Observations of phytoplankton and nutrients from a Lagrangian drifter off northern California

A Lagrangian drifter was deployed in a cold filament off northern California as part of the Coastal Transition Zone program. The drifter was equipped with an optical package (consisting of a spectroradiometer, a fluorometer, and a beam transmissometer) suspended at 8.5-m depth and a water sampler suspended at 16.3-m depth. The drifter was recovered after 8 days. Optical, chemical, and biological properties changed considerably as the drifter moved offshore in the cold filament. Concentrations of phytoplankton chlorophyll increased rapidly in the first 2 days, in parallel with the disappearance of nitrate and nitrite. After this initial period, chlorophyll decreased gradually over the next 6 days with prominent diurnal fluctuations present in the last 3 days. Water transparency also showed similar long-term as well as diurnal fluctuations. The phytoplankton community became increasingly dominated by large centric diatoms throughout the deployment. Although total cell volume was higher towards the middle of the deployment, this increase occurred without a parallel increase in chlorophyll. In addition, total particulate concentrations were highest nearshore. Although the drifter slippage was approximately 1 cm/s, the biological, chemical, and physical characteristics of the water were affected by both in situ changes and vertical motions of the water. These results are generally consistent with results from other up welling studies.

[1]  A. Huyer,et al.  CTD and velocity surveys of seaward jets off northern California, July 1981 and 1982 , 1986 .

[2]  R. Davis,et al.  Moored wind, temperature, and current observations made during Coastal Ocean Dynamics Experiments 1 and 2 over the Northern California Continental Shelf and upper slope , 1987 .

[3]  E. Traganza,et al.  Nutrient Mapping and Recurrence of Coastal Upwelling Centers by Satellite Remote Sensing: Its Implication to Primary Production and the Sediment Record , 1983 .

[4]  Libe Washburn,et al.  The evolving structure of an upwelling filament , 1985 .

[5]  B. Jones,et al.  The asymmetric distribution of chlorophyll associated with a coastal upwelling center , 1988 .

[6]  L. Pietrafesa,et al.  High frequency sampling of the 1984 spring bloom within the mid-Atlantic Bight: Synoptic shipboard, aircraft, and in situ perspectives of the SEEP-I experiment , 1988 .

[7]  Kenneth H. Brink,et al.  The Coastal Transition Zone program , 1991 .

[8]  Kathryn A. Kelly,et al.  The influence of winds and topography on the sea surface temperature patterns over the northern California slope , 1985 .

[9]  M. Abbott,et al.  Spatial and temporal variability of phytoplankton pigment off northern California during Coastal Ocean Dynamics Experiment 1 , 1987 .

[10]  Russ E. Davis,et al.  Drifter observations of coastal surface currents during CODE: The statistical and dynamical views , 1985 .

[11]  Tommy D. Dickey,et al.  The Biowatt Bio‐Optical and Physical Moored Program , 1986 .

[12]  M. Estrada Phytoplankton distribution and composition off the coast of Galicia (northwest of Spain) , 1984 .

[13]  P. Kosro Structure of the coastal current field off northern California during the Coastal Ocean Dynamics Experiment , 1987 .

[14]  T. Whitledge,et al.  Observations of chlorophyll concentrations off Long Island from a moored in situ fluorometer , 1983 .

[15]  J. Simpson Air-sea exchange of carbon dioxide and oxygen induced by phytoplankton: methods and interpretation , 1985 .

[16]  Thomas M. Powell,et al.  In situ response of phytoplankton fluorescence to rapid variations in light1 , 1982 .

[17]  C. Mooers,et al.  Genetic tracers of zooplankton transport in coastal filaments off northern California , 1989 .

[18]  Tommy D. Dickey,et al.  Optical determination of particulate abundance and production variations in the oligotrophic ocean , 1989 .

[19]  M. Fukuchi,et al.  A phytoplankton bloom and associated processes observed with a long-term moored system in antarctic waters , 1988 .

[20]  R. Spinrad A calibration diagram of specific beam attenuation , 1986 .

[21]  A. Robinson,et al.  Turbulent Jets and Eddies in the California Current and Inferred Cross-Shore Transports , 1984, Science.

[22]  B. Mitchell,et al.  Development of Moored Oceanographic Spectroradiometer , 1987 .

[23]  Graham P. Harris,et al.  The relationship between chlorophyll a fluorescence, diffuse attenuation changes and photosynthesis in natural phytoplankton populations , 1980 .

[24]  Russ E. Davis,et al.  Drifter observations of coastal surface currents during CODE: The method and descriptive view , 1985 .

[25]  B. Jones,et al.  Observations of a Persistent Upwelling Center off Point Conception, California , 1983 .

[26]  William J. Emery,et al.  Satellite Observations and Modeling of Meanders in the California Current System off Oregon and Northern California , 1984 .

[27]  C. R. Booth,et al.  Moorable Spectroradiometers In The BIOWATT Experiment , 1988, Defense, Security, and Sensing.

[28]  Dale A. Kiefer,et al.  Chlorophyll a fluorescence in phytoplankton: relationship to photosynthesis and biomass , 1985 .

[29]  D. Kiefer,et al.  Fluorescence properties of natural phytoplankton populations , 1973 .

[30]  J. Ronald,et al.  A Transmissometer For Profiling And Moored Observations In Water , 1978, Optics & Photonics.

[31]  Brian J. Rothschild,et al.  Toward a theory on biological-physical interactions in the world ocean , 1988 .

[32]  Russ E. Davis,et al.  Water-following characteristics of a mixed layer drifter , 1987 .

[33]  T. Dickey Recent Advances and Future Directions in Multi-Disciplinary In Situ Oceanographic Measurement Systems , 1988 .

[34]  R. W. Austin,et al.  Beam Transmissometers for Oceanographic Measurements , 1974 .

[35]  G. Friederich,et al.  An Inexpensive Moored Water Sampler for Investigating Chemical Variability , 1986 .

[36]  James K. B. Bishop,et al.  The correction and suspended particulate matter calibration of Sea Tech transmissometer data , 1986 .

[37]  James W. Brown,et al.  A semianalytic radiance model of ocean color , 1988 .

[38]  M. Abbott,et al.  Satellite observations of phytoplankton variability during an upwelling event , 1985 .

[39]  D. Blasco,et al.  Primary production cycle in an upwelling center , 1985 .

[40]  R C Smith,et al.  Oceanographic biooptical profiling system. , 1984, Applied optics.

[41]  D. Mackas,et al.  A performance comparison for two lagrangian drifter designs , 1989 .

[42]  Andrew J. Willmott Forced double Kelvin waves in a stratified ocean , 1984 .

[43]  R. Eppley,et al.  PLANKTON POPULATIONS AND UPWELLING OFF THE COAST OF PERU, JUNE 1969 , 1971 .