One-dimensional ecosystem model of the equatorial Pacific upwelling system. Part II: Sensitivity analysis and comparison with JGOFS EqPac data

Deep-Sea Research Part II: Topical Studies in Oceanography

Volumn 49, Issue 13-14, 2002, Pages 2747-2768

  Dugdale, R C ^a   Barber, R T ^b   Chai, F ^c   Peng, T H ^d   Wilkerson, F P ^a  

^a SAN FRANCISCO STATE UNIVERSITY   (United States)

^b DUKE UNIVERSITY MARINE LABORATORY   (United States)

^c UNIVERSITY OF MAINE   (United States)

^d ATLANTIC OCEANOGRAPHIC AND METEOROLOGICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

AMMONIA; CARBON; ECOSYSTEMS; NUTRITION; SEDIMENTS; SILICON COMPOUNDS; SURFACE PHENOMENA;

GRAZERS;

OCEANOGRAPHY;

DIATOM; ECOSYSTEM MODELING; GRAZING; NUTRIENT; PHYTOPLANKTON; SENSITIVITY ANALYSIS; UPWELLING;

PACIFIC OCEAN;

BACILLARIOPHYTA;

EID: 0036078599     PISSN: 09670645     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0967-0645(02)00056-5     Document Type: Article

References (41)

1. Regulation of primary productivity rate in the equatorial Pacific
2. Primary productivity and its regulation in the equatorial Pacific during and following the 1991-1992 El Niño
3. Spatial and temporal variability of phytoplankton pigment distributions in the central equatorial Pacific Ocean
4. Biomass, growth rates and limitation of Equatorial Pacific diatoms
5. 3 condition in the equatorial Pacific
6. One-dimensional ecosystem model of the equatorial Pacific upwelling system. Part I: Model development and silicon and nitrogen cycle
7. Growth rates, grazing, sinking and iron limitation of equatorial Pacific phytoplankton
8. Phytoplankton variability in the central and eastern tropical Pacific
9. A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean
10. Photosynthetic characteristics and estimated growth rates indicate grazing is the proximate control of primary production in the equatorial Pacific
11. Silicate regulation of new production in the equatorial Pacific upwelling
12. Estimating new production in the equatorial Pacific Ocean at 150°W
13. The role of a silicate pump in driving new production
14. Silicon-nitrogen coupling in the equatorial Pacific upwelling zone
15. 2 distributions and sea-air fluxes in the central and eastern equatorial Pacific during the 1991-1994 El Niño
16. Long waves and primary productivity variations in the equatorial Pacific at 0°, 140°W
17. Grazing and iron limitation in the phytoplankton stock and nutrient concentration: A chemostat analogue of the Pacific equatorial upwelling zone
18. Micro-phytoplankton at the equatorial Pacific (140°W) during the JGOFS EqPac time series studies: March to April 1992
19. What controls dissolved iron concentrations in the world ocean?
20. The 1991-1993 El Niño in the central Pacific
21. 228Ra-derived nutrient budgets in the upper equatorial Pacific and the role of "new" silicate in limiting productivity
22. Iron and grazing constraints on primary production in the central equatorial Pacific: An EqPac synthesis
23. An iron-based ecosystem model of the central equatorial Pacific
24. A distribution of nitrate, phosphate and silicate in the world oceans
25. Silicon limitation of biogenic silica production in the equatorial Pacific
26. An ecosystem model with iron limitation of primary production in the equatorial Pacific at 14°W
27. New production along 140°W in the equatorial Pacific during and following the 1992 El Niño event
28. Net community production in "High Nutrient-Low Chlorophyll" waters of the tropical and Antarctic Oceans: Grazing versus iron hypothesis
29. La technique de la culture contnue: Theorie at applications
30. A US JGOFS process study in the equatorial Pacific (EqPac): Introduction
31. 234Th approach
32. Primary productivity and size structure of phytoplankton biomass on a transect of the equator at 135°W in the Pacific Ocean
33. The equatorial Pacific Ocean: Grazer controlled phytoplankton populations in an iron-limited ecosystem
34. Carbon and nitrogen uptake and export in the equatorial Pacific at 150°W: Evidence of an efficient regenerated production cycle
35. Export flux of particles at the equator in the western and central Pacific Ocean
36. Primary productivity and trace metal contamination measurements from a clean rosette system versus ultra-clean Go-Flo bottles
37. Herbivory as a factor in patterns of nutrient utilization in the sea
38. An estimate of equatorial upwelling in the Pacific