Open AccessOn the Dynamical Relationship between Equatorial Pacific Surface Currents, Zonally Averaged Equatorial Sea Level, and El Niño Prediction
Author(s) -
Xiaolin Zhang,
Allan J. Clarke
Publication year - 2017
Publication title -
journal of physical oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.706
H-Index - 143
eISSN - 1520-0485
pISSN - 0022-3670
DOI - 10.1175/jpo-d-16-0193.1
Subject(s) - rossby wave , equator , thermocline , kelvin wave , geology , zonal flow (plasma) , sea surface height , equatorial waves , geostrophic wind , latitude , climatology , boundary current , sea level , geostrophic current , forcing (mathematics) , ocean current , geophysics , sea surface temperature , geodesy , physics , oceanography , plasma , quantum mechanics , tokamak
Previous work has shown that for large zonal scales and low frequencies, wind-forced sea level, even near the equator, can be described by wind-forced long Rossby waves. In the eastern equatorial Pacific where the interannual wind forcing is small, these waves are essentially locally unforced and propagate westward from the boundary. At the boundary the waves’ sea level is in phase because of geostrophy and no normal flow to the boundary. However, because the waves propagate more slowly with increasing latitude, west of the boundary lag increases as latitude increases. Consequently a northward sea level gradient is like a time derivative, and the zonal geostrophic flow is like a time derivative of the sea level. This implies that the equatorial flow should lead the equatorial sea level by about 9 months on El Niño time scales. However, analysis shows that when dissipation of the large-scale flow is taken into account, this lead is reduced to about 3 months. This lead time is approximately the dissipation time scale of the second vertical mode, which dominates the zonal surface flow. Since the eastern equatorial Pacific sea level η E is proportional to eastern equatorial thermocline displacement and El Niño, the zonal equatorial flow leads El Niño indices. Analysis also shows that the zonally averaged equatorial Pacific sea level leads El Niño and that this lead is associated with the geostrophic zonal velocity and the long Rossby wave physics.