Dataset: OOI Coastal Pioneer New England Shelf Array CTD and Discrete Water Sampling Data from Mooring Overturning Cruises at the New England Continental Shelf from 2013-2022 (OOI Cruise Data Project)

ValidatedFinal no updates expectedDOI: 10.26008/1912/bco-dmo.966896.1Version 1 (2025-07-03)Dataset Type:Cruise Results

Principal Investigator: Albert Plueddemann (Woods Hole Oceanographic Institution)

Data Manager: Andrew Reed (Woods Hole Oceanographic Institution)

BCO-DMO Data Manager: Sawyer Newman (Woods Hole Oceanographic Institution)


Program: Ocean Observatories Initiative (OOI)

Project: OOI Discrete CTD and Water Sampling Cruise Data (OOI Cruise Data)


Abstract

The hydrographic sampling performed by OOI-CGSN (the Ocean Observatories Initiative - Coastal and Global Scale Nodes) as part of each Array turn represents a significant collection of valuable physical, chemical, and biological information. In addition to the CTD, collected hydrographic data include discrete oxygen, salinity, nutrient (nitrate, nitrite, silicate, phosphate, ammonium), chlorophyll, and carbon system measurements. These data serve several important functions. First, they are neces...

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Spatial Extent: N:41.20 E:-70.19 S:39.10 W:-71.42
Temporal Extent: 2014-04-12 - 2022-11-22
The New England Continental Shelf in the western Atlantic Ocean

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OOI-CGSN CTD Sampling Guidelines

In general, water samples are collected for analysis at depths that correspond to instrumentation making in situ measurements.  For example, Near Surface Instrument Frames (NSIFs) have instrumentation that measure dissolved oxygen (DO), salinity (CTD), nitrate (NUTNR), the partial pressure of CO2 (CO2), and chlorophyll a fluorescence, so water samples should be collected at the depth of the NSIF for analyses of all those parameters.  Additionally, as noted above, OOI water sampling data are valid long-term datasets in and of themselves. Thus, some measurement locations are driven by broader science questions.

Soak Time – The CTD rosette should be allowed to equilibrate (e.g., the CTD sensor readout stabilizes) at the desired target depth for at least 1 minute or more depending on conditions.  Longer soak times may occur to accommodate acoustic release testing or other activities.

 

Citing OOI Data

Refer to specific guidance related to citing OOI data on the OOI website at https://oceanobservatories.org/how-to-use-acknowledge-and-cite-data/. 


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Related Publications

Methods

Clayton, T. D., & Byrne, R. H. (1993). Spectrophotometric seawater pH measurements: total hydrogen ion concentration scale calibration of m-cresol purple and at-sea results. Deep Sea Research Part I: Oceanographic Research Papers, 40(10), 2115–2129. doi:10.1016/0967-0637(93)90048-8
Methods

Knapp, G. P., Stalcup, M. C., & Staney, R. J. (1990). Automated oxygen titration and salinity determination. https://doi.org/10.1575/1912/1020
Methods

Wang, Z. A., & Cai, W.-J. (2004). Carbon dioxide degassing and inorganic carbon export from a marsh-dominated estuary (the Duplin River): A marsh CO2pump. Limnology and Oceanography, 49(2), 341–354. doi:10.4319/lo.2004.49.2.0341