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Imbalance of energy and momentum source terms of the sea wave transfer equation for fully developed seas

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Figure

Figure 4b, where the total integrated source term obtainedfor the oldest seas is reduced to less than 5 % of the inputand dissipation source terms taken separately.
Fig. 1.ϕ)=k4F(k,ϕ) in the high wavenumber range (k≥direction ( = 0), while the thin line stands for the spectrum in the crosswind Curvature spectrum25kϕ = π/k ≥ 25kp) as given by Elfouhaily et al.’s (1997)4 B(k,ϕ) = kF(k,ϕ) in the highϕgiven by  Elfouhaily
Table 2. Same as Table 1, but Elfouhaily et al.’s (1997) wave spec-trum is replaced by Kudryavtsev et al.’s (2003) spectrum at highwavenumbers (k ≥ 25kp).
Fig. 2. 25kp k = 25kp, the sea wave spectralµ quantifying the downward spectral energy flux (as defined by equation  µis from Komen et al
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