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An improved parameterization of tidal mixing for ocean models

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Academic year: 2017

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Table 1. Energy flux (TW) out of the barotropic tide estimated by JS01 and ER03 for different depth ranges
Table 2. Acronyms of climate model experiments performed with different estimates of the barotropic tide energy flux E 2 - D
Table 3. Ocean circulation indices in Sv. “Mid global” denotes the strength of the mid-depth global meridional overturning cell
Fig. 1. Logarithm of total energy flux out of the barotropic tide E (W m −2 ) estimated from satellite altimetry (ER03, left) and a tide model (JS01, right)
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