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Instituto Español de Oceanografía

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    The tide gauge of Arrecife (Lanzarote) is located in the eastern part of the harbour and it measures the sea level from 1949 onwards.

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    The tide gauge of Ceuta is located in the harbour and it measures the sea level from 1944 onwards.

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    The tide gauge of Palma de Mallorca is located in the eastern part of the harbour and it measures the sea level from 1964 to 1966. Note that another station (PSMSL ID 1892) was recording data from 1997 onwards in a near location.

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    The tide gauge of Santa Cruz de La Palma is located in the harbour and it measured the sea level from 1997 to 2018. This station replaced the previous one (PSMSL ID 585)

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    Temperature monthly climatology for the Iberian Peninsula region, Balearic Islands and Canary Islands, at 0.2º of horizontal spatial resolution and 33 vertical levels.

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    The tide gauge of Pasajes measured the sea level from 1948 to 1963.

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    Operational configuration of ROMS (Regional Ocean Modeling System) off NorthWest Iberia. In this configuration, two grids are nested during online execution. Data from the coarser (4 km horizontal resolution) 236 x 181 grid force the lateral open boundaries of the finer (~1.3 km) 312 x 167 embedded grid. Outputs at hourly and daily temporal resolution.

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    The viewer allows to visualize interactively the zooplankton abundance data obtained monthly in the RADIALES cruises (called RADCAN or RCAN cruises for those carried out since 2013 at the three Cantabrian transects: Santander, Gijón, and Cudillero). The layout displays a sidebar, where you can select the desired option for a series of variables (station, year, plot type, …) and a main panel where the graphs are displayed. It is organized into four tabs: [1] ‘Plot’ displays data from one single station (the complete list of the stations and their geographic coordinates are in https://seriestemporales-ieo.net, and are represented on a map in the fourth tab of this viewer). [2] ‘multipanel’ lays out together in the same figure the individual plots of all the stations, allowing for comparison among them. It allows to select the plot type. [3] ‘Sampling dates’ shows graphically the months, from the starting of the project, with zooplankton abundance data available. [4] 'Stations Map' displays the map with the positions of all stations.

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    The estimation of air-sea CO2 fluxes is largely dependent on wind speed through the gas transfer velocity parameterization. This sketch visualizes this estimation by using data obtained on board an opportunity vessel that transported Citröen cars from/to Vigo (Spain) to/from Saint Nazaire (France), from October 2002 to July 2003. You can explore the spatio-temporal variability of the CO2 flux along the route. Moreover, you can examine the differences in the estimation when a different wind speed source is selected or the algorithm employed to perform the estimation is modified. If you like this sketch or you want to learn more, please, visit and cite our published article in Biogeosciences: Otero, P., X. A. Padin, M. Ruiz-Villarreal, L. M. García-García, A. F. Ríos and F. F. Pérez. Net sea–air CO2 flux uncertainties in the Bay of Biscay based on the choice of wind speed products and gas transfer parameterizations. Biogeosciences, 10, 2993-3005, 2013.

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    The tide gauge of Puerto de la Luz (Las Palmas de Gran Canaria) is located at the reina Sofía dock and it records sea level data from 1949 onwards.