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The Global Characteristics of the Wavenumber Spectrum of Ocean Surface Wind

机译:海洋表面风波数谱的全局特征

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摘要

The wavenumber spectra of wind kinetic energy over the ocean from Quick Scatterometer (QuikSCAT) observations have revealed complex spatial variability in the wavelength range of 1000-3000 km, with spectral slopes varying from -1.6 to -2.9. Here the authors performed a spectral analysis of QuikSCAT winds over the global ocean and found that (i) the spectral slopes become steeper toward the Poles in the Pacific and in the South Atlantic, and the slopes exhibit minimal longitudinal dependence in the South Pacific; (ii) the steepest slopes are in the tropical Indian Ocean and the shallowest slopes are in the tropical Pacific and Atlantic; and (iii) the spectra are steeper in winter than summer in most regions of the midlatitude Northern Hemisphere. The new findings reported in the paper provide a test bed for theoretical studies and atmospheric general circulation models.
机译:快速散射仪(QuikSCAT)观测到的海洋风动能的波数谱显示出1000-3000 km波长范围内复杂的空间变异性,光谱斜率从-1.6到-2.9。在这里,作者对全球海洋上的QuikSCAT风进行了频谱分析,发现(i)频谱斜率在太平洋和南大西洋朝波兰两极变陡,而在南太平洋,这些斜率表现出最小的纵向依赖性; (ii)最陡峭的斜坡是在热带印度洋,而最浅的斜坡是在热带太平洋和大西洋; (iii)在北半球中纬度的大多数地区,冬天的光谱要比夏天的光谱陡。本文报道的新发现为理论研究和大气总循环模型提供了试验平台。

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  • 来源
    《Journal of Physical Oceanography》 |2011年第8期|p.1576-1582|共7页
  • 作者单位

    Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California;

    Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California;

    Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology,Cambridge, Massachusetts;

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