Solitary Rossby Waves in the Lower Tropical Troposphere

Figure 4

Configuration of streamlines in the case of weakly nonlinear approximation with 𝐶₀=10m⋅s⁻¹ and 𝜖=0.01 for (a)  𝐶₁=0.05m⋅s⁻¹; (b)  𝐶₁=0.5m⋅s⁻¹; (c)  𝐶₁=5m⋅s⁻¹; and (d)  𝐶₁=25m⋅s⁻¹.

(a)

(b)

(c)

(d)