves. Streaming flows are mean flows that include Eulerian and Lagrangian contributions. Meandering flows include both difference (streaming) and sum frequency interactions. Meandering flows, like streaming flows, have Eulerian and Lagrangian contributions. Normal to the free surface, the meandering flows exponentially attenuate away from the free surface with an oscillatory behavior. The magnitudes of the meandering flows agree with Langmuir’s original observations (Langmuir, 1938). The good agreement suggests that the formation of Langmuir circulations is due to meandering flows.… Read more

Magnetic Induction due to the Effects of Breaking Ocean Waves

https://www.researchgate.net/publication/344482876

Breaking waves generate meandering currents and winds in the oceanic and atmospheric boundary layers. The length scales and frequencies of the meandering currents and winds are respectively longer and higher than those of the underlying ocean waves. The difference in spatial and temporal scales makes it possible to indirectly measure the meandering current in the oceanic boundary layer using the principles of magnetic induction that would otherwise be difficult using more direct methods. Such measurements are desirable to quantify mixing in the oceanic and atmospheric boundary layers due to meandering flows.

The Generation of Electric Fields by Meandering Flows

https://www.researchgate.net/publication/344787449

Meandering flows are wave driven much like streaming flows. The interaction of the wavy portion of the flow with the vortical portion of the flow gives rise to meandering flows. Meandering flows, like streaming flows, are not turbulent. The nonlinear wave interactions give sum and difference frequencies in meandering flows. The difference frequencies have long been associated with streaming flows in the ocean (Longuet-Higgins, 1953). Meandering flows occur in the atmosphere as well as the ocean. Streaming flows are a subset of meandering flows. Meandering flows are expected to vary over long distances due to nonlinear wave interactions, variations in currents and winds, etc. In the upper ocean, (Dommermuth, 2020d) shows that slow variations of the meandering wind-drift interacting with the earth’s magnetic field induces a magnetic disturbance in the upper ocean and lower atmosphere. Dommermuth (2018b,c,d,e) show how the wind drift affects wave breaking. Here, the effects of variations in the meandering wind drift and meandering wind on the surface charge density are considered. Blanchard (1963); Gathman (1986) show that the surface charge density is due to the electrification of the atmosphere by (1) bubbles bursting on the ocean surface due to the effects of wave breaking and (2) sea spray torn off the crests of waves by wind shear. The variations in surface charge density are expected due to variations in wave breaking and wind shear occurring over long spatial scales due to meandering flows. This paper along with Dommermuth (2020d) provide experimentalists with bases for measuring effects of meandering flows on the magnetic and electric fields in the ocean and atmosphere. Experiments can be performed to confirm the existence of meandering flows and to quantify the mixing of the upper ocean and lower atmosphere. During fair weather the electric field that is generated by the effect of meandering flows on the surface charge density is about 10% of the potential gradient at altitudes 3km above the ocean surface. The effects of the electric disturbance attenuate slowly with altitude at a rate that is very similar to the potential gradient. The frequencies of oscillations are about 0.2-1Hz due to nonlinear sum-frequency wave interactions. During a storm the electric field that is generated by the meandering flows would become increasingly violent with significant energy being radiated within specific frequency bands in an organized manner.

Spilling Breaking Ocean Waves and Inverse Energy Cascades

https://www.researchgate.net/publication/348136300

The Ocean’s Heartbeat (OH) is an inverse energy cascade that occurs through interactions between surface gravity waves and organized vortical structures in the atmosphere and the ocean. The vortical wake of spilling breaking waves can generate the inverse energy cascade even in the absence of wind and current shear. Standing waves are generated as the vortical portions of the flow modulate the generation and evolution of surface gravity waves and vice versa. Resonances occur between the standing waves and coherent structures in the ocean. Monopolar, dipolar, tripolar, and quadrupolar vortical structures (OH structures) are shed out the back of spilling breaking waves. Intense OH structures generate knots in the free-surface elevation in the wake of spilling breaking waves. OH structures surf the crests of spilling breaking waves slightly behind the whitecaps. The results of numerical simulations give credence to two conjectures: 1) OH standing waves can generate microseisms even when opposing wave groups are not present and 2) The OH inverse energy cascade is present in satellite altimetry of sea surface height measurements.

