Mean meridional upper ocean temperature, salinity and zonal velocity sections across the Pacific Ocean between 8°S and 8°N are combined with other oceanographic and air-sea flux data in an inverse model. The tropical Pacific Ocean can be divided into three regions with distinct circulation patterns: western (143°E-170°W); central (170°W-125°W); and eastern (125°W-eastern boundary). In the central and eastern Pacific the downward limbs of the shallow tropical cells are 15(±13)Sv in the north and 20(±11)Sv in the south. The Pacific cold tongue in the eastern region results from diapycnal upwelling through all layers of the Equatorial Undercurrent, which preferentially exhausts the lightest (warmest) layers of the Undercurrent (10(±6)Sv) between 125°W and 95°W and adjacent to the American coast. An inter-hemispheric exchange of 13(±13)Sv between the southern and northern Pacific Ocean forms the Pacific branch of the Pacific-Indian interbasin exchange. Southern hemisphere water enters the tropical Pacific Ocean via the direct route at the western boundary and via an interior (basin) pathway. However, this water moves irreversibly into the North Pacific by upwelling in the eastern equatorial Pacfici and by air-sea transformation that drives poleward interior transport across 2°N.
Dr. William S. Kessler
NOAA / PMEL / OCRD
7600 Sand Point Way NE
Seattle WA 98115 USA
|See also:||Kessler home page Kessler publications PMEL home page|