New and Export Productivity Regulation by Si and Fe in the Equatorial Pacific Ocean
NSF: OCE-9712359 / 9802061 / 9802060 / 9802062, 36 months
PROJECT SUMMARY:
To identify and quantify the principal processes that control the partitioning of carbon among oceanic reservoirs and between the ocean and atmosphere on local and regional scales, with a view towards synthesis and prediction on a global scale, is a specific goal of the U.S. JGOFS Synthesis and Modeling Project. As a contribution towards achieving this goal, Drs. Barber, Peng, Chai, Dugdale and Wilkerson will develop an ecosystem model for the equatorial Pacific Ocean, with a focus on how silicate and iron affect new and export productivity and the partitioning of carbon between the atmosphere, surface ocean and deep ocean. The study will use an ecosystem model embedded in a state-of-the-art general circulation model for the equatorial Pacific Ocean to investigate how new and export productivity responds to changing physical and chemical forcing. The domain of the model is between 30S and 30N, 120E and 70W, with real geometry and topography, but analysis will focus on the equatorial region from 5N to 5S. The recent upgrade of supercomputers at North Carolina Supercomputing Center (NCSC) (CrayT90) and Arctic Region Supercomputing Center (ARSC) (Cray-YMP) and the award of several hundred hours of CPU time to Peng, Chai and Barber make it possible to embed an ecosystem model with modest complexity in a high resolution, three dimensional prognostic ocean model, and to conduct numerous experiments on the ecosystem model structure and parameters in a timely and efficient manner.
Phase 1 of the project will modify an existing five-compartment ecosystem model by adding three more compartments (silicate, diatoms and mesozooplanktonic grazers) following the approach of Dugdale et al. The preliminary objective of this three-dimensional Si/N/light model is to reproduce High Nitrate-Low Silicate-Low Chlorophyll (HNLSLC) conditions. With size-dependent growth rate responses in small phytoplankton and diatoms and varying grazing vulnerability, the role of new diatom production regulating on Si and Fe can be thoroughly investigated. Also in Phase 1, TCO2 and total alkalinity (ALK) will be added in order to calculate pCO2. The pre-industrial atmospheric CO2 (280 ppm) will be used to hindcast air-sea flux of CO2 in the equatorial Pacific. New production regulating on silicate should provide a more accurate calculation of CO2 compared to using nitrate as a regulating nutrient.
In Phase 2 the effect of iron is added to the model making a, the initial
slope of the photosynthesis vs. irradiance curve, a function of iron. The
values of a are based on equatorial observations of natural and experimental
iron additions. Independently, Ks for Si(OH4) is made a function
of iron, an effect that involves only diatoms. The `balance to bloom`
transition will be simulated with the two iron effects to reproduce the
IronEx 1 and 2 phytoplankton responses to a transient iron addition.
This modeling study will provide estimates of new and export productivity,
and a formal description of Si and Fe as regulating mechanisms in the equatorial
Pacific Ocean. When new and export productivity is modeled accurately
and validated with JGOFS studies, it will possible to predict with increased
confidence how climate change may alter, via
biogenic export, maintenance
of the air-sea dpCO2 and hence the ocean's uptake and release
of CO2.
Richard Barber
Duke University Marine Laboratory
135 Duke Marine Lab Road
Beaufort NC 28516-9751
tel: (919) 504-7578
fax: (919) 504-7648
rbarber@acpub.duke.edu
Fei Chai
School of Marine Sciences
5741 Libby Hall
University of Maine
Orono, ME 04469-5741
tel: (207) 581-4317
fax: (207) 581-4388
fchai@maine.edu
Richard Dugdale
Romberg Tiburon Center for Environmental Studies
San Francisco State University
PO Box 855
3150 Paradise Drive
Tiburon, CA 94920-0855
tel: (415) 338-3518
fax: (415) 435-7120
rdugdale@sfsu.edu
Frances P. Wilkerson
Romberg Tiburon Center
San Francisco State University
PO Box 855
3150 Paradise Drive
Tiburon, CA 94920
tel: (415) 338-3519
fax: (415) 435-7120
fwilkers@sfsu.edu
Tsung-Hung Peng
Ocean Chemistry Division
NOAA/AOML
4301 Rickenbacker Causeway
Miami, FL 33149-1026
tel: (305) 361-4399
fax: (305) 361-4392
peng@aoml.noaa.gov