ESS228
Prof. Jin-Yi Yu
Equatorial Waveguide
Linearized shallow-water equations
Assume wave-form solutions
•Wave-like solutions can result from this equation if this coefficient has a positive value.
•When y increases (i.e., away from the equator), this coefficient becomes negative (due to the b2y2 term) and the wave-like solution becomes an exponential solution (i.e., the wave solution disappears).
•Equatorial waves are trapped in the tropics.
•This waveguide effect is due entirely to the variation of Coriolis parameter with latitude.