Research Papers and Reports

Langmuir Circulations and Meandering Flows

Windrows

The Ocean’s Heartbeat

Electric and Magnetic Fields of Meandering Flows

  • Dommermuth, D. G., “Magnetic Induction due to the Effects of Breaking Ocean Waves,” ResearchGate preprint, Oct 2020.
    https://www.researchgate.net/publication/344482876
  • Dommermuth, D. G., “The Generation of Electric Fields by Meandering Flows,” ResearchGate preprint, Oct 2020. https://www.researchgate.net/publication/344787449 (Please see more recent technical reports on the electric field that is induced by the transport of space charge density by the meandering wind.)
  • Dommermuth, D. G., “The Electric and Magnetic Fields due to the Transport of Space Charge Density by the Meandering Wind over the Ocean Surface,” ResearchGate preprint, Sep 2021. https://www.researchgate.net/publication/354665883 (Please see more recent technical reports on the electric field that is induced by the transport of space charge density by the meandering wind.)
  • Dommermuth, D.G., “The Electric and Magnetic Fields due to the Transport of Space Charge Density by the Meandering Wind over the Ocean Surface: New Evidence of an Inverse Energy Cascade in the Lower Atmosphere,” ResearchGate preprint, Sep 2021. https://www.researchgate.net/publication/354935485
  • Dommermuth, D.G., “The Electric and Magnetic Fields due to Magnetic Induction by Meandering Flows in the Oceanic and Atmospheric Boundary Layers: New Evidence of an Inverse Energy Cascade in the Upper Ocean,” ResearchGate preprint, Oct 2021. https://www.researchgate.net/publication/355215804
  • Dommermuth, D.G., “The Magnetic Fields due to Magnetic Induction by Meandering Drift Currents,” ResearchGate preprint, Oct 2021. https://www.researchgate.net/publication/355651651
  • Dommermuth, D.G., “A Parametric Study of the Electric Field in the Atmosphere due to the Transport of Space Charge Density by the Meandering Wind over the Ocean Surface,” ResearchGate preprint, Nov 2021. https://www.researchgate.net/publication/356002487

Maxima Scripts for Meandering Flows

  • Dommermuth, D.G., “Maxima Coding for Solving the Electric and Magnetic Fields due to the Transport of Space Charge Density over the Ocean Surface: New Evidence of an Inverse Energy Cascade in the Lower Atmosphere,” ResearchGate code, Sep 2021. https://www.researchgate.net/publication/354935522
  • Dommermuth, D.G., “A Maxima Script for Solving the Electric and Magnetic Fields due to Magnetic Induction by Meandering Flows in the Oceanic and Atmospheric Boundary Layers: New Evidence of an Inverse Energy Cascade in the Upper Ocean,” ResearchGate code, Oct 2021. https://www.researchgate.net/publication/355209396

Fortran Codes for Meandering Flows

  • Dommermuth, D.G., “A Fortran Code for Calculating Electric and Magnetic Fields due to the Transport of Space Charge Density by the Meandering Wind over the Ocean Surface: New Evidence of an Inverse Energy Cascade in the Lower Atmosphere,” ResearchGate code, Sep 2021. https://www.researchgate.net/publication/354935467
  • Dommermuth, D.G., “A Fortran Code for Calculating the Electric and Magnetic Fields due to Magnetic Induction by Meandering Flows in the Oceanic and Atmospheric Boundary Layers: New Evidence of an Inverse Energy Cascade in the Upper Ocean,” ResearchGate code, Oct 2021. https://www.researchgate.net/publication/355209298
  • Dommermuth, D.G., “F90 Coding for Calculating the Magnetic Fields due to Magnetic Induction by Meandering Drift Currents,” ResearchGate code, Oct 2021. https://www.researchgate.net/publication/355651566
  • Dommermuth, D.G., “F90 Coding for a Parametric Study of the Electric Field in the Atmosphere due to the Transport of Space Charge Density by the Meandering Wind over the Ocean Surface,” ResearchGate code, Nov 2021. https://www.researchgate.net/publication/356002311

The Effect of the Wind Drift on Wave Growth, Wave Breaking, and the Production of Turbulence

The Effect of Standing Waves on the Wave Energy Cascade

Helmholtz Decompositions into Wavy and Vortical Portions

  • Dommermuth, D. G., “The laminar interactions of a pair of vortex tubes with a free surface,” J. Fluid Mech., Vol. 246, 1993, pp. 91–115. https://doi.org/10.1017/S0022112093000059
  • Mui, R. C. and Dommermuth, D. G., “The vortical structure of a near-breaking gravity-capillary wave,” Journal of Fluids Engineering, Vol. 117, 1994,355–361. https://doi.org/10.1115/1.2817269
  • Dommermuth, D. G., Novikov, E.A., and Mui, C.Y., “The Interaction of Surface Waves with Turbulence,” The Proceedings of the Symposium on Free-Surface Turbulence, ASME Fluids Engineering Division Summer Meeting, Lake Tahoe, California, USA, 1994. https://www.researchgate.net/publication/271527603

Entrainment and Mixing due to Plunging Breaking Waves

Numerical Methods