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Full text: 15: Strombeobachtungen in der Deutschen Bucht in den Jahren 1956 - 1958

Tuchen et al. 
data and processing protocols are provided by the IRD IMAGO 
‚eam via: https://www.seanoe.org/data/00601/71295/. PIRATA 
moored surface buoy current meter data can be accessed via: 
https://www.pmel.noaa.gov/tao/drupal/disdel/ and high vertical 
resolution PIRATA ADCP data between October 2008 and June 
2009 can be accessed via: www.pmel.noaa.gov/tao/drupal/disdel/ 
adcp_0n23w/index.html. 
AUTHOR CONTRIBUTIONS 
FPT and PB conceived the study. FPT wrote the manuscript, 
nandled the MMP data, and produced the final data product and 
ügure. PB acquired project funding and ship time on research 
zruises to maintain the subsurface mooring. JH, RH, and GK 
handled the KPO (L)ADCP and current meter data. BB and CP 
provided PIRATA (L)ADCP and current meter measurements. 
MM provided additional PIRATA ADCP data. JT developed the 
MMP processing toolbox and helped with early MMP 
deployments. All authors contributed to the discussion of the 
data report, read, and approved the submitted version. 
FUNDING 
This study was funded by EU H2020 under grant agreement 817578 
TRIATLAS project, by the Deutsche Forschungsgemeinschaft as part 
of the Sonderforschungsbereich754 “Climate-Biogeochemistry 
REFERENCES 
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Moored Velocity Observations at 0°N, 23°W 
Interactions in the Tropical Ocean” and through several research 
cruises with RV Meteor, RV Maria S. Merian, RV L’Atalante, and RV 
Sonne and by the Deutsche Bundesministerium für Bildung und 
Forschung (BMBF) as part of the projects RACE (03F06518) and by 
the European Union 7th Framework Programme (FP7) under Grant 
Agreement 603521. Moored velocity observations were acquired in 
cooperation with the PIRATA project supported by NOAA (USA), 
IRD and Meteo-France (France), INPE (Brazil) and the Brazil Navy. 
This research was performed while FPT held an NRC Research 
Associateship Award at NOAA’s Atlantic Oceanographic and 
Meteorological Laboratory. FPT, PB, JH, RH, and GK are grateful 
for continuing support from GEOMAR Helmholtz Centre for Ocean 
Research Kiel. MM acknowledges the support of NOAA; PMEL 
contribution no. 5359. JT's contributions to this study were 
supported by the U.S. National Science Foundation. 
ACKNOWLEDGMENTS 
We thank the captains, crews, scientists and technical groups 
involved in several research cruises to the tropical Atlantic that 
contributed to collecting shipboard and moored data and 
making them freely available. We thank M. Dengler, S.-H. 
Didwischus, J. Fischer, A. Funk, V. Hormann, R. Kopte and 
the IRD IMAGO team for their help with acquiring and 
processing parts of the velocity data. We further thank R. C. 
Perez for comments on an early draft of the manuscript and two 
reviewers for their helpful feedback. 
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une 2022 | Valıume 9 | Article 91097
	        
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