http://lod.bco-dmo.org/id/dataset/986667
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2025-10-13
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Dissolved oxygen time series measured on the Overturning in the Subpolar North Atlantic Program (OSNAP) moorings within the boundary currents of the Labrador and Irminger Seas from summer 2020 to summer 2022
2025-10-13
publication
2025-10-13
revision
Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)
2026-04-01
publication
https://doi.org/10.26008/1912/bco-dmo.986667.1
Jaime B. Palter
University of Rhode Island
principalInvestigator
Daaria Atamanchuk
Dalhousie University
principalInvestigator
Isabela Le Bras
Woods Hole Oceanographic Institution
principalInvestigator
David P. Nicholson
Woods Hole Oceanographic Institution
principalInvestigator
Hilary I. Palevsky
Boston College
principalInvestigator
Kristen E. Fogaren
Boston College
principalInvestigator
Clare Johnson
Marum Centre for Marine Environmental Sciences at University Bremen
principalInvestigator
Jannes Koelling
Dalhousie University
principalInvestigator
Margaret Lindeman
University of Southampton
principalInvestigator
Una Kim Miller
University of Rhode Island
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Miller, U. K., Palter, J. B., Fogaren, K. E., Atamanchuk, D., Johnson, C., Koelling, J., Le Bras, I., Lindeman, M., Nagao, H., Nicholson, D. P., Palevsky, H. I., Park, E., Yoder, M. (2026) Dissolved oxygen time series measured on the Overturning in the Subpolar North Atlantic Program (OSNAP) moorings within the boundary currents of the Labrador and Irminger Seas from summer 2020 to summer 2022. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-10-13 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.986667.1 [access date]
Dataset Description: <p>This dataset contains dissolved oxygen time series in two formats: a combined table and individual tables by instrument. The combined table, “986667_v1_oxygen-time-series.csv,” includes the contents of all 60 CSV files contained within Oxygen_time_series-per-instrument.zip, along with metadata from deployment_metadata.csv.</p>
<div>This dataset was supported by NSF-OCE awards 1947829, 1947970, 1947567, 2122579&nbsp;with additional support from the Canada Excellence Research Chair Program (Chairholder Prof. Douglas Wallace) and the&nbsp;Ocean Frontier Institute, through an award from the Canada First Research Excellence Fund (LRP Module B, PI: Prof. Douglas Wallace and HQP Dr. Dariia Atamanchuk)<br />
<br />
OSNAP = Overturning in the Subpolar North Atlantic Program</div>
<div>
<div>GOHSNAP = Gases in the Overturning and Horizontal circulation of the Subpolar North Atlantic Program</div>
</div> Methods and Sampling: <p>Optodes were deployed on moorings within the boundary currents entering and exiting the Labrador Sea, specifically, the Labrador Current in the western Labrador Sea (moorings C1_b, C2_b, C3_b, K7, K8, K9, K10, DSOW 2, and DSOW5), the West Greenland Current in the eastern Labrador Sea (LS1, LS3, LS4, LS5, LS6, LS7, and LS8), and the East Greenland Current in the western Irminger Sea (moorings &nbsp;CF1, CF3, CF4, CF5, CF6, CF7, M1, M2, and M3). These moorings were part of the Overturning in the Subpolar North Atlantic Program (OSNAP) mooring array. &nbsp;Optodes were set to sample every 15 minutes and were deployed from June 2020 - June 2022. &nbsp;LS1, LS3, LS4, LS5, LS6, LS7, and LS8 in the eastern Labrador Sea. Depths of oxygen data collection on the moorings ranged from as shallow as 50 m to as deep as 3500 m, selected to cover the seasonally-stratified, near-surface waters, Labrador Sea Water, Northeast Atlantic Deep Water, and Denmark Strait&nbsp;Overflow Water masses.</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1947829 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1947829
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1947970 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1947970
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1947567 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1947567
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2122579 Award URL: https://www.nsf.gov/awardsearch/show-award/?AWD_ID=2122579
completed
Jaime B. Palter
University of Rhode Island
401-874-6490
University of Rhode Island Graduate School of Oceanography
