Internal-wave induced and double-diffusive nutrient fluxes to the nutrient-consuming surface layer in the oligotrophic subtropical North Atlantic

In the literature, an inconsistency exists between estimates of biotically-effected carbon export inferred from large-scale geochemical studies (Jenkins 1982; 47 gC m−2 a−1) and local measurements of turbulent nutrient supply (Lewis et al. 1986; 4 gC m−2 a−1) in the eastern subtropical North Atlanti...

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Bibliographic Details
Published in:Ocean Dynamics
Main Authors: Dietze, Heiner, Oschlies, Andreas, Kähler, Paul
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2004
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/6449/
https://oceanrep.geomar.de/id/eprint/6449/1/518_K%C3%A4hler_2004_InternalwaveInducedAndDoublediffusiveNutrient_Artzeit_pubid5992.pdf
https://doi.org/10.1007/s10236-003-0060-9
Description
Summary:In the literature, an inconsistency exists between estimates of biotically-effected carbon export inferred from large-scale geochemical studies (Jenkins 1982; 47 gC m−2 a−1) and local measurements of turbulent nutrient supply (Lewis et al. 1986; 4 gC m−2 a−1) in the eastern subtropical North Atlantic. Nutrient supply to the upper ocean by turbulent mixing is reexamined using local standard oceanographic measurements and high-resolution vertical profiles of nutrients averaged over a large region directly comparable to that investigated by Jenkins (1982).