Dissolution of calcium carbonate: observations and model results in the subpolar North Atlantic

International audience We investigate the significance of in situ dissolution of calcium carbonate above its saturation horizons using observations from the open subpolar North Atlantic [sNA] and to a lesser extent a 3-D biogeochemical model. The sNA is particularly well suited for observation-based...

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Bibliographic Details
Main Authors: Friis, K., Najjar, R. G., Follows, M. J., Dutkiewicz, S., Körtzinger, A., Johnson, K. M.
Other Authors: PennState Meteorology Department, Pennsylvania State University (Penn State), Penn State System-Penn State System, Massachusetts Institute of Technology (MIT), Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
North Atlantic
Online Access:https://hal.science/hal-00297607
https://hal.science/hal-00297607/document
https://hal.science/hal-00297607/file/bg-4-205-2007.pdf
Description
Summary:International audience We investigate the significance of in situ dissolution of calcium carbonate above its saturation horizons using observations from the open subpolar North Atlantic [sNA] and to a lesser extent a 3-D biogeochemical model. The sNA is particularly well suited for observation-based detections of in situ, i.e. shallow-depth CaCO 3 dissolution [SDCCD] as it is a region of high CaCO 3 production, deep CaCO 3 saturation horizons, and precisely-defined pre-formed alkalinity. Based on the analysis of a comprehensive alkalinity data set we find that SDCCD does not appear to be a significant process in the open sNA. The results from the model support the observational findings by indicating that there is not a significant need of SDCCD to explain observed patterns of alkalinity in the North Atlantic. Instead our investigation points to the importance of mixing processes for the redistribution of alkalinity from dissolution of CaCO 3 from below its saturation horizons. However, mixing has recently been neglected for a number of studies that called for SDCCD in the sNA and on global scale.

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