Geostrophic current - PowerPoint PPT Presentation

 p and  surfaces are parallel

Barotropic flow:.  p and  surfaces are parallel. For a barotropic flow, we have. is geostrophic current. Since. . Given a barotropic and hydrostatic conditions,. and. Therefore,. By definition,   and  t are both constant in barotropic flow. And. So.

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warm

The aim of this study and data sources. Comparison (@Kuroshio Extension). Surface wind (Ekman Trans) Data source: CCMP (1/4 deg). Ocean waves (Stokes Trans) Data source: WW3 (1/4 deg). Wind modulation by SST (e.g., Chelton et al2004) (included in CCMP product). Wave modulation

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