Seasonal variability of coastal pH and CO2 using an oceanographic buoy in the Canary Islands
Ocean acidification, caused by the absorption of carbon dioxide (CO 2 ) from the atmosphere into the ocean, ranks among the most critical consequences of climate change for marine ecosystems. Most studies have examined pH and CO 2 trends in the open ocean through oceanic time-series research. The an...
| Published in: | Frontiers in Marine Science |
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| Main Authors: | , , , , |
| Other Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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Frontiers Media SA
2024
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.3389/fmars.2024.1337929 https://www.frontiersin.org/articles/10.3389/fmars.2024.1337929/full |
| Summary: | Ocean acidification, caused by the absorption of carbon dioxide (CO 2 ) from the atmosphere into the ocean, ranks among the most critical consequences of climate change for marine ecosystems. Most studies have examined pH and CO 2 trends in the open ocean through oceanic time-series research. The analysis in coastal waters, particularly in island environments, remains relatively underexplored. This gap in our understanding is particularly important given the profound implications of these changes for coastal ecosystems and the blue economy. The present study focuses on the ongoing monitoring effort that started in March 2020 along the east coast of Gran Canaria, within the Gando Bay, by the CanOA-1 buoy. This monitoring initiative focuses on the systematic collection of multiple variables within the CO 2 system, such as CO 2 fugacity ( f CO 2 ), pH (in total scale, pH T ), total inorganic carbon (C T ), and other hydrographic variables including sea surface salinity (SSS), sea surface temperature (SST) and wind intensity and direction. Accordingly, the study allows the computation of the CO 2 flux (FCO 2 ) between the surface waters and the atmosphere. During the study period, stational (warm and cold periods) behavior was found for all the variables. The lowest SST values were recorded in March, with a range of 18.8-19.3°C, while the highest SST were observed in September and October, ranging from 24.5-24.8°C. SST exhibited an annual increase with a rate of 0.007°C yr -1 . Warmer months increased SSS, while colder periods, influenced by extreme events like tropical storms, led to lower salinity (SSS=34.02). The predominant Trade Winds facilitated the arrival of deeper water, replenishing seawater. The study provided insights into atmospheric CO 2 . Atmospheric f CO 2 averaged 415 ± 4 µatm (2020-2023). Surface water f CO 2sw presented variability, with the highest values recorded in September and October, peaking at 437 µatm in September 2021. The lowest values for f CO 2sw were found in February 2021 (368 ... |
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