Long-term trends of pH, alkalinity, and hydrogen ion concentration in an upwelling-dominated coastal ecosystem: Ría de Vigo, NW Spain

Abstract The present study focuses on the Ría de Vigo (NW Spain), a coastal embayment influenced by the Canary Current Upwelling System, which is among the world’s significant Eastern Boundary Upwelling Ecosystems. The research assesses historical changes in the marine carbonate system by generating...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Sara Cameselle, Antón Velo, María Dolores Doval, Daniel Broullón, Fiz F. Pérez
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2024
Subjects:
R
Q
Online Access:https://doi.org/10.1038/s41598-024-68694-z
https://doaj.org/article/44091f23232d416f88a0f435340d56f9
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Summary:Abstract The present study focuses on the Ría de Vigo (NW Spain), a coastal embayment influenced by the Canary Current Upwelling System, which is among the world’s significant Eastern Boundary Upwelling Ecosystems. The research assesses historical changes in the marine carbonate system by generating 25-year weekly time series at six stations . Assessing ocean acidification in the region is complex due to diverse factors influencing coastal carbon dynamics, making predictions more challenging. To capture the specific dynamics in Ría de Vigo, ensembles of Neural Networks were applied. These networks were trained with a data set obtained in several oceanographic cruises, in order to retrieve pH, hydrogen ion concentration and alkalinity, achieving a root mean square error of 0.0272 pH units, 0.588 nmol $$\hbox {kg}^{-1}$$ kg - 1 , and 10.6 $$\upmu$$ μ mol $$\hbox {kg}^{-1}$$ kg - 1 , respectively. Subsequently, time series of the selected variables were generated, applying data of predictors measured at the aforementioned stations . An increase in normalized alkalinity was observed for all stations, except in the surface layer at the innermost location. A decrease in pH and an increase in hydrogen ion concentration were observed for all points, with trends that exceed reported rates of ocean acidification in the open ocean.