Sustained Observations of Ocean Acidification in Alaska Coastal Seas
Why we care Coastal regions around Alaska experience some of the most rapid and extensive progressions of ocean acidification (OA) in the United States. Assessments indicate that Alaska coastal communities have a varying degree of vulnerability to OA ranging from moderate to severe. Economically vital fishing regions are the most vulnerable. Sustained monitoring is critical to track the extent and impact of ocean acidification in habitats that are home to sensitive species such as red king crab in the Bering Sea.
What we are doing This project “rethinks” the coastal Alaskan OA monitoring effort (initiated in 2015) by sampling Alaska waters directly through the annual population survey program of the Alaska Fisheries Science Center (AFSC). This new vision doubles the spatial footprint of Alaska OA observations, increases the time resolution of these observations, and complements shipboard surveys in Alaska. Carbonate chemistry samples will be combined with fisheries population surveys to assess OA in the habitats of keystone organisms in the Bering Sea and Gulf of Alaska.
Benefits of our work This project enhances our understanding of how the accumulation of anthropogenic carbon dioxide affects the seasonal progression of carbonate carbonate chemistry variables in the Gulf of Alaska. The observations can also be used to validate new OA models developed for the Gulf of Alaska and Bering Sea. Additionally, it can be applied to bioeconomic forecast models of crab and walleye pollock providing insight on how to adapt and build resilience to impacted industries and communities.
Evaluation of OA impacts to plankton and fish distributions in the Gulf of Mexico during GOMECC-4 with a focus on HAB-interactions
Why we care Ocean change in the Gulf of Mexico, including acidification and eutrophication, can impact biodiversity and the flow of energy through ecosystems from microscopic phytoplankton to higher trophic levels like fish. These processes can impact the health of fisheries and coastal ecosystems. This project collects information to evaluate the links between ocean conditions and important species in the Gulf of Mexico.
What we are doing During the 4th Gulf of Mexico Ecosystem and Carbon Cruise (GOMECC-4), scientists collect samples of phytoplankton, zooplankton, and ichthyoplankton to characterize fish distribution and abundance, larval fish condition and diet, microplastic abundance, and harmful algal bloom species. These collections coincide with measurements of acidification, oxygen, and eutrophication to make connections between ocean chemistry and biology.
Benefits of our work This project will help characterize how changes in ocean conditions interact with biological processes like harmful algal bloom formation and ecosystem productivity that are important to local fisheries and stakeholders.
PMEL Sustained Investment Coastal Underway Ocean Acidification Observations (PUO)
Why we care Underway ship measurements of ocean acidification (OA) data on ships of opportunity (SOOP) have proven to be a robust and cost-effective way of expanding OA observations. Ship-based observations provide an understanding of the spatial extent of processes that drive OA. Surface underway observations, in conjunction with coastal moorings and dedicated large-scale surveys, make an important contribution to addressing the hypothesis that acidification varies across space and time as a consequence of local and regional processes.
What we are doing The focus of this project is to sustain existing underway OA monitoring systems on NOAA Ships Oscar Dyson and Bell M. Shimada, which operate along the U.S. West Coast. Project objectives also include sustaining underway OA observations in the equatorial Pacific, upgrading sensor systems, and improving oxygen data collection.
Benefits of our work This project increases high-quality surface water OA data taken underway to accompany NOAA Fisheries cruises. Efforts also improve spatial and temporal coverage of OA measurements, improving our understanding of OA variability along the Pacific coast of North America.
Assessing ecosystem responses of Gulf of Mexico coastal communities to ocean acidification using environmental DNA
Why we care Recent efforts to monitor ocean acidification in the Gulf of Mexico via the Gulf of Mexico Ecosystems and Carbon Cycle (GOMECC) cruises have revealed spatial differences in ocean acidification. While we know that ocean acidification negatively impacts many species and exacerbates the effects of oxygen limitation and harmful algal blooms, there is little work to monitor or predict the effects of ocean acidification on biodiversity. This project employs cutting-edge technology using environmental DNA to assess biodiversity in different conditions in the Gulf of Mexico region.
What we are doing Every organism sheds DNA. This project analyzes environmental DNA (eDNA), which is free-floating or microscopic DNA found in seawater, collected during the 4th GOMECC cruise, to identify biodiversity of bacteria, plankton, and fish in the Gulf of Mexico. eDNA will be compared to ocean properties to draw conclusions about drivers of biodiversity.
Benefits of our work Links between eDNA, ocean acidification, and other ocean properties will provide a deeper understanding of environmental drivers of biodiversity. These relationships can inform predictions of biodiversity patterns and guide the management of key habitats in the Gulf of Mexico, and help us adapt to changing ocean conditions.
Among the NOAA designated Large Marine Ecosystems, the Gulf of Mexico (GOM) remains poorly understood in terms of its current OA conditions, despite its ecological and economic significance. In the northwestern GOM (nwGOM), decadal acidification has been observed in the shelf-slope region, with metabolic production of CO2 contributing to a larger fraction of CO2 accumulation than uptake of anthropogenic CO2, and the observed rate of acidification is significantly greater than that in other tropical and subtropical areas. Unfortunately, whether the observed OA in this region represents a short-term phenomenon or a long-term trend is unknown. It is hypothesized that increasing atmospheric CO2, increasing terrestrial nutrient export due to an enhanced hydrological cycle, and enhanced upwelling due to climate change will cause the continental shelf-slope region in the nwGOM to acidify faster than other tropical and
subtropical seas. In order to test this hypothesis wave gliders, in -stiu sensor along withe underway measurements from research vessels will measure carbonated chemistry in in surface and shallow waters. Modeling will be used tp integrate the chemical signals into the models to hindcast/predict spatia; and temporal variation of the OA signal for the the optimization of monitoring design and implementation.