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Data on temperature, salinity and currents in the water column, sea level trends, wave height and period, wind speed and direction, water turbidity (light attenuation), underwater noise, river flow, and sea-ice coverage.

EMODnet Physics is an upstream ocean data integrating service. It builds on the discovery of data sources or providers and their connection to the EMODnet Physics infrastructure. It provides a single point of access to in situ ocean physics time-series data and vertical profiles, data products and metadata built with common standards, free of charge and no restrictions.
The available parameters cover temperature, salinity and currents profiles, sea level trends, wave height and period, wind speed and direction, water turbidity (light attenuation), underwater noise, river flow, and sea-ice coverage.


EMODnet Physics has successfully designed, organized, and is running operational services that provide ocean physics data and data products built with common standards, free of charge, and without restrictions. The available parameters cover temperature, salinity, and current profiles, sea level trends, wave height and period, wind speed and direction, water turbidity (light attenuation), underwater noise, river flow, and sea-ice coverage.

The data sources can include research institutes that hold data from scientific expeditions, such as ICES; environmental protection agencies that perform routine monitoring surveys; research programs and infrastructures that manage marine monitoring systems (e.g., Argo, OceanSITES, GO-SHIP, etc.) and repeated observations (CTDs) or observatories and networks (e.g., EMSO, SeaDataNet); and private companies that work in the blue economy sector.

The data products consist of collections of in-situ data, reanalysis and trends of parameters, and space and time aggregated in situ data and model outputs.


EMODnet Physics marine data infrastructure originated from the advancements made by the Global Ocean Observing System (GOOS) community, particularly the European component (EuroGOOS), in the development of operational physical oceanography capabilities.

The consortium represents a strong cooperation between the Copernicus Marine Service (CMS) In Situ Thematic Assembly Centre (INS TAC), the SeaDataNet network of National Oceanographic Data Centers (NODCs), the International Council for the Exploration of the Sea (ICES), and the Joint Technical Commission for Oceanography and Marine Meteorology in situ Observations Programme Support Centre (OceanOPS).

EMODnet Physics combines European marine data collection projects with international programs such as Argo, the Data Buoy Cooperation Group (DBCP), OceanSITES, the Global Ocean Ship-based Hydrographic Investigation Program (GO-SHIP), the Global Sea Level Observing System (GLOSS), and the Ship Observation Team (SOT), which comprises the Volunteer Observing Ship (VOS) and Ship of Opportunity Program (SOOP). Additionally, OceanGliders and tagged animals.

However, it is important to acknowledge that the primary investigators, marine technicians, ship's crew, and volunteers who have made and continue to make numerous oceanographic measurements, often under challenging conditions, are responsible for the quality and quantity of the oceanographic data. The institutions that maintain the platforms and the projects that plan, fund, and execute field campaigns and operational ocean monitoring are responsible for the spatial and temporal coverage of the oceanographic profile data. The data managers are responsible for preserving and ensuring the reusability of the data. This vast network, maintained and updated over time, deserves credit for the aggregated data collections available in EMODnet Physics.


EMODnet Physics does not operate any platforms; instead, it serves as the final step in gathering oceanographic data for public dissemination. Data from key European oceanographic repositories and marine infrastructures (such as EuroGOOS, Copernicus Marine Service INSTAC, and SeaDataNet NODCs) are integrated with other available data sources, including the ICES database, PANGAEA repository, the Permanent Service for Mean Sea Level, the SONEL - GNSS data assembly center for Global Sea Level, the Global Sea Level Observing Service, and the European Multidisciplinary Seafloor and Water Column Observatory (EMSO). This integration aims to provide the most comprehensive catalog of in-situ ocean physics data. In this context, EMODnet Physics encourages the adoption of the CC-BY license for data products.

In addition to this federated data management system, EMODnet Physics develops aggregated data products and interoperability services to facilitate machine-to-machine interaction. Datasets are provided with metadata and are downloadable in multiple data formats (netcdf, csv, txt, etc.).

EMODnet Physics catalogs go beyond European borders to offer a comprehensive entry point to global ocean physical observations, covering regions from the Arctic Ocean (International Arctic Buoy Program - IABP) to the Southern Ocean Observing System (SOOS), the Deep Ocean Observing System (DOOS), and the Global Oceans (ARGO, GO-SHIP, etc.).

The available data collections are discoverable based on themes (such as temperature, salinity, and current profiles), platforms (mooring, drifting buoys, tide gauges, etc.), recording age (near-real-time, delayed mode), depth, provider, and area. Each dataset/platform has a dedicated platform page that provides users with metadata, plots, download features, platform products (such as monthly averages and transects), as well as additional information and links to the data provider or program. Data quality information is available in connection with datasets, along with the ability to explore available machine-to-machine services.


Temperature and Salinity in the water column

Temperature is a crucial component of the climate system and its variability in the water column. Sea-surface temperature (SST) has a significant impact on energy, momentum, and gas exchanges between the ocean and atmosphere. Daily variations in SST can exceed 3°C and can lead to changes of over 10 Wm-2 in the surface energy budget in the tropics and subtropics.

Subsurface ocean temperature is a fundamental observation for understanding various ocean phenomena that influence climate, including ocean stratification, circulation, mixed layer dynamics, water mass properties, and coastal shelf-open ocean exchange. Profiling subsurface temperature observation systems also contribute to in-situ validation of satellite observations of surface temperature. Changes in ocean temperature, for instance, can impact the growth rate of farmed fish, as well as the distribution and abundance of wild fish stocks and other economically and socially valuable marine species.

Salinity observations play a role in monitoring the global water cycle, ocean density, mass, and more. These in-situ data are essential inputs for many ocean models, for validating and calibrating remote sensing observations, and for understanding the ocean's role in the global climate system.

EMODnet Physics provides in-situ observations from various catalogues, both European (such as SeaDataNet, CMS, ICES DB, etc.) and international (including MEOP, SOOS, DOOS, IOOS, etc.), linking different platforms with a wide range of spatial and temporal scales.

The EMODnet Physics data collection includes moorings, which offer high temporal resolution at specific locations but have limited spatial resolution due to array density; gliders and tagged animals that provide higher spatial resolution depending on endurance and instrument characteristics; profiling floats (ARGO) that deliver temperature profiles typically from 0-2,000 meters; casts from ship-based Conductivity-Temperature-Depth (CTD) observations along research voyage tracks, providing temperature observations throughout the water column; Expendable probes (xBT) dropped from a network of volunteer commercial vessels along major shipping routes, observing temperature to several hundred meters depth on a roughly seasonal repeat schedule; and surface loads and ferrybox repeated transects, which offer high-resolution sea surface temperature datasets.

Using these in situ data, it is possible to analyze trends, create maps, and generate gridded data products. Examples include the CORA (Coriolis Ocean Dataset for Reanalysis), developed by IFREMER for the Copernicus Marine Service and regularly updated (annually), and the SeaDataNet Regional Climatology products, developed by SeaDataNet partners using DIVA software and periodically updated. 

A near real time picture of the sea surface temperature and salinity  is made available by a dedicated web interactive page.

EMODnet Physics is also offering a SMOS Sea Surface Salinity product developed by the Barcelona Expert Center – CISC for EMODnet.

Sea Surface Currents

The general circulation of the ocean surface plays a significant role in the transport of heat, salt, passive tracers, and ocean pollutants. Ocean currents, in conjunction with atmospheric currents, contribute to the redistribution of equatorial heat content towards the poles. There are two main types of sea currents: surface wind-driven currents and the thermohaline circulation.

The existing surface current observing systems, such as moorings and Lagrangian drifters, capture a substantial portion of this range. EMODnet Physics combines these observations with land-based High-Frequency (HF) radar observations, which provide a high-resolution tool (albeit with limited spatial coverage) for improved understanding of surface currents, eddies, air-sea fluxes, and exchanges between coastal waters and the open ocean. The EMODnet Physics HFR catalogue , which includes approximately 150 antennas, combines the European HFR node observation capacity with global sources, making it one of the most comprehensive sources of HF Radar observations worldwide.

Sea Level

Sea level is considered an Essential Ocean Variable by the Global Ocean Observing System (GOOS). Measurements of sea level along coasts have been conducted since the 19th century using tide gauges.

Tide gauges remain a key method for observing trends in mean sea level, assessing extreme events, making tidal predictions, supporting geodetic applications, and facilitating harbor operations and navigation. Tide gauge measurements are increasingly important for new warning systems for tsunamis and storm surges, as coastal inundation and storm surges can lead to significant flood events and the destruction of property and infrastructure.

Sea level is regarded as one of the most crucial Essential Climate Variables (ECVs), given that its projected evolution over the next few decades is predicted to pose challenges for millions of people, particularly those in vulnerable areas. Continuous monitoring of sea level trends is essential, and EMODnet Physics incorporates different data collections:

European Tide Gauge Stations (EuroGOOS - Tide Gauge task team), which constitute a network of approximately 500 operational stations providing hourly data. These data undergo near-real-time quality control (NRTQC) to identify spikes.

The UNESCO IOC Sea Level Monitoring Service, which comprises a network of over 1,250 operational tide gauges providing near-real-time data that contributes to international tsunami networks. These data are available "as is" and are not quality controlled or intended for research purposes.

The Global Sea Level Observing Systems (GLOSS) core network, consisting of around 300 stations that form the foundation of the global in-situ sea level network. This network ensures even sampling of coastal sea level variation at various time scales.

JRC-TAD tsunami array devices, a network of over 1,000 smart sensors that monitor real-time sea level status at a frequency of one minute, supporting tsunami warning services.

The GLOOS Fast Delivery (FD) and Research Quality (RQD) tide gauge data, operated by the University of Hawaii Sea Level Centre (UHSLC). The database includes 574 stations. FD data are released within 1-2 months of data collection and undergo basic quality control focusing on large level shifts and obvious outliers. FD data is replaced by RQD data as it becomes available, usually 1-2 years after FD.

The Permanent Service for Mean Sea Level (PSMSL) global sea level database, which provides long-term sea level change information from tide gauges and bottom pressure recorders. The database comprises over 2,350 stations and contains monthly and annual mean sea level values.

These in situ data are processed by the PSMSL expert center, which provides relative sea level trend and sea level anomalies products. The relative sea level trends measured by tide gauges reflect local changes in water level plus local vertical land motion. However, these trends are not corrected for land movement. Tide gauge trends are relative to a fixed point on land and can be influenced by land movements caused by earthquakes or ground-water withdrawal. These in-situ trends are part of the EMODnet Physics products collection in the EMODnet GeoViewer.

The absolute sea level is processed using geodetic data from GNSS stations (SONEL). SONEL serves as the GNSS data assembly center for the Global Sea Level Observing System (GLOSS), developed under the auspices of the IOC/UNESCO. Based on the SONEL product, EMODnet Physics offers an absolute sea level trend product.

EMODnet Physics also includes gridded and reanalysis products developed by CMCC for EMODnet Physics. The map  is based on SSALTO/DUACS altimeter products produced and distributed by the Copernicus Marine Service. The satellite trends reflect changes in sea surface height, with most of the spatial variation resulting from the influence of winds blowing over the ocean.

Wave (height and period) - Sea State and Wind (speed and direction)

Sea state refers to the characterization of waves and swells, including their height, wavelength, period, and directional wave energy flux. It is widely recognized that sea state significantly impacts marine safety, marine transport, and the potential for damage to structures. However, the availability of in-situ wave and wind observations remains limited.

EMODnet Physics provides access to these data by integrating multiple data sources, such as the Data Buoy Cooperation Panel, OceanSITES, EuroGOOS regional observations in Europe, and more, into a single catalogue. Operational data are aggregated to provide a synoptic dynamic view of sea state conditions.

River Runoff Data

River runoffs exert a strong influence on their neighboring coastal areas in various ways, such as modifying water stratification, introducing significant fluctuations in circulation patterns, and modulating the impact of upwelling events. However, uncertainties arise due to the global decline of hydrometric networks, which affects the availability of river runoff data and information on water properties like temperature and salinity.

Typically, climatology products of rivers are imposed at the land boundaries of coastal or regional ocean models, overlooking the inter-annual variability in flow and associated properties of rivers. This omission limits our understanding of river dynamics and their impact on coastal areas. River flow fluctuations, from low to high levels, occur frequently and rapidly due to heavy rainfall, disrupting plant life and animal reproduction. These factors are crucial for coastal area management and improved forecasting systems.

EMODnet Physics serves as an in situ hub for accessing operational river runoff data, offering over 600 stations. River runoff data can be accessed through the EMODnet geoviewer and an advanced product that also includes river catchment information.

The EMODnet Physics River runoff  operational product is developed in collaboration with CoLabAtlantic+. The research-quality river data database is operated by the Global Runoff Data Center (GRDC). EMODnet Physics includes a subset of the GRDC, focusing on coastal areas and including only stations located near the river mouths.

Water Clarity (Light Attenuation)

Light attenuation is a significant parameter for determining the photic zone, which refers to the zone with sufficient light for photosynthesis. It is essential for understanding total primary production and the distribution between pelagic and benthic primary production. In addition to working on in-situ data collection of water clarity data, including the availability of a database for parameters such as turbidity, EMODnet Physics offers a Total Suspended Matter (TSM) product.

The TSM product represents the percentage of suspended particles (not dissolved) and is presented as a gridded product. It is based on the CoastColour L2W Concentrations Data, which is obtained from the OC4 algorithm for clear and moderately turbid waters, as well as the CoastColour v1 neural network. The L2W product is then remapped onto a regular grid while maintaining a full resolution of 300 meters. This allows for the generation of products covering European sea basins on a monthly average basis.

The TSM product, developed by CNR – ISMAR for EMODnet Physics, covers the period from 2003 to 2012.

Underwater Noise

Underwater noise, which has adverse effects on the health of marine species and biological productivity, is gaining attention as a form of pollution. Maritime traffic serves as the main source of continuous noise, while impulsive noise sources include pile driving during construction, seismic exploration using airguns, explosions, and sonar systems.

EMODnet Physics provides two products related to underwater noise: the collection of impulsive noise events and the atlas of sites for continuous noise monitoring.

The impulsive noise events are compiled nationally from registers of licensed events, such as pile driving, controlled explosions from naval operations, and other activities that release energy. Most Member States provide these data to the Regional Sea Conventions, contributing to regional assessments of MSFD descriptor 11.1.1 (Low and mid-frequency impulsive noise). Regional registries, operated by ICES (HELCOM, OSPAR) and Centro Tecnologico Naval (Mediterranean Sea), are unified and made available through EMODnet Physics.

These efforts aim to enhance understanding and assessment of underwater noise impacts in different regions.

Guidelines from TG NOISE:

Ice Extent and Ice-type

Sea ice extent and thickness are rapidly decreasing, particularly in the Arctic. This loss of sea ice can have long-lasting effects on the cold branch of the global thermohaline circulation. EMODnet Physics incorporates in-situ data collections from various sources, including the International Arctic Buoy Cooperation Program, the Woods Hole Ice-Tethered Profiler Program, and icebreakers and research vessels operating in the Arctic area (ARICE). Additionally, EMODnet Physics supports the Southern Ocean Observation System (SOOS ) by providing the data backend infrastructure to host and make Southern Ocean data accessible.

The positions of the platforms are superimposed on the sea ice extent in both the Arctic and Antarctic Oceans. Sea ice extent is derived from the SEAICE_GLO_SEAICE_L4_NRT_OBSERVATIONS_011_001 product, which was developed by SIW-METNO-OSLO-NO for the Copernicus Marine Service.