4.6 Article

Effects of Sea-Surface Waves and Ocean Spray on Air-Sea Momentum Fluxes

Journal

ADVANCES IN ATMOSPHERIC SCIENCES
Volume 35, Issue 4, Pages 469-478

Publisher

SCIENCE PRESS
DOI: 10.1007/s00376-017-7101-7

Keywords

drag coefficient; marine atmospheric boundary layer; ocean spray droplets; surface waves

Funding

  1. National Natural Science Foundation of China [41576013, 41476021, 41621064]
  2. National Key Research and Development Program of China [2016YFC1401404]
  3. Indo-Pacific Ocean Environment Variation and Air-Sea Interaction project [GASI-IPOVAI-04]

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The effects of sea-surface waves and ocean spray on the marine atmospheric boundary layer (MABL) at different wind speeds and wave ages were investigated. An MABL model was developed that introduces a wave-induced component and spray force to the total surface stress. The theoretical model solution was determined assuming the eddy viscosity coefficient varied linearly with height above the sea surface. The wave-induced component was evaluated using a directional wave spectrum and growth rate. Spray force was described using interactions between ocean-spray droplets and wind-velocity shear. Wind profiles and sea-surface drag coefficients were calculated for low to high wind speeds for wind-generated sea at different wave ages to examine surface-wave and ocean-spray effects on MABL momentum distribution. The theoretical solutions were compared with model solutions neglecting wave-induced stress and/or spray stress. Surface waves strongly affected near-surface wind profiles and sea-surface drag coefficients at low to moderate wind speeds. Drag coefficients and near-surface wind speeds were lower for young than for old waves. At high wind speeds, ocean-spray droplets produced by wind-tearing breaking-wave crests affected the MABL strongly in comparison with surface waves, implying that wave age affects the MABL only negligibly. Low drag coefficients at high wind caused by ocean-spray production increased turbulent stress in the sea-spray generation layer, accelerating near-sea-surface wind. Comparing the analytical drag coefficient values with laboratory measurements and field observations indicated that surface waves and ocean spray significantly affect the MABL at different wind speeds and wave ages.

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