Two physical oceanography cruises on the R/V Endeavor were conducted by the co-PIs Jack Barth and Mike Kosro as part of the ONR-sponsored Coastal Mixing and Optics (CMO) Accelerated Research Initiative. The objective was to rapidly survey a region around 40.5N, 70.5W where a set of moorings and a stationary...
As part of the Coastal Ocean Processes (CoOP) project Coastal Ocean Advances in Shelf Transport (COAST), this was the second of two cruises in 2001 to study cross-shelf transport processes in a wind-driven coastal ocean. The project includes field experiments off the Oregon coast and coordinated ocean circulation/ecosystem and atmospheric...
Since June 2010, the Geostationary Ocean Color Imager (GOCI) has been collecting the first
diurnally resolved satellite ocean measurements. Here GOCI retrievals of phytoplankton chlorophyll
concentration and fluorescence are used to evaluate daily to seasonal changes in photophysiological
properties. We focus on nonphotochemical quenching (NPQ) processes that protect phytoplankton from...
Since June 2010, the Geostationary Ocean Color Imager (GOCI) has been collecting the first
diurnally resolved satellite ocean measurements. Here GOCI retrievals of phytoplankton chlorophyll
concentration and fluorescence are used to evaluate daily to seasonal changes in photophysiological
properties. We focus on nonphotochemical quenching (NPQ) processes that protect phytoplankton from...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
Since June 2010, the Geostationary Ocean Color Imager (GOCI) has been collecting the first diurnally resolved satellite ocean measurements. Here GOCI retrievals of phytoplankton chlorophyll concentration and fluorescence are used to evaluate daily to seasonal changes in photophysiological properties. We focus on nonphotochemical quenching (NPQ) processes that protect phytoplankton from...
Submarine volcanic eruptions can result in both real and apparent changes in marine algal communities, e.g., increases in phytoplankton biomass and/or growth rates that can cover thousands of square kilometers. Satellite ocean color monitoring detects these changes as increases in chlorophyll and particulate backscattering. Detailed, high resolution analysis is needed...
This report summarizes the SeaSoar and CTD observations from R/V Wecoma cruise
W9408A (23 August to 2 September 1994) conducted as part of the Coastal Jet Separation
(CJS) experiment, under funding from the National Science Foundation. The goal of this
study is to establish how and why a strong alongshore...
This report summarizes the Seasoar and CTD observations from Wecoma
cruises W9306A (5 June to 12 July, 1993) and W9308B (14 August to 22 September
1993) conducted as part of the Eastern Boundary Currents Accelerated Research
Initiative, under funding by the Office of Naval Research. The cruises were
designed to...
As part of the Coastal Ocean Processes (CoOP) project Coastal Ocean Advances in Shelf
Transport (COAST), this was the first of two cruises in 2001 to study cross-shelf transport
processes in a wind-driven coastal ocean. The project includes field experiments off the Oregon
coast and coordinated ocean circulation/ecosystem and atmospheric...
As part of the GLOBEC NEP collaborative research project on the California Current (CC),
this was the second of two cruises in 2002 to study the physical and biological oceanographic
distributions and processes that influence juvenile salmonid habitat along the Oregon and northern
California coast. The 2002 cruises followed similar...
An international Coupled Ocean-Atmosphere Response Experiment (COARE)
was conducted in the warm-pool region of the western equatorial Pacific Ocean over a four-month period from November 1992 through February 1993 (Webster and Lukas, 1992). Most of the oceanographic and meteorological observations were concentrated in the Intensive Flux Array (IFA) centered at...
An international Coupled Ocean-Atmosphere Response Experiment
(COARE) was conducted in the warm-pool region of the western equatorial
Pacific Ocean over a four-month period from November 1992 through February
1993 (Webster and Lukas, 1992). Most of the oceanographic and meteorological
observations were concentrated in the Intensive Flux Array (IFA) centered at...