Sea water temperature from an ADCP at the Munkholmen buoy in the Trondheim fjord

Sea water CTD measurements at 90 m depth in Trondheim, Norway, with salinity and temperature. netcdf.

Tallink ship Victoria I, with ferrybox system mounted onboard, is traveling (since end of 2023) regularly between Tallinn and Helsinki was appointed for summer of 2024 to Tallinn Mariehamn Stockholm line. During that period there were also some cruises to Visby (starting from Tallinn and via Helsinki).

This datasets includes all the CTD profiles taken by the scientific teams on-board the RV Belgica during the year 2022-2024. The vast majority of the profiles are measured in the Belgian part of the North Sea.

This dataset includes daily measurements of water temperature at Canary Islands Marine Aquaculture Facility tank.

This dataset includes in situ observations of CTDs collected during the FRUELA experiment.

This dataset includes in situ observations of water sampling bottles collected during the PEP 1982 experiment.

The present sumbission includes CTD profiles from GD standard section acquired during STOCA 2012-10 cruise.

The ReZoEnv field campaign was conducted at 9 sites distributed within contrasted seagrass (Zostera notlei) meadows in the Arcachon Bay. This multi-parameter survey was conducted during one year (November 2015 – November 2016). Water levels, temperature and light were recorded every 10 minutes. While bed sediment characteristics (granulometry, water content, organic matter content), seagrass characteristics (coverage, biometry, chlorophyll and CNP content) were measured monthly. Additionally, wind-wave parameters were obtained from high frequency pressure sensor at 4 sites, every 20 minutes. List of sites : ANDE : 44.745091 N, 1.121366 O FONT : 44.722631 N, 1.080133 O GAIL : 44.662573 N, 1.099575 O GARR : 44.705132 N, 1.121562 O HAUT : 44.729331 N, 1.15608 O ILE : 44.683117 N, 1.162716 O JACQ : 44.724563 N, 1.181109 O PASS : 44.689927 N, 1.089491 O ROCH : 44.648529 N, 1.127736 O Important Note: This submission has been initially submitted to SEA scieNtific Open data Edition (SEANOE) publication service and received the recorded DOI. The metadata elements have been further processed (refined) in EMODnet Ingestion Service in order to conform with the Data Submission Service specifications.

Approximately 25% of Antarctic Bottom Water has its origin as dense water exiting the western Ross Sea, but little is known about what controls the release of dense water plumes from the Drygalski Trough. We deployed two moorings on the slope from February, 2018, to January, 2019, to investigate the water properties of the bottom water exiting the region at Cape Adare and the relationship with the seasonal cycle, winds, and tides. Mooring P2 was placed at 1750 metres depth on the slope at Cape Adare at the same location as an earlier deployment of mooring CA1 in the CALM experiment (Gordon et al., 2015). Instruments on P2 were placed at the same depths as CA1 to continue that time series. Mooring P3 was placed on the same isobath on the slope at the mouth of the Drygalski Trough to measure the water properties moving along the slope from the east. Findings from the observations are described in Bowen et al. (2021). Important Note: This submission has been initially submitted to SEA scieNtific Open data Edition (SEANOE) publication service and received the recorded DOI. The metadata elements have been further processed (refined) in EMODnet Ingestion Service in order to conform with the Data Submission Service specifications.