Full-depth conductivity-temperature-depth (CTD)/hydrographic measureme
nts with high horizontal and vertical resolution were made in February
-April 1993 along a line lying at a nominal longitude of 88 degrees W
and extending from southern Chile (54 degrees S) to Guatemala (14 degr
ees N). It crossed five major deep basins (Southeast Pacific, Chile, P
eru, Panama, and Guatemala basins) east of the East Pacific Rise. Vert
ical sections of potential temperature, salinity, potential density, o
xygen, silica, phosphate, nitrate, and nitrite are presented to illust
rate the structure of the entire water column. Some features of intere
st found in the sections are described, and an attempt is made to inte
rpret them in terms of the isopycnal property distributions associated
with the large-scale ocean circulation. These features include: vario
us near-surface waters observed in the tropical and subtropical region
s and the fronts that mark the boundaries of these waters; the possibl
e importance of salt fingering to the downward salt transfer from the
high-salinity subtropical water; a shallow thermostad (pycnostad) deve
loped at 16 degrees-18.5 degrees C in the subtropical water; low-salin
ity surface water in the subantarctic zone west of southern Chile; lar
ge domains of extremely low oxygen in the subpycnocline layer on both
sides of the equator and a secondary nitrite maximum associated with a
nitrate minimum in these low-oxygen domains; high-salinity, low-oxyge
n, high-nutrient subpycnocline water that is carried poleward along th
e eastern boundary by the Peru-Chile Undercurrent; the Subantarctic Mo
de and Antarctic Intermediate waters; middepth isopycnal property extr
ema observed at the crest of the Sala y Gomez Ridge; influences of the
North Pacific and the North Atlantic upon deep waters along the secti
on; and the characteristics and sources of the bottom waters in the fi
ve deep basins along the section.