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

被引:8
作者
Zhang, Ting [1 ,2 ]
Song, Jinbao [1 ,2 ]
机构
[1] Zhejiang Univ, Ocean Coll, Zhoushan 316000, Peoples R China
[2] State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China
基金
中国国家自然科学基金;
关键词
drag coefficient; marine atmospheric boundary layer; ocean spray droplets; surface waves; DRAG COEFFICIENT; BOUNDARY-LAYER; WIND SPEEDS; PROFILES; COASTAL; IMPACT; SWELL;
D O I
10.1007/s00376-017-7101-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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.
引用
收藏
页码:469 / 478
页数:10
相关论文
共 35 条
  • [1] Andreas EL, 2004, J PHYS OCEANOGR, V34, P1429, DOI 10.1175/1520-0485(2004)034<1429:SSR>2.0.CO
  • [2] 2
  • [3] Andreas EL, 1998, J PHYS OCEANOGR, V28, P2175, DOI 10.1175/1520-0485(1998)028<2175:ANSSGF>2.0.CO
  • [4] 2
  • [5] [Anonymous], 1955, Q. J. R. Meteorol. Soc., DOI [DOI 10.1002/QJ.49708135027, DOI 10.1002/QJ.49708135027,ARXIV:HTTPS://RMETS.ONLINELIBRARY.WILEY.COM/DOI/PDF/10.1002/QJ.49708135027]
  • [6] On the limiting aerodynamic roughness of the ocean in very strong winds
    Donelan, MA
    Haus, BK
    Reul, N
    Plant, WJ
    Stiassnie, M
    Graber, HC
    Brown, OB
    Saltzman, ES
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (18) : L183061 - 5
  • [7] Wave-Dependence of Friction Velocity, Roughness Length, and Drag Coefficient over Coastal and Open Water Surfaces by Using Three Databases
    Gao Zhiqiu
    Wang, Qing
    Zhou Mingyu
    [J]. ADVANCES IN ATMOSPHERIC SCIENCES, 2009, 26 (05) : 887 - 894
  • [8] Grachev AA, 2003, J PHYS OCEANOGR, V33, P2408, DOI 10.1175/1520-0485(2003)033<2408:WSVOOW>2.0.CO
  • [9] 2
  • [10] Wave-driven wind jets in the marine atmospheric boundary layer
    Hanley, Kirsty E.
    Belcher, Stephen E.
    [J]. JOURNAL OF THE ATMOSPHERIC SCIENCES, 2008, 65 (08) : 2646 - 2660