<?xml version="1.0" encoding="UTF-8"?><srw_dc:dc xmlns:srw_dc="info:srw/schema/1/dc-schema" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="info:srw/schema/1/dc-schema http://www.loc.gov/standards/sru/recordSchemas/dc-schema.xsd">
<dc:title>EUROPEAN SEAS GRIDDED L4 SEA SURFACE HEIGHTS AND DERIVED VARIABLES REPROCESSED (1993-ONGOING)</dc:title>
<dc:creator>SL-CLS-TOULOUSE-FR (PM)</dc:creator>
<dc:subject>EARTH SCIENCE&gt;OCEANS&gt;COASTAL PROCESSES&gt;SEA SURFACE HEIGHT</dc:subject>
<dc:subject>Oceanographic geographical features</dc:subject>
<dc:subject>satellite-observation</dc:subject>
<dc:subject>surface_geostrophic_eastward_sea_water_velocity_assuming_sea_level_for_geoid</dc:subject>
<dc:subject>sea_surface_height_above_geoid</dc:subject>
<dc:subject>surface_geostrophic_northward_sea_water_velocity_assuming_sea_level_for_geoid</dc:subject>
<dc:subject>surface_geostrophic_eastward_sea_water_velocity</dc:subject>
<dc:subject>surface_geostrophic_northward_sea_water_velocity</dc:subject>
<dc:subject>sea_surface_height_above_sea_level</dc:subject>
<dc:subject>multi-year</dc:subject>
<dc:subject>coastal-marine-environment</dc:subject>
<dc:subject>weather-climate-and-seasonal-forecasting</dc:subject>
<dc:subject>marine-safety</dc:subject>
<dc:subject>marine-resources</dc:subject>
<dc:subject>black-sea</dc:subject>
<dc:subject>north-west-shelf-seas</dc:subject>
<dc:subject>iberian-biscay-irish-seas</dc:subject>
<dc:subject>global-ocean</dc:subject>
<dc:subject>baltic-sea</dc:subject>
<dc:subject>mediterranean-sea</dc:subject>
<dc:subject>arctic-ocean</dc:subject>
<dc:subject>Level 4</dc:subject>
<dc:subject>Not Applicable</dc:subject>
<dc:description>'''Short description:'''Altimeter satellite gridded Sea Level Anomalies (SLA) computed with respect to a twenty-year [1993, 2012] mean. The SLA is estimated by Optimal Interpolation, merging the L3 along-track measurement from the different altimeter missions available. Part of the processing is fitted to the European Sea area. (see QUID document or http://duacs.cls.fr [http://duacs.cls.fr] pages for processing details). The product gives additional variables (i.e. Absolute Dynamic Topography and geostrophic currents (absolute and anomalies)). It serves in delayed-time applications.This product is processed by the DUACS multimission altimeter data processing system.'''DOI (product):'''https://doi.org/10.48670/moi-00141</dc:description>
<dc:date>2012-08-26T00:00:00.00Z</dc:date>
<dc:type>series</dc:type>
<dc:identifier>SEALEVEL_EUR_PHY_L4_MY_008_068</dc:identifier>
<dc:language>eng</dc:language>
<dc:rights>No limitations on public access</dc:rights>
</srw_dc:dc>
