Anisotropic tidal dissipation in misaligned planetary systems

Open Access

Table 2

Features of the global ocean modes that are resonantly excited by the semidiurnal tidal forces.

n	$Λ_{n}^{2, 1}$ ${\rm{\Lambda }}_n^{2,1}$	P_n (hours)	log₁₀ (P_n) (days)
2	11.129	33.653	0.147
4	41.333	17.462	−0.138
6	91.060	11.765	−0.310
8	160.424	8.864	−0.433
10	249.469	7.108	−0.528
12	358.213	5.932	−0.607
14	486.671	5.089	−0.674
16	634.847	4.456	−0.731
18	802.747	3.962	−0.782
20	990.374	3.567	−0.828

Notes. From left to right are provided the degrees of the ocean modes, their associated eigenvalues, and their resonant rotation periods, given in both hours and days (in logarithmic scale).

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