5
views
0
recommends
+1 Recommend
1 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Observing Changes in Ocean Carbonate Chemistry: Our Autonomous Future

      review-article

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Purpose of Review

          We summarize recent progress on autonomous observations of ocean carbonate chemistry and the development of a network of sensors capable of observing carbonate processes at multiple temporal and spatial scales.

          Recent Findings

          The development of versatile pH sensors suitable for both deployment on autonomous vehicles and in compact, fixed ecosystem observatories has been a major development in the field. The initial large-scale deployment of profiling floats equipped with these new pH sensors in the Southern Ocean has demonstrated the feasibility of a global autonomous open-ocean carbonate observing system.

          Summary

          Our developing network of autonomous carbonate observations is currently targeted at surface ocean CO 2 fluxes and compact ecosystem observatories. New integration of developed sensors on gliders and surface vehicles will increase our coastal and regional observational capability. Most autonomous platforms observe a single carbonate parameter, which leaves us reliant on the use of empirical relationships to constrain the rest of the carbonate system. Sensors now in development promise the ability to observe multiple carbonate system parameters from a range of vehicles in the near future.

          Related collections

          Most cited references120

          • Record: found
          • Abstract: found
          • Article: found
          Is Open Access

          Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming

          Ocean acidification represents a threat to marine species worldwide, and forecasting the ecological impacts of acidification is a high priority for science, management, and policy. As research on the topic expands at an exponential rate, a comprehensive understanding of the variability in organisms' responses and corresponding levels of certainty is necessary to forecast the ecological effects. Here, we perform the most comprehensive meta-analysis to date by synthesizing the results of 228 studies examining biological responses to ocean acidification. The results reveal decreased survival, calcification, growth, development and abundance in response to acidification when the broad range of marine organisms is pooled together. However, the magnitude of these responses varies among taxonomic groups, suggesting there is some predictable trait-based variation in sensitivity, despite the investigation of approximately 100 new species in recent research. The results also reveal an enhanced sensitivity of mollusk larvae, but suggest that an enhanced sensitivity of early life history stages is not universal across all taxonomic groups. In addition, the variability in species' responses is enhanced when they are exposed to acidification in multi-species assemblages, suggesting that it is important to consider indirect effects and exercise caution when forecasting abundance patterns from single-species laboratory experiments. Furthermore, the results suggest that other factors, such as nutritional status or source population, could cause substantial variation in organisms' responses. Last, the results highlight a trend towards enhanced sensitivity to acidification when taxa are concurrently exposed to elevated seawater temperature.
            Bookmark
            • Record: found
            • Abstract: found
            • Article: not found

            Evidence for upwelling of corrosive "acidified" water onto the continental shelf.

            The absorption of atmospheric carbon dioxide (CO2) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO2 has increased the areal extent of the affected area.
              Bookmark
              • Record: found
              • Abstract: found
              • Article: found
              Is Open Access

              High-Frequency Dynamics of Ocean pH: A Multi-Ecosystem Comparison

              The effect of Ocean Acidification (OA) on marine biota is quasi-predictable at best. While perturbation studies, in the form of incubations under elevated pCO2, reveal sensitivities and responses of individual species, one missing link in the OA story results from a chronic lack of pH data specific to a given species' natural habitat. Here, we present a compilation of continuous, high-resolution time series of upper ocean pH, collected using autonomous sensors, over a variety of ecosystems ranging from polar to tropical, open-ocean to coastal, kelp forest to coral reef. These observations reveal a continuum of month-long pH variability with standard deviations from 0.004 to 0.277 and ranges spanning 0.024 to 1.430 pH units. The nature of the observed variability was also highly site-dependent, with characteristic diel, semi-diurnal, and stochastic patterns of varying amplitudes. These biome-specific pH signatures disclose current levels of exposure to both high and low dissolved CO2, often demonstrating that resident organisms are already experiencing pH regimes that are not predicted until 2100. Our data provide a first step toward crystallizing the biophysical link between environmental history of pH exposure and physiological resilience of marine organisms to fluctuations in seawater CO2. Knowledge of this spatial and temporal variation in seawater chemistry allows us to improve the design of OA experiments: we can test organisms with a priori expectations of their tolerance guardrails, based on their natural range of exposure. Such hypothesis-testing will provide a deeper understanding of the effects of OA. Both intuitively simple to understand and powerfully informative, these and similar comparative time series can help guide management efforts to identify areas of marine habitat that can serve as refugia to acidification as well as areas that are particularly vulnerable to future ocean change.
                Bookmark

                Author and article information

                Contributors
                sb17@princeton.edu
                Journal
                Curr Clim Change Rep
                Curr Clim Change Rep
                Current Climate Change Reports
                Springer International Publishing (Cham )
                2198-6061
                7 May 2019
                7 May 2019
                2019
                : 5
                : 3
                : 207-220
                Affiliations
                [1 ]ISNI 0000 0001 2097 5006, GRID grid.16750.35, Program in Atmospheric and Oceanic Sciences, , Princeton University, ; 300 Forrestal Road, Sayre Hall, Princeton, NJ 08544 USA
                [2 ]ISNI 0000 0001 0116 3029, GRID grid.270056.6, Monterey Bay Aquarium Research Institute, ; 7700 Sandholdt Road, Moss Landing, CA USA
                [3 ]ISNI 0000 0001 1266 2261, GRID grid.3532.7, Pacific Marine Environmental Laboratory, , National Oceanic and Atmospheric Administration, ; 7600 Sand Point Way, NE, Seattle, WA USA
                Author information
                http://orcid.org/0000-0001-5106-4678
                Article
                129
                10.1007/s40641-019-00129-8
                6659613
                31404217
                a7a2b5c9-01d5-4186-a4e2-16a9379e7345
                © The Author(s) 2019

                Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License ( http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

                History
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/100000001, National Science Foundation;
                Award ID: NSF PLR -1425989
                Funded by: FundRef http://dx.doi.org/10.13039/100000104, National Aeronautics and Space Administration;
                Award ID: NNX17AI73G
                Funded by: Carbon Mitigation Initiative - BP, Princeton University
                Funded by: FundRef http://dx.doi.org/10.13039/100000008, David and Lucile Packard Foundation;
                Funded by: National Academies of Sciences Research Associateship Programs Postdoctoral Fellowship
                Categories
                Carbon Cycle and Climate (K Zickfeld, JR Melton and N Lovenduski, Section Editors)
                Custom metadata
                © Springer Nature Switzerland AG 2019

                autonomous platforms,carbonate observations,ocean acidification,ocean biogeochemical sensors

                Comments

                Comment on this article