Ocean acidification from below in the Tropical Pacific

2020

Article référencé dans le Web of Science WOS:000566242800001

Ishii M., Rodgers K. B., Inoue H. Y., Toyama K., Sasano D., Kosugi N., Ono H., Enyo K., Nakano T., Iudicone D., Blanke B., Aumont Olivier, Feely R. A.

Global Biogeochemical Cycles, 2020, 34 (8), e2019GB006368 [15 p.] ISSN 0886-6236

Identifying ocean acidification and its controlling mechanisms is an important priority within the broader question of understanding how sustained anthropogenic CO(2)emissions are harming the health of the ocean. Through extensive analysis of observational data products for ocean inorganic carbon, here we quantify the rate at which acidification is proceeding in the western tropical Pacific Warm Pool, revealing -0.0013 +/- 0.0001 year(-1)for pH and -0.0083 +/- 0.0007 year(-1)for the saturation index of aragonite for the years 1985-2016. However, the mean rate of total dissolved inorganic carbon increase (+0.81 +/- 0.06 mu mol . kg(-1) . year(-1)) sustaining acidification was similar to 20% slower than what would be expected if it were simply controlled by the rate of atmospheric CO2 increase and transmitted through local air-sea CO(2)equilibration. Joint Lagrangian and Eulerian model diagnostics indicate that the acidification of the Warm Pool occurs primarily through the anthropogenic CO2 that invades the ocean in the extra-tropics is transported to the tropics through the thermocline shallow overturning circulation and then re-emerges into surface waters within the tropics through the Equatorial Undercurrent from below. An interior residence time of several years to decades, acting in conjunction with the accelerating CO(2)growth in the atmosphere, can be expected to contribute to modulating the rate of Warm Pool acidification.

Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Limnologie physique / Océanographie physique [032]

PACIFIQUE ; ZONE TROPICALE

Fonds IRD [F B010079703]

fdi:010079703