Kingston
RI
02881-1967
USA
jpalter@uri.edu
pointOfContact
Daaria Atamanchuk
Dalhousie University
dariia.atamanchuk@dal.ca
pointOfContact
Isabela Le Bras
Woods Hole Oceanographic Institution
ilebras@whoi.edu
pointOfContact
David P. Nicholson
Woods Hole Oceanographic Institution
508-289-3547
266 Woods Hole Rd. MS#25
Woods Hole
MA
02543
USA
dnicholson@whoi.edu
pointOfContact
Hilary I. Palevsky
Boston College
617-552-4936
Boston College Dept of Earth and Environmental Sciences 140 Commonwealth Ave
Chestnut Hill
MA
02467
USA
palevsky@bc.edu
pointOfContact
Kristen E. Fogaren
Boston College
Boston College Department of Earth and Environmental Sciences
kristen.fogaren@bc.edu
pointOfContact
Clare Johnson
Marum Centre for Marine Environmental Sciences at University Bremen
clare.johnson@sams.ac.uk
pointOfContact
Jannes Koelling
Dalhousie University
jannes@uw.edu
pointOfContact
Margaret Lindeman
University of Southampton
mlindeman@seas.harvard.edu
pointOfContact
Una Kim Miller
University of Rhode Island
umiller@cornell.edu
pointOfContact
asNeeded
Dataset Version: 1
Unknown
ISO_DateTime_UTC
TEMP
PTEMP
PSAL
PRES
DOXY
DOXY_drift_corrected
filename
serial_number
mooring
osnap_id
depth
location
latitude
longitude
deploy_cruise_id
deploy_date
recovery_cruise_id
recovery_date
P_c
G_1
G_2
reversible_drift
Aanderaa 4330 optodes integrated with RBR loggers
theme
None, User defined
ISO_DateTime_UTC
water temperature at measurement depth
potential temperature
practical salinity
water pressure
dissolved Oxygen
file_name
inst_serial_numb
mooring identification
depth
site description
latitude
longitude
Cruise identfier
date_start
date end
No BCO-DMO term
flag
featureType
BCO-DMO Standard Parameters
Optode
instrument
BCO-DMO Standard Instruments
AR46
AR69-01
AR45
AR69-03
MSM94
M184
service
Deployment Activity
Irminger Sea
Labrador Sea
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Collaborative Research: Gases in the Overturning and Horizontal circulation of the Subpolar North Atlantic Program (GOHSNAP)
https://osprey.bco-dmo.org/project/897705
Collaborative Research: Gases in the Overturning and Horizontal circulation of the Subpolar North Atlantic Program (GOHSNAP)
<p><strong>NSF Award Abstract:</strong><br />
Every winter, frigid winds blowing eastward from the North American continent cool the surface waters of the Labrador Sea, which is situated between Canada and Greenland. As the ocean cools, oxygen and carbon dioxide are mixed from the atmosphere into a thick layer of water that ultimately spreads southward to fill a large volume of the North Atlantic and beyond. The presence of this water mass prevents the North Atlantic anywhere from becoming completely devoid of oxygen. Vertical mixing in the Labrador Sea also redistributes carbon dioxide into the deep ocean, where it can remain for hundreds of years, preventing it from contributing to the greenhouse effect. Yet, the processes governing the uptake of gases by the ocean are not well understood or quantified. Given that, over the last century, the ocean has become steadily more depleted in oxygen while also absorbing a large fraction of anthropogenic carbon dioxide, observing gas exchange processes is essential for understanding and predicting the evolution of the ocean and climate system. The circulation of the Labrador Sea has been monitored since 2014 with an array of instrumented cables extending from the seafloor to nearly the ocean surface. This project adds gas sensors to this array to investigate the rates and processes governing gas exchange. Through this project, a student and postdoc will be trained in interdisciplinary oceanography with a rich network of international collaborators. Responding to the need to increase public ocean literacy, the project scientists will work with University of Rhode Island’s Inner Space Center to broadcast live, interactive science sessions to educators at partner high schools and will follow-up with in-person science cafés at three participating schools.</p>
<p>Given the unique role of the Labrador Sea in providing a pathway for oxygen (O2) and carbon dioxide (CO2) to enter the intermediate depths of the ocean, a quantification and mechanistic understanding of the gas uptake and transport in the basin is a leading scientific priority. Oxygenation of Labrador Sea water prevents large-scale hypoxia from developing anywhere in the Atlantic Ocean and anthropogenic CO2 storage in the basin is the highest in the global ocean. The assumption that, in the Atlantic Ocean, O2 and CO2 uptake and their variability are tied to the dynamics of heat loss and the overturning circulation pervades the literature but has never been evaluated on the basis of direct observations. Thus, GOHSNAP (Gases in the Overturning and Horizontal circulation of the Subpolar North Atlantic Program) addresses this gap and the urgent need to better understand interactions between gas uptake, transport, and the overturning circulation. Specifically, this program will provide a continuous 2-year record of the trans-basin, full water column transport of O2 across the southern boundary of the Labrador Sea, leveraging the mooring infrastructure of the US-lead, international Overturning in the Subpolar North Atlantic Program (OSNAP). The addition of O2 sensors at various depths on this array, supplemented by observations collected by autonomous platforms will allow for the quantification of O2 export from the Labrador Sea. The data will further be used to empirically model carbon concentrations and estimate carbon export. Proposed instruments will also measure the mixed layer O2 and pCO2 for two winters, from which air-sea gas exchange will be calculated and compared against analogous observations in the convective interior of the Labrador Sea.</p>
<p>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.</p>
GOHSNAP
largerWorkCitation
project
Oxygen pathways into the deep ocean: investigating boundary current ventilation in the western Irminger Sea
https://osprey.bco-dmo.org/project/995624
Oxygen pathways into the deep ocean: investigating boundary current ventilation in the western Irminger Sea
<p>NSF Award Abstract:</p>
<p>This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2).<br />
This proposal would fund recovery of deployed oxygen sensors on the OSNAP moorings in the western boundary current of the Irminger Sea, along with deep calibration casts upon recovery, and subsequent processing and analysis of the data. The purpose is to measure O2 that ventilates the deeper boundary current through several pathways leading from the near surface ocean exposed to the atmosphere, into the deeper boundary current, and to investigate the processes responsible. In so doing, the project will also provide information about the pathways of dissolved atmosphere-derived CO2 from the near surface ocean to the deep. Carbon dioxide uptake in the subpolar North Atlantic is thought to significantly mitigate global warming, but as global warming continues, ventilation may decline, potentially weakening this CO2 sink and also reducing oxygen levels throughout the Atlantic. A lack of direct observations of dissolved gases has limited accurate budgeting and hindered understanding of the processes which govern the sequestration of gases into the deep ocean. These results may apply to other ocean regions and inform dissolved gas coupling in ocean and climate models. Broad use of these data will be promoted, to fuel additional advances in the ocean chemistry, ecology, and climate dynamics of this critical region. The project will support an early career female Hispanic/Latina scientist and a graduate student, along with several outreach activities, including documentation of at-sea experience through a blog and interaction with URM student groups.</p>
<p>Carbon dioxide uptake in the subpolar North Atlantic is thought to significantly mitigate global warming; moreover, oxygen uptake in this region prevents large scale hypoxia throughout the North Atlantic. As global warming continues, convection is expected to decline, potentially weakening this CO2 sink and reducing oxygen levels throughout the Atlantic. However, a lack of direct observations of dissolved gases, particularly in winter and in boundary current regions, has limited accurate budgeting and has hindered our understanding of the processes which govern the sequestration of gases into the deep ocean. Careful calibration and analysis of these valuable new O2 observations is planned, to emphasize an understanding of the dynamics underlying boundary current ventilation and interior-boundary current exchange. Science question addressed are: 1) How effectively does slantwise convection directly ventilate boundary currents? 2) How much oxygen reaches the Irminger Sea’s boundary current through the draining of Labrador Sea Water (LSW) from the interior? 3) To what extent does LSW entrainment set the high oxygen levels in Denmark Strait Overflow Water (DSOW)? These results may apply to other ocean regions and inform dissolved gas coupling in ocean and climate models.</p>
<p>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.</p>
Western Irminger ventilation
largerWorkCitation
project
eng; USA
oceans
Irminger Sea; Labrador Sea
-51.9634
-40.275
52.685
60.07
2020-06-23
2022-09-14
From projects that focused on the following 2 locations: 1. Subpolar North Atlantic 2. Western Irminger Sea (east of Greenland and southwest of Iceland)
0
BCO-DMO catalogue of parameters from Dissolved oxygen time series measured on the Overturning in the Subpolar North Atlantic Program (OSNAP) moorings within the boundary currents of the Labrador and Irminger Seas from summer 2020 to summer 2022
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/990187.rdf
Name: ISO_DateTime_UTC
Units: unitless
Description: <p>Datetime with timezone (ISO 8601 format), UTC</p>
http://lod.bco-dmo.org/id/dataset-parameter/990189.rdf
Name: TEMP
Units: degrees Celsius
Description: <p>in-situ temperature</p>
http://lod.bco-dmo.org/id/dataset-parameter/990190.rdf
Name: PTEMP
Units: degrees Celsius
Description: <p>potential temperature</p>
http://lod.bco-dmo.org/id/dataset-parameter/990191.rdf
Name: PSAL
Units: Practical Salinity Units (PSU)
Description: <p>practical salinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/990192.rdf
Name: PRES
Units: decibars (dbar)
Description: <p>pressure</p>
http://lod.bco-dmo.org/id/dataset-parameter/990193.rdf
Name: DOXY
Units: micromoles per kilogram (umol/kg)
Description: <p>Uncalibrated dissolved oxygen</p>
http://lod.bco-dmo.org/id/dataset-parameter/990194.rdf
Name: DOXY_drift_corrected
Units: micromoles per kilogram (umol/kg)
Description: <p>Dissolved oxygen that has been corrected for the instantaneous pressure effect and drift</p>
http://lod.bco-dmo.org/id/dataset-parameter/990195.rdf
Name: filename
Units: unitless
Description: <p>Name of mooring on which the optode was deployed</p>
http://lod.bco-dmo.org/id/dataset-parameter/990196.rdf
Name: serial_number
Units: unitless
Description: <p>Optode serial number</p>
http://lod.bco-dmo.org/id/dataset-parameter/990197.rdf
Name: mooring
Units: unitless
Description: <p>Name of mooring on which the optode was deployed</p>
http://lod.bco-dmo.org/id/dataset-parameter/990198.rdf
Name: osnap_id
Units: unitless
Description: <p>The Overturning in the Subpolar North Atlantic Program (OSNAP) mooring ID</p>
http://lod.bco-dmo.org/id/dataset-parameter/990199.rdf
Name: depth
Units: meters (m)
Description: <p>Depth of optode deployment</p>
http://lod.bco-dmo.org/id/dataset-parameter/990201.rdf
Name: location
Units: unitless
Description: <p>Region of mooring/optode deployment</p>
http://lod.bco-dmo.org/id/dataset-parameter/990202.rdf
Name: latitude
Units: decimal degrees
Description: <p>latitude (Positive north, negative south)</p>
http://lod.bco-dmo.org/id/dataset-parameter/990203.rdf
Name: longitude
Units: decimal degrees
Description: <p>longitude (Positive east, negative west)</p>
http://lod.bco-dmo.org/id/dataset-parameter/990204.rdf
Name: deploy_cruise_id
Units: unitless
Description: <p>Name of research cruise on which the optode/mooring was deployed. AM is Amudsen, AR is Armstrong, MSM is Maria S Merian</p>
http://lod.bco-dmo.org/id/dataset-parameter/990205.rdf
Name: deploy_date
Units: unitless
Description: <p>Date on which the optode/mooring was deployed</p>
http://lod.bco-dmo.org/id/dataset-parameter/990206.rdf
Name: recovery_cruise_id
Units: unitless
Description: <p>Name of the research cruise on which the optode/mooring was recovered. AT is Atlantis, M is Meteor, AR is Armstrong</p>
http://lod.bco-dmo.org/id/dataset-parameter/990207.rdf
Name: recovery_date
Units: unitless
Description: <p>Date on which the optode/mooring was recovered</p>
http://lod.bco-dmo.org/id/dataset-parameter/990208.rdf
Name: P_c
Units: unitless
Description: <p>The pressure correction factor used to correct for the instantaneous pressