Soliciting 2025 East Coast Ocean Acidification Cruise proposals
NOAA OAP solicits proposals to expand capacity on ocean acidification research cruises.
Soliciting 2025 East Coast Ocean Acidification Cruise proposals Read More »
NOAA OAP solicits proposals to expand capacity on ocean acidification research cruises.
Soliciting 2025 East Coast Ocean Acidification Cruise proposals Read More »
This project assesses how ocean acidification impacts microbes and phytoplankton driving the biological carbon pump in the Gulf of America.
How ocean acidification affects microbes and plankton in the Gulf of America Read More »
This project specifically investigates how the observing network is contributing to forecasting models using these complex tools to estimate ocean acidification conditions throughout the central California Current System.
Optimizing the ocean acidification observing system in California Read More »
NOAA’s Ocean Acidification Program announces five projects expanding observational and experimental capacity on two coastal ocean acidification cruises.
OAP supports 5 projects on coastal research cruises Read More »
This project will build a reference material (RM) production facility at NOAA’s Atlantic Oceanic and Meteorological Laboratory (AOML), with the capability to produce RMs for use by NOAA laboratories and affiliated partners.
Building capacity for seawater certified reference materials Read More »
Global ocean physical and chemical trends are reviewed and updated using seven key ocean climate change indicators: (i) Sea Surface Temperature, (ii) Ocean Heat Content, (iii) Ocean pH, (iv) Dissolved Oxygen concentration (v) Arctic Sea Ice extent, thickness, and volume (vi) Sea Level and (vii) the strength of the Atlantic Meridional Overturning Circulation (AMOC). The
We investigated the seasonal carbonate chemistry variability within a semi-enclosed tropical mangrove lagoon in southwestern Puerto Rico. Biweekly measurements of seawater temperature, salinity, total alkalinity (TA), and dissolved inorganic carbon (DIC) were conducted from 2014 to 2018. We describe the possible mechanisms driving the observed variability by correlating the DIC/TA ratio with pH and Ωarg,
In the coastal ocean, local carbonate system variability is determined by the interaction between ocean acidification and local processes. Sporadic observations indicate that biological metabolism, river input, and water mass mixing are dominant local processes driving carbonate system variability in northeast US shelf waters. These processes are also reflected in the variability of observed temperature
Multiple stressors are affecting the Pacific Northwest (PNW) coastal ocean, including harmful algal blooms (HABs), ocean acidification, marine heatwaves, and hypoxia (low oxygen). While these conditions or events are tied to seasonal cycles such as upwelling periods and multiyear cycles such as El Niño/La Niña, they are becoming increasingly frequent and intense. Additionally, they can
Comprehensive sampling of the carbonate system in estuaries and coastal waters can be difficult and expensive because of the complex and heterogeneous nature of near-shore environments. We show that sample collection by community science programs is a viable strategy for expanding estuarine carbonate system monitoring and prioritizing regions for more targeted assessment. ‘Shell Day’ was
Synoptic assessment of coastal total alkalinity through community science Read More »