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dc.contributor.authorBigorre, Sebastien P.  Concept link
dc.contributor.authorLord, Jeffrey  Concept link
dc.contributor.authorGalbraith, Nancy R.  Concept link
dc.contributor.authorWhelan, Sean P.  Concept link
dc.contributor.authorOtto, William  Concept link
dc.contributor.authorHolte, James W.  Concept link
dc.contributor.authorBariteau, Ludovic  Concept link
dc.contributor.authorWeller, Robert A.  Concept link
dc.coverage.spatial20°S, 85°W
dc.coverage.spatialChile
dc.date.accessioned2012-03-21T14:02:31Z
dc.date.available2012-03-21T14:02:31Z
dc.date.issued2011-09
dc.identifier.urihttps://hdl.handle.net/1912/5088
dc.description.abstractThe Ocean Reference Station at 20°S, 85°W under the stratus clouds west of northern Chile is being maintained to provide ongoing climate-quality records of surface meteorology, air-sea fluxes of heat, freshwater, and momentum, and of upper ocean temperature, salinity, and velocity variability. The Stratus Ocean Reference Station (ORS Stratus) is supported by the National Oceanic and Atmospheric Administration’s (NOAA) Climate Observation Program. It is recovered and redeployed annually, with past cruises that have come between October and January. A NOAA vessel was not available, so this cruise was conducted on the chartered ship, Moana Wave, belonging to Stabbert Maritime. During the 2011 cruise on the Moana Wave to the ORS Stratus site, the primary activities were the recovery of the subsurface part of the Stratus 10 WHOI surface mooring, deployment of a new (Stratus 11) WHOI surface mooring, in-situ calibration of the buoy meteorological sensors by comparison with instrumentation installed on the ship by staff of the NOAA Earth System Research Laboratory (ESRL), and collection of underway and on station oceanographic data to continue to characterize the upper ocean in the stratus region. The Stratus 10 mooring had parted, and the surface buoy and upper part had been recovered earlier. Underway CTD (UCTD) profiles were collected along the track and during surveys dedicated to investigating eddy variability in the region. Surface drifters and subsurface floats were also launched along the track. The intent was also to visit a buoy for the Pacific tsunami warning system maintained by the Hydrographic and Oceanographic Service of the Chilean Navy (SHOA). This DART (Deep- Ocean Assessment and Reporting of Tsunami) buoy had been deployed in December 2010.en_US
dc.description.sponsorshipFunding was provided by the National Oceanic and Atmospheric Administration under Grant No. NA0900AR4320129en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherWoods Hole Oceanographic Institutionen_US
dc.relation.ispartofseriesWHOI Technical Reportsen_US
dc.relation.ispartofseriesWHOI-2011-06en_US
dc.relation.ispartofseriesUpper Ocean Processes Groupen_US
dc.relation.ispartofseriesUOP-2011-02en_US
dc.subjectMoana Wave (Ship) Cruise Stratus 11en_US
dc.subjectMarine meteorologyen_US
dc.subjectOceanographyen_US
dc.titleStratus 11 : Eleventh Setting of the Stratus Ocean Reference Station Cruise on board RV Moana Wave, March 31 - April 16, 2011, Arica - Arica, Chileen_US
dc.typeTechnical Reporten_US
dc.identifier.doi10.1575/1912/5088


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