A predictive model for estimating rates of primary production in the subtropical North Pacific Ocean

Abstract A primary production model, specific to the subtropical North Pacific, was developed using productivity and chlorophyll data collected at Station ALOHA (22.75°N, 158.00°W) and measured phytoplankton physiological parameters. The production algorithm is a mechanistic, full spectral model that provides depth-dependent photosynthesis rates. Six years of phytoplankton pigment data were analyzed to derive seasonal cycles and to parameterize chlorophyll a (Chl; monovinyl and divinyl chlorophyll a) versus depth profiles. The Chl profiles fit a Gaussian-type distribution with depth over a constant background concentration equal to mixed-layer values. Maximum Chl concentrations were always found below the surface, and the parameters displayed distinct monthly and seasonal patterns. Photosynthesis versus irradiance experiments were conducted at a number of locations and seasons in the vicinity of Station ALOHA to calculate phytoplankton physiological parameters needed for the computation of primary production rates. Relationships were explored between environmental conditions and the physiological and profile parameters in order to develop algorithms based on remotely sensed sea-surface variables and time of year. These relationships were used to model primary production rates using data collected during the Hawaii Ocean Time-series (HOT) program. The performance of the model and model parameters were tested by comparing modeled results to those measured directly at Station ALOHA by trace metal-clean, in situ 14C incubation techniques. Monthly averaged chlorophyll profile parameters and a constant maximum quantum yield (0.026 mol C(mol quanta)−1) generates an annual production estimate of 168 g C m−2, which closely resembles that measured at Station ALOHA (181 g C m−2) during the same period. The measured and modeled primary production rates for the subtropical North Pacific are twice as high as values derived from Coastal Zone Color Scanner (CZCS) data (60–90 g C m−2) during the period 1978–1986. If the study area near Station ALOHA is representative of most oligotrophic waters, current global estimates of primary production rates have been significantly underestimated.

[1]  R. Bidigare,et al.  Temporal variations in diatom abundance and downward vertical flux in the oligotrophic North Pacific gyre , 1999 .

[2]  E. Venrick Phytoplankton seasonality in the central North Pacific: The endless summer reconsidered , 1993 .

[3]  D. Siegel,et al.  Variability of the effective quantum yield for carbon assimilation in the Sargasso Sea , 2001 .

[4]  K. M. Rajesh,et al.  Distribution of phytoplankton pigments in the Nethravathi estuary , 2002 .

[5]  Ricardo M Letelier,et al.  Seasonal and interannual variations in photosynthetic carbon assimilation at Station , 1996 .

[6]  A. Fowler Validation of annual growth increments in the otoliths of a small, tropical coral reef fish , 1990 .

[7]  J. Marra,et al.  Phytoplankton production in the Sargasso Sea as determined using optical mooring data , 1994 .

[8]  P. Deschamps,et al.  Description of a computer code to simulate the satellite signal in the solar spectrum : the 5S code , 1990 .

[9]  Michael Ondrusek,et al.  Measurements of photophysiological parameters and primary production in the Central North Pacific Ocean , 1997, Other Conferences.

[10]  O. Schofield,et al.  Spectral photosynthesis, quantum yield and blue-green light enhancement of productivity rates in the diatom Chaetoceros gracile and the prymnesiophyte Emiliania huxleyi , 1990 .

[11]  P. Richerson,et al.  Photoinhibition and the diurnal variation of phytoplankton photosynthesis—I. Development of a photosynthesis—irradiance model from studies of in situ responses , 1987 .

[12]  J. Mcgowan,et al.  Mixing and oceanic productivity , 1978 .

[13]  B. Prézelin,et al.  Bio-Optical Models and the Problems of Scaling , 1992 .

[14]  S. Hooker An overview of SeaWiFS and ocean color , 1992 .

[15]  E. Venrick Mesoscale patterns of chlorophyll a in the Central North Pacific , 1990 .

[16]  R. Bidigare,et al.  Temporal variability of phytoplankton community structure based on pigment analysis , 1993 .

[17]  S. Fitzwater,et al.  Metal contamination and its effect on primary production measurements1 , 1982 .

[18]  R. Goericke,et al.  Chlorophylls a and b and divinyl chlorophylls a and b in the open subtropical North Atlantic Ocean , 1993 .

[19]  S. Maritorena,et al.  Bio-optical modeling of primary production on regional scales: the Bermuda BioOptics project , 2001 .

[20]  L. Prieur,et al.  An optical classification of coastal and oceanic waters based on the specific spectral absorption curves of phytoplankton pigments, dissolved organic matter, and other particulate materials1 , 1981 .

[21]  Karen S. Baker,et al.  Oceanic primary production estimates from measurements of spectral irradiance and pigment concentrations , 1987 .

[22]  D. Cayan,et al.  Climate and Chlorophyll a: Long-Term Trends in the Central North Pacific Ocean , 1987, Science.

[23]  Trevor Platt,et al.  Mathematical formulation of the relationship between photosynthesis and light for phytoplankton , 1976 .

[24]  A. Vézina,et al.  Biological Production of the Oceans - the Case for a Consensus , 1989 .

[25]  T. Platt,et al.  Ocean primary production and available light: further algorithms for remote sensing , 1988 .

[26]  Oscar Schofield,et al.  In situ photosynthetic quantum yield. Correspondence to hydrographic and optical variability within the Southern California Bight , 1993 .

[27]  John Marra,et al.  Question of a nutrient effect on the bio-optical properties of phytoplankton , 1994, Other Conferences.

[28]  Oscar Schofield,et al.  Influence of zeaxanthin on quantum yield of photosynthesis of Synechococcus clone WH7803 (DC2) , 1989 .

[29]  David M. Karl,et al.  The Hawaii Ocean Time-series (HOT) program: Background, rationale and field implementation , 1996 .

[30]  R. Bidigare,et al.  Spatial and temporal variability of phytoplankton pigment distributions in the central equatorial Pacific Ocean , 1996 .

[31]  W. Richard,et al.  TEMPERATURE AND PHYTOPLANKTON GROWTH IN THE SEA , 1972 .

[32]  Ricardo M Letelier,et al.  The role of dissolved organic matter release in the productivity of the oligotrophic North Pacific Ocean , 1998 .

[33]  P. Falkowski,et al.  Photosynthetic rates derived from satellite‐based chlorophyll concentration , 1997 .

[34]  P. Falkowski,et al.  Phytoplankton productivity in the North Pacific ocean since 1900 and implications for absorption of anthropogenic CO2 , 1992, Nature.

[35]  Cathrine Myrmehl,et al.  Accounting for the marine reflectance bidirectionality when processing remotely sensed ocean color data , 1994, Other Conferences.

[36]  R. Bidigare,et al.  Distribution of phytoplankton pigments in the North Pacific Ocean in relation to physical and optical variability , 1991 .

[37]  E. Venrick Recurrent Groups of Diatom Species in the North Pacific. , 1971, Ecology.

[38]  Trevor Platt,et al.  Phytoplankton and thermal structure in the upper ocean: Consequences of nonuniformity in chlorophyll profile , 1983 .

[39]  J. Smith,et al.  A Small Volume, Short-Incubation-Time Method for Measurement of Photosynthesis as a Function of Incident Irradiance , 1983 .

[40]  D. Antoine,et al.  Oceanic primary production: 2. Estimation at global scale from satellite (Coastal Zone Color Scanner) chlorophyll , 1996 .

[41]  R. Bidigare,et al.  Phytoplankton photosynthesis parameters along 140°W in the equatorial Pacific , 1995 .

[42]  R. Bidigare,et al.  Long-term changes in plankton community structure and productivity in the North Pacific Subtropical Gyre: The domain shift hypothesis , 2001 .

[43]  James K. B. Bishop,et al.  Surface solar irradiance from the International Satellite Cloud Climatology Project 1983–1991 , 1997 .

[44]  M. Perry,et al.  Maximal quantum yield of photosynthesis in the northwestern Sargasso Sea , 1989 .

[45]  A. Morel Optical modeling of the upper ocean in relation to its biogenous matter content (case I waters) , 1988 .

[46]  André Morel,et al.  Light and marine photosynthesis: a spectral model with geochemical and climatological implications , 1991 .

[47]  André Morel,et al.  Available, usable, and stored radiant energy in relation to marine photosynthesis , 1978 .

[48]  H. A. Matlick,et al.  Diurnal patterns of size-fractioned primary productivity across a coastal front , 1987 .

[49]  Dale A. Kiefer,et al.  In-vivo absorption properties of algal pigments , 1990, Defense, Security, and Sensing.

[50]  Paul G. Falkowski,et al.  Primary Productivity and Biogeochemical Cycles in the Sea , 1992 .

[51]  T. Platt,et al.  An estimate of global primary production in the ocean from satellite radiometer data , 1995 .

[52]  David M. Karl,et al.  Seasonal and interannual variability in primary production and particle flux at Station ALOHA , 1996 .

[53]  H. Claustre,et al.  Variability in the chlorophyll‐specific absorption coefficients of natural phytoplankton: Analysis and parameterization , 1995 .

[54]  Ricardo M Letelier,et al.  Seasonal and interannual variations in photosynthetic carbon assimilation at Station ALOHA , 2003 .

[55]  Curtiss O. Davis,et al.  Photosynthetic characteristics and estimated growth rates indicate grazing is the proximate control of primary production in the equatorial Pacific , 1992 .

[56]  M. D. Keller,et al.  A comparison of HPLC pigment signatures and electron microscopic observations for oligotrophic waters of the North Atlantic and Pacific Oceans , 1996 .

[57]  Daniel J. Repeta,et al.  Improved HPLC method for the analysis of chlorophylls and carotenoids from marine phytoplankton , 1991 .

[58]  Ricardo M Letelier,et al.  Seasonal variability in the phytoplankton community of the North Pacific Subtropical Gyre , 1995 .

[59]  Motoaki Kishino,et al.  Estimation of the spectral absorption coefficients of phytoplankton in the sea , 1985 .