Me. Huntley et al., MESOSCALE DISTRIBUTION OF ZOOPLANKTON IN THE CALIFORNIA CURRENT IN LATE SPRING, OBSERVED BY OPTICAL PLANKTON COUNTER, Journal of marine research, 53(4), 1995, pp. 647-674
A survey of zooplankton in the upper 300 m of the central California C
urrent, from the coastal shelf to 128W and between 36.5N and 39.5N, wa
s conducted in early June 1993 using an Optical Plankton Counter (OPC)
as part of an interdisciplinary study of mesoscale ocean circulation
and biological dynamics. The OPC was part of a multi-instrument packag
e towed on an undulating vehicle (SeaSoar). Estimates of normalized si
ze spectra and absolute abundance from OPC data compared favorably wit
h measurements based on Bongo net catches. After processing, the stand
ardized OPC data set provides a resolution of approximate to 7 km in t
he horizontal and 10 m in the vertical for 60 size categories of zoopl
ankton ranging in estimated body weight from 3 mu g C to 3000 mu g C.
Results reveal rich mesoscale variability in zooplankton distributions
at scales of 30-60 km, with regions of enhanced biomass and abundance
coinciding with the location of mesoscale eddies, both cyclonic and a
nticyclonic. The central jet of the California Current departed from t
he coastline near Cape Mendocino (39.5N), separating a region of gener
ally greater zooplankton biomass near the coast from one of lower biom
ass to the west. The jet usually contained lower biomass than adjacent
eddies. Total zooplankton biomass ranged from <2g C m(-2) to >20 g C
m(-2). The two mesoscale features containing the highest biomass, one
200 nm offshore of Cape Mendocino and another 100 nm west of Monterey
Bay, were dominated by euphausiids.