<?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>Global Ocean-Delayed Mode in-situ Observations of surface and sub-surface ocean currents</dc:title>
<dc:creator>INS-CLS-TOULOUSE-FR</dc:creator>
<dc:subject>EARTH SCIENCE&gt;OCEANS&gt;OCEAN TEMPERATURE&gt;WATER TEMPERATURE</dc:subject>
<dc:subject>Oceanographic geographical features</dc:subject>
<dc:subject>in-situ-observation</dc:subject>
<dc:subject>eastward_sea_water_velocity</dc:subject>
<dc:subject>northward_sea_water_velocity</dc:subject>
<dc:subject>upward_sea_water_velocity</dc:subject>
<dc:subject>sea_water_temperature</dc:subject>
<dc:subject>multi-year</dc:subject>
<dc:subject>marine-safety</dc:subject>
<dc:subject>marine-resources</dc:subject>
<dc:subject>coastal-marine-environment</dc:subject>
<dc:subject>weather-climate-and-seasonal-forecasting</dc:subject>
<dc:subject>global-ocean</dc:subject>
<dc:subject>Level 2</dc:subject>
<dc:subject>Not Applicable</dc:subject>
<dc:description>"'Short description: '''Global Ocean - This delayed mode product designed for reanalysis purposes integrates the best available version of in situ data for ocean surface and subsurface currents. Current data from 4 different types of instruments are distributed: * The NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML) Surface Velocity Program (SVP) Drifter’s reprocessing from 1990. It provides the drifter's position, velocity and includes temperature measurements. In addition, a wind slippage correction is provided from 1993. * The near-surface zonal and meridional total velocities, and near-surface radial velocities, measured by High Frequency (HF) radars that are part of the European HF radar Network. These data are delivered together with standard deviation of near-surface zonal and meridional raw velocities, Geometrical Dilution of Precision (GDOP), quality flags and metadata. * The zonal and meridional velocities, at parking depth (mostly around 1000m) and at the surface, calculated along the trajectories of the floats which are part of the Argo Program. * The velocity profiles within the water column coming from Acoustic Doppler Current Profiler (vessel mounted ADCP, Moored ADCP, saildrones) platforms'''DOI (product) :'''https://doi.org/10.17882/86236</dc:description>
<dc:date>2012-08-26T00:00:00.00Z</dc:date>
<dc:type>series</dc:type>
<dc:identifier>INSITU_GLO_PHY_UV_DISCRETE_MY_013_044</dc:identifier>
<dc:language>eng</dc:language>
<dc:rights>No limitations on public access</dc:rights>
</srw_dc:dc>
