Cited by 11Marine and coastal ecosystemsOceanographic and Atmospheric ProcessesClimate variability and models

Simulation of the nitrate seasonal cycle in the equatorial Atlantic Ocean during 1983 and 1984

Loukos, Harilaos, Mémery, Laurent·1999·Journal of Geophysical Research: Oceans

Abstract

We use a three‐dimensional, off‐line geochemical model to simulate the nitrate cycle in the equatorial Atlantic during the years 1983–1984 corresponding to the Français Océan et Climat dans l'Atlantique Equatorial (FOCAL) and Seasonal Response of the Equatorial Atlantic programs. After comparing our simulations with FOCAL data, we investigate interactions between equatorial circulation and biological activity on both seasonal and interannual timescales. Our results suggest that the upwelling of nitrate in the surface layer is strongly dependent on the behavior of both the nitracline and Equatorial Undercurrent (EUC). In the western basin, the equatorial upwelling partly feeds the EUC and has a low signature on surface nitrate. On the contrary, in the eastern basin, where the upwelling core and the nitracline are closer to the surface, vertical advection is the driving mechanism causing seasonal variations of nitrate concentration. Above the EUC, nitrate is transferred to the very surface by vertical diffusion, whereas the contribution by vertical advection is negligible. While slightly cold oceanic conditions prevailed in 1983, a warm anomaly produced by a decrease in trade winds and upwelling was observed in 1984. In our simulations, the significant changes in circulation do not notably alter the seasonal cycle of new production. Consequently, variations of annual primary production between 1983 and 1984 are small (9% decrease in the 2°S–2°N band) compared to the amplitude of the seasonal cycle (twofold variations). Contrary to the Pacific Ocean, where the interannual signal dominates, our results suggests that seasonal variability is the most significant large‐scale signal on primary production in the equatorial Atlantic.

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Crossref · 10.1029/1999jc900084

Cites

52 of 53 references verified1 citation errors · 0 not checkable

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  • The Atlantic equatorial upwelling is a region of enhanced biological production mainly driven by nitrate supply.

    “The Atlantic equatorial upwelling is a region of enhanced biological production mainly driven by nitrate supply (Voituriez and Herbland, 1977;Loukos and Mémery, 1999).”

    From Physical drivers of the nitrate seasonal variability in the Atlantic cold tongue (2020) · cites this paper as Loukos and Mémery, 1999

  • Seasonal variations of chlorophyll in the equatorial Atlantic are primarily related to seasonal variability of nitrate input.

    “In the equatorial Atlantic, the seasonal variations of chlorophyll are thought to be primarily related to seasonal variability of the nitrate input (Voituriez and Herbland, 1977;Loukos and Mémery, 1999).”

    From Physical drivers of the nitrate seasonal variability in the Atlantic cold tongue (2020) · cites this paper as Loukos and Mémery, 1999

Cites

Flagged first, then by citations

Research works printed but not linked: 14

  1. Anderson L. The determination of Redfield ratios for use in global oceanic nutrient cycle models Ph.D. thesis Princeton Univ. Princeton N. J. 1993.
  2. Andrich P. P.Delecluse P.Levy G.Madec A multi‐tasked general circulation model of the ocean Science and Engineering on Cray Supercomputers Proceedings of the Fourth International Symposium 407–428Cray Research Inc. Minneapolis Minnesota 1988.
  3. Blanke B. Couche de mélange dans un modéle tropical de circulation océanique Ph.D. thesis Univ. Pierre et Marie Curie Paris 1992.
  4. Chavez F. P., 1995, Upwelling in the Ocean: Modern Processes and Ancient Records, 149
  5. Chavez F. P., 1995, Upwelling in the Ocean: Modern Processes and Ancient Records, 149
  6. Eppley R. W., 1981, Relations between nutrient assimilation and growth in phytoplankton with a brief review of estimates of growth rate in the ocean, Can. Bull. Fish. Aquat. Sci., 210, 251
  7. Honjo S., 1978, Sedimentation of material in the Sargasso Sea at 5367m, J. Mar. Res., 36, 469
  8. Honjo S., 1980, Material fluxes and modes of sedimentation in the mesopelagic and bathypelagic zones, J. Mar. Res., 38, 53
  9. Marti O. Etude de l'ocèan mondial: Modélisation de la circulation et des traceurs anthropiques Ph.D. thesis Univ. Pierre et Marie Curie Paris 1992.
  10. Merle J., 1980, Variabilité thermique annuelle et interannuelle de locéan Atlantique équatorial Est, lhypothèse dun El Niño Atlantique, Oceanol. Acta, 3, 209
  11. 10.1175/1520-0485(1983)013<0018:POTSUI>2.0.CO;2 · DOI
  12. Toggweiler J. R., 1995, Upwelling in the Ocean: Modern Processes and Ancient Records, 337
  13. Voituriez B., 1983, Océanographie Tropicale, 163
  14. Voituriez B., 1983, Océanographie Tropicale, 185

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Authors
Loukos, H., & Mémery, L.
Venue
Journal of Geophysical Research: Oceans
Published
1999-07-15
Volume
104
Issue
C7
Pages
15549-15573
ISSN
0148-0227 (ISSN-L)
OpenAlex
W1975299795
Cited by
11
References
53
Citations by year
2026: 1 · 2025: 1 · 2023: 1 · 2020: 1
FWCI
1.22
Type
journal article
Language
en
Open access
closed
Locations
  • Journal of Geophysical Research Atmospheres (publishedVersion)
  • HAL (Le Centre pour la Communication Scientifique Directe) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
Keywords
equatorial Atlantic, Equatorial Undercurrent, nitracline, equatorial upwelling, vertical advection, vertical diffusion, primary production, new production, interannual variability, ocean biogeochemistry, FOCAL

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