https://doi.pangaea.de/10.1594/PANGAEA.996431Hummels, RebeccaRebeccaHummels0000-0002-3746-6213GEOMAR - Helmholtz Centre for Ocean Research KielBrandt, PeterPeterBrandt0000-0002-9235-955XGEOMAR - Helmholtz Centre for Ocean Research KielDengler, MarcusMarcusDengler0000-0001-5993-9088GEOMAR - Helmholtz Centre for Ocean Research KielPANGAEA2026Mooringphysical dataTropical South AtlanticSample code/labelDATE/TIMEDEPTH, waterQuality flag, water depthPressure, waterQuality flag, water pressureTemperature, waterQuality flag, water temperatureSalinityQuality flag, salinityCurrent velocity, east-westQuality flag, current velocityCurrent velocity, north-southMooringM98M106Meteor (1986)Regional Atlantic Circulation and global Change (RACE)Tropical Atlantic Circulation and Overturning at 11°S (TRACOS)2013-07-04T20:00:00/2014-05-14T14:48:46Dataset10.2312/cr_m10610.2312/cr_m9810.1002/2015GL06525410.1029/2020JC016592https://store.pangaea.de/Publications/HummelsR_2026/kpo_1095.zip10.1594/PANGAEA.9251692054304 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThis data set contains quality-controlled observations from a GEOMAR mooring deployment. Depending on the mooring configuration, measurements may include pressure, temperature, conductivity, dissolved oxygen, and current velocity recorded by oceanographic instruments throughout the deployment period.
Data Processing: Instruments equipped with pressure, temperature, conductivity, and oxygen sensors were calibrated in situ immediately before deployment and after recovery by attaching them to the CTD frame during CTD/O2 casts. Sensor readings were compared with calibrated CTDO2 observations during dedicated calibration stops lasting several minutes. Correction terms were derived from the differences between the moored instruments and the CTDO measurements and subsequently applied to the complete deployment records. Calibration-stop results were additionally validated using nearby CTD observations obtained during the deployment (CTD data of deployment cruise: https://doi.org/10.1594/PANGAEA.868640) and recovery cruises (CTD data of recovery cruise: https://doi.org/10.1594/PANGAEA.869361). This procedure enables the detection and correction of potential sensor drift and provides estimates of calibration and measurement uncertainties. Details of the deployment and recovery operations are documented in the corresponding cruise reports.instrument = Label:kpo_1095_02 File:kpo_1095_instr_02.nc Type:Seabird MicroCat 37-SM with pressure SN:06862
instrument = Label:kpo_1095_03 File:kpo_1095_instr_03.nc Type:Seabird MicroCat 37-SM SN:01282 depth/pressure data was at least partially derived and not directly measured, consult quality flags for details
instrument = Label:kpo_1095_04 File:kpo_1095_instr_04.nc Type:Teledyne RDI LongRanger 75 SN:12530
instrument = Label:kpo_1095_05 File:kpo_1095_instr_05.nc Type:Seabird MicroCat 37-SM SN:00921 depth/pressure data was at least partially derived and not directly measured, consult quality flags for details
instrument = Label:kpo_1095_06 File:kpo_1095_instr_06.nc Type:Seabird MicroCat 37-SM SN:00933 depth/pressure data was at least partially derived and not directly measured, consult quality flags for details
instrument = Label:kpo_1095_07 File:kpo_1095_instr_07.nc Type:Nortek Aquadopp Seriell SN:08409
instrument = Label:kpo_1095_08 File:kpo_1095_instr_08.nc Type:Seabird MicroCat 37-SM SN:01288 depth/pressure data was at least partially derived and not directly measured, consult quality flags for details-35.907666666667-35.8685-10.274666666667-10.26983333Federal Ministry of Education and Researchhttps://doi.org/10.13039/50110000234703F0605BRole of the tropical Atlantic for climate variability in the Atlantic sector (RACE I)