Cruise SR2504 by research vessel Sally Ride in March 2025 had the objective to service moorings for the CCE and CORC projects (California Current Ecosystem, Consortium on the Ocean's Role in Climate), with additional data collections en route in the Southern California Bight. To calibrate and validate the mooring data, CTD casts with water samples were collected. The CTD data are reported here. The CTD data have been quality-controlled and adjusted using the water sample data.

Cruise RL-24-04 by NOAA Ship Reuben Lasker in March/April 2024 had the objective to service moorings for the CCE (California Current Ecosystem) project, as well as the CORC (Consortium on the Ocean's Role in Climate) project. To calibrate and validate the mooring data, CTD casts with water samples were taken. The CTD data are reported here. The CTD data have been quality-controlled and adjusted using the water sample data. The raw instrument data (*.xmlcon and *.hex files from the software by Sea-Bird Scientific) are provided as well.

This dataset contains profile discrete measurements of dissolved inorganic carbon, total alkalinity, pH on total scale, water temperature, salinity, nutrients, and oxygen collected during NOAA Ship Henry B. Bigelow cruise HB2401 (EXPOCODE 33HH20240217) in New York Bight, North Atlantic Ocean, Stellwagen Bank National Marine Sanctuary from 2024-02-17 to 2024-02-22. Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry ultimately resulting in a reduction in pH, a process termed ocean acidification.

There is one bimonthly coral Δ14C timeseries from the western Makassar Strait in the Indonesian Seas, and one bimonthly coral Ba/Ca record from the Northern Lombok Strait in the Indonesian Seas. These data were used to explore the climate drivers of biennial variability, namely the interaction of ENSO and the East Asian Winter Monsoon.

This dataset contains profile discrete measurements of dissolved inorganic carbon, total alkalinity, pH on total scale, water temperature, salinity, nutrients, and oxygen collected during NOAA Ship Henry B. Bigelow cruise HB2403 (EXPOCODE 33HH20240526) in New York Bight, North Atlantic Ocean, Stellwagen Bank National Marine Sanctuary from 2024-05-26 to 2024-06-14. Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry ultimately resulting in a reduction in pH, a process termed ocean acidification.

This dataset contains profile discrete measurements of dissolved inorganic carbon, total alkalinity, pH on total scale, water temperature, salinity, nutrients, and oxygen collected during NOAA Ship Henry B. Bigelow cruise HB2406 (EXPOCODE 33HH20240812) in New York Bight, North Atlantic Ocean, Stellwagen Bank National Marine Sanctuary from 2024-08-12 to 2024-08-22. Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry ultimately resulting in a reduction in pH, a process termed ocean acidification.

This data set consists of dissolved inorganic carbon (DIC), total alkalinity, pH on total scale, nutrients, water temperature, salinity and other variables collected from profile and discrete samples observations during the NOAA Ship Pisces cruise PC2406 (EXPOCODE 334B20241027) in the New York Bight, Northeast U.S. Shelf, North Atlantic Ocean from 2024-10-27 to 2024-11-12. Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry ultimately resulting in a reduction in pH, a process termed ocean acidification.

This dataset consists of Dissolved inorganic carbon, total alkalinity, pH on total scale, and other variables collected from discrete samples and profile observations during the R/V F. G. Walton Smith cruise WS25221 (EXPOCODE 33WA20250809) in the North Atlantic Ocean, Gulf of America from 2025-08-09 to 2025-08-17. Near-shore estuarine and coastal regions are where most recreational fishing and tourism occur, yet they are vastly under-sampled. Their susceptibility to OA is not well understood due to their high biogeochemical variability.

The NOAA/National Environmental Satellite, Data, and Information Service (NESDIS)/Office of Satellite and Product Operations (OSPO) Satellite Analysis Branch provides position and intensity estimates derived from the Dvorak Technique (DT) for tropical disturbances across the globe every 6 hours. This dataset provides SAB's Tropical Cyclone Analysis Worksheet for each system that was classified. Dvorak estimates to include DT, FT, PT, MET and CI T-Numbers as well as position estimates done every six hours, globally.

This dataset contains laboratory experiment data that were collected to examine potential effects of warming and ocean acidification in high latitude marine ecosystems. Warming in high latitude marine ecosystems is leading to the borealization of Arctic communities. Species-specific responses to temperature provide insight into potential co-occurrence or competitive advantage between Arctic and boreal species. Ocean acidification may also lead to unique species-specific responses.