According to the model, what normally signals the disappearance of an El Nino?
A.
The arrival in the eastern Pacific of negative sea-level Kelvin waves.
B.
An increase in the speed at which negative Rossby waves cross the Pacific.
C.
A shift in the direction of the winds produced by the start of an anti-El Nino elsewhere in the Pacific.
D.
The reflection of Kelvin waves after they reach the eastern boundary of the Pacific, along Ecuador and Peru.