The Benthic Deepwater Animal Identification Guide is a collection of in situ images of marine animals created from seafloor video taken by NOAA Ocean Exploration in the North Atlantic, North Pacific, and South Pacific Oceans from 2 Aug 2015 to 14 Sept 2019. Video were collected using the remotely operated vehicle (ROV) Deep Discover (D2) deployed from the NOAA Ship Okeanos Explorer. The purpose of this guide is to aid onboard scientists in animal identification, as well as for public interest.

This dataset contains a data product including calculated CO2 system parameters based on the Salish cruise data product (https://www.ncei.noaa.gov/access/ocean-carbon-acidification-data-system…).

This dataset contains water temperature, bottom topography, currents, marine gravity, and sub bottom profiles taken from R/V Kaimei in the North Pacific. Based on the detail seafloor observation by remotely operative vehicles (KM-ROV and BMS), we observed the distribution of deep-sea hydrothermal activities and microbial and macrofaunal communities with the seafloor topography, obtained various types of rocks, sediments, hydrothermal deposits and waters, and animals.

This dataset includes surface underway chemical, meteorological and physical data collected from Autonomous Surface Vehicle (ASV) Saildrone 1033 (EXPOCODE 32DB20210808) in the North Pacific Ocean, Bering Sea from 2021-08-08 to 2021-10-07.

This dataset includes surface underway chemical, meteorological and physical data collected from Autonomous Surface Vehicle (ASV) Saildrone 1034 (EXPOCODE 32DB20210808-2) in the North Pacific Ocean, Bering Sea from 2021-08-08 to 2021-10-08.

The East Coast Ocean Acidification (ECOA-3) Cruise on board the R/V Ronald H. Brown from Newport, took place in the Gulf of Maine and then along the East US coast to Miami. The effort was in support of the coastal monitoring and research objectives of the NOAA Ocean Acidification Program (OAP). The cruise was designed to obtain a snapshot of key carbon, physical, and biogeochemical parameters as they relate to ocean acidification (OA) in the coastal realm.

Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry resulting in a reduction in pH, a process termed ocean acidification. In support of the coastal monitoring and research objectives of the NOAA Ocean Acidification Program (OAP), the South Florida Project Cruises (SFP) are utilized to collect water samples to measure surface water inorganic carbon and hydrographic parameters including nutrients.

Increasing amounts of atmospheric carbon dioxide from human industrial activities are causing changes in global ocean carbon chemistry resulting in a reduction in pH, a process termed ocean acidification. In support of the coastal monitoring and research objectives of the NOAA Ocean Acidification Program (OAP), the South Florida Project Cruises (SFP) are utilized to collect water samples to measure surface water inorganic carbon and hydrographic parameters including nutrients.

This dataset consists of the GLODAPv2.2023 data product composed of data from 1108 scientific cruises covering the global ocean between 1972 and 2021. It includes full depth discrete bottle measurements of salinity, oxygen, nitrate, silicate, phosphate, dissolved inorganic carbon (TCO2), total alkalinity (TAlk), CO2 fugacity (fCO2), pH, chlorofluorocarbons (CFC-11, CFC-12, CFC-113, and CCl4), SF6, and various isotopes and organic compounds. It was created by appending data from 23 cruises to GLODAPv2.2022 (Lauvset et al., 2022, NCEI Accession 0257247).

The Northern North Pacific (NNP) is a resource-rich coastal zone with abundant fisheries and other material resources. The NNP Regional Climatology version 2 replaces the previous version of the NNP RC published in 2013. This NNP Regional Climatology (NNP RC) is based on almost seventy years of observations, and it incorporates a significant amount of data not previously available to the public. The NNP RC version 2, covering a longer time range of seven decades compared to six decades in v 1.