This mode has large loadings over the region of high standard deviation of the Tmin temperatures (Fig. 1a) and has a pattern similar to the spatial distribution of Tmin anomalies during TYPE1 cold wave events (Fig. 1d).
The more populated primary mode has a restricted range of movement with small librational amplitudes (ϕ2,3 = 6 ± 1°, ψ2,3 = 12 ± 7°), while the secondary mode has larger librational amplitudes (ϕ2,3 = 10 ± 5°, ψ2,3 = 25 ± 11°) that are similar to those of the S1 R2 linkage.
For fixed h, the lower order modes had larger skin depth (stronger coupling intensity) than the higher orders; then, the stronger coupling resulted in a large spectra shift.
As expected, the dominant modes have "larger" basins, i.e. stronger attraction, the larger their eigenvalues are.
That is, the mode having a large amplitude at the ionospheric dynamo layer, which is around 110 120 km on the dayside and a slightly higher altitude on the nightside, could dominate.
The velocity model including the water layer strongly suppresses fundamental mode (mode 0) generation, likely due to the fundamental mode having its largest amplitude at zero depth, i.e., on the contact surface of ground with the water layer.
Developing design strategies based on the use of ring stiffeners as a way of preventing global buckling (i.e., buckling modes that have large displacements around the top edge) was introduced by Schmidt et al. (1998).
The in-phase mode has relatively large tank amplitudes and does not preserve its symmetry under periodic parametric excitation.
The directions of propagation of these two numerical modes are opposite, and, in most practical cases, the spurious mode has a large damping rate.
This size range (accumulation mode) has extremely large atmospheric residence time and thus features a high potential for long-range dispersal.
If both We ⪢ 1 and ϱ We ⪢ 1, the spatial growth rate of both sinuous and varicose modes is almost the same, except at the small wavenumbers where the sinuous mode has slightly larger growth rate than the corresponding varicose mode.
