Birds and mammals are important components of pelagic marine ecosystems, bu
t our knowledge of their foraging ecology is limited. We distinguish six di
stinct types of data that can be used in various combinations to understand
their foraging behavior and ecology. We describe methods that combine conc
urrent dive recorder deployment, oceanographic sampling, and hydroacoustic
surveys to generate hypotheses about interactions between the physical envi
ronment and the distribution, abundance, and behavior of pelagic predators
and their prey. Our approach is to (1) map the distribution of whales in re
lation to the distribution of their prey and the physical features of the s
tudy area (bottom topography, temperature, and salinity); and (2) measure t
he foraging behavior and diet of instrumented whales in the context of the
fine-scale distribution and composition of their prey and the physical envi
ronment. We use this approach to demonstrate a relationship between blue wh
ale distribution, sea surface temperature, and concentrations of their euph
ausiid prey at different spatial scales offshore of the Channel Islands, Ca
lifornia. Blue whale horizontal spatial distribution was correlated with re
gions of high acoustic backscatter. Blue whale dive depths closely tracked
the depth distribution of krill. Net sampling and whale diet revealed that
whales fed exclusively upon dense schools of Euphausia pacifica (between 10
0 and 200 m) and Thysanoessa spinifera (from the surface to 100 m). Whales
concentrated foraging efforts upon those dense euphausiid schools that form
downstream from an upwelling center in close proximity to regions of steep
topographic relief We propose that (1) the distribution of Balaenoptera wh
ales in the coastal California Current region is defined by their attractio
n to areas of predictably high prey density; (2) the preferred prey of thes
e whales are several species of euphausiids (E. pacifica, T. spinifera, and
N. simplex) that are abundant in the California Current region; (3) blue w
hales concentrate their foraging efforts on dense aggregations of euphausii
ds found at discrete depths in the water column; (4) these localized areas
of high euphausiid densities are predictable and sustained by enhanced leve
ls of primary productivity in regions which are located downstream from coa
stal upwelling centers (indicated by sea surface temperature); (5) topograp
hic breaks in the continental shelf located downstream from these upwelling
centers work in concert with euphausiid behavior to collect and maintain l
arge concentrations of euphausiids swarms, and (6) despite seasonal and int
er-annual variability, these processes are sufficiently consistent that the
distribution of Balaenoptera whales can be predicted. (C) 1998 Elsevier Sc
ience Ltd. All rights reserved.