  This study aims to describe the response of two persistent chlorophyll-a
maxima to physical processes affecting the thermocline and nitracline position
in the Eastern Tropical North Pacific (ETNP). We focused on Long Rossby Waves
given their relevance to the ETNP circulation and its potential as a mechanism
introducing nutrients into the euphotic zone. We found the shallower
chlorophyll-a maximum in oxygenated waters became more intense when denser
waters (more nutrients) moved toward the surface. It suggests that isopycnals
and nitracline displacements modify the nutrient supply in the euphotic zone,
which produces changes in phytoplankton growth. The suboxic and deeper
chlorophyll a maximum showed a strong association with the 26 kg m^{-3}
isopycnal being only mechanically displaced, and its chlorophyll-a content does
not seem to covary with irradiance or nutrients. The different responses of the
chlorophyll-a maxima could be explained if different phytoplankton groups are
associated with them. Long Rossby Waves can affect the position of the
thermocline, nitracline and isopycnals in an annual cycle, but it seems to be a
background signal modulated by higher frequency processes such as mesoscale
eddies and other Rossby waves. The co-occurrence of processes can control the
nitracline depth, and hence the input of nutrients into the euphotic zone that
can cause sporadic enhancements of the chlorophyll-a concentration of one
maximum.
