The relationship between temperature and nitrate in the upper 200 m of
the central and eastern tropical Pacific was investigated using regre
ssion techniques, and the slope of this relationship was compared alon
g spatial and temporal dimensions. In the open-ocean waters of the eas
tern and central Pacific, variation in the slope of the temperature-ni
trate (TN) relationship was primarily north-south, with the steepness
of the slope decreasing to the south. In the more coastal waters of th
e southeastern Pacific, however, the slope showed strong gradients in
the east-west direction, with the slope steepening from west to east.
Seasonal trends in the slope of the TN relationship were examined alon
g the equator. During March-May the relatively flat slope of the TN re
lationship that is found year-round in the central Pacific is found to
extend further east, associated with the intensification and shoaling
of the Equatorial Undercurrent during this same period. Regressions p
redicting nitrate from temperature were tested on new data and errors
of prediction were low for open-ocean locations (1.4 mu M); however, e
rrors increased (to 3.2-4.3 mu M) With proximity to coastal waters, re
flecting the increasing and variable contribution of nitrate uptake by
phytoplankton.