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Evaluating Carbonate System Algorithms in a Nearshore System: Does Total Alkalinity Matter?
Jonathan M Jones1,2,3, Julia Sweet1, Mark A Brzezinski1,3
1Marine Science Institute, University of California Santa Barbara, Santa Barbara, California, United States of America.
Ocean acidification monitoring is crucial for marine life. While total alkalinity is hard to predict from salinity in nearshore waters, pH and salinity measurements can effectively track changes in dissolved inorganic carbon and saturation state.
Area of Science:
- Marine chemistry
- Oceanography
- Environmental science
Background:
- Ocean acidification poses a significant threat to marine organisms, particularly those with calcium carbonate shells and skeletons.
- Accurate measurement of the marine carbonate system is essential for understanding ocean acidification drivers.
- Logistical challenges often limit regular carbonate system sampling in remote or difficult-to-access nearshore environments.
Purpose of the Study:
- To assess the feasibility of estimating total alkalinity from salinity in shallow nearshore waters (<15 m depth).
- To evaluate the accuracy of calculating carbonate system parameters using salinity-derived total alkalinity compared to direct measurements.
- To determine if autonomous measurements of pH and salinity can effectively monitor coastal ocean acidification trends.
Main Methods:
- Routine water sampling at a pier in southern California to measure carbonate system parameters.
- Comparison of carbonate system parameters calculated from measured values versus estimated total alkalinity (TA) derived from salinity.
- Analysis of the predictability of total alkalinity using salinity and temperature data.
Main Results:
- Total alkalinity was not reliably predictable from salinity or temperature at the studied nearshore site.
- Dissolved inorganic carbon (DIC) and calcium carbonate saturation state were estimated within 5% of measured values using measured pH and salinity-derived or regionally averaged TA.
- The study demonstrated that autonomous measurement of pH and salinity can be a viable method for monitoring coastal changes.
Conclusions:
- Estimating total alkalinity from salinity alone is not universally applicable in all nearshore environments.
- Autonomous measurement of pH and salinity provides a cost-effective and high-frequency method for tracking key indicators of ocean acidification in coastal areas.
- This approach can support long-term monitoring of ocean acidification impacts on marine ecosystems.
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