A time series of coastal zone color scanner (CZCS) derived chlorophyll (CZCS‐chl) and sea
surface temperature (SST) satellite imagery was developed for the Mid‐Atlantic Bight (MAB) …

Spatial distributions and variability of suspended particulate matter (SPM) were determined
optically during CTD/transmissometer surveys of warm-core ring (WCR) 82B and …

An array of tall current meter moorings, bottom-mounted inverted echo sounders and
pressure gauges was deployed for one year in an area about 150-500 km northeast of Cape …

Rates of utilization for NO 3−, NH 4+, urea, and PO 4− by primary producers and the
abundances of particulate C, N, and P were determined for the euphotic zone of warm-core …

Intense cooling of a warm-core ring or warming of the fluids surrounding a ring can increase
the density of that ring relative to the surrounding fluids. This increase in density can cause …

Abstract Nonmigratory, 12-kHz, deep sound-scattering layers (NMDSLs) were entrained
within Sargasso Sea-Gulf Stream waters during the formation of warm-core rings 82B and …

The abundance, carbon isotopic composition (Δ14C and δ13C), and lipid biomarker
(alkenones and saturated fatty acids) distributions of suspended particulate organic matter …

The hydrographic properties of warm-core ring 82B are shown from three cruises; April,
June and August 1982. The velocity field for each cruise is formed from the gradient-current …

During the spring and summer of 1982, Gulf Stream warm core ring (WCR) 82B was
sampled during four cruises from April to August to investigate phytoplankton distributional …

Regeneration of a warm anticyclonic ring as a result of interaction with cold water masses
was observed within the western subarctic gyre of the North Pacific. Satellite, profiling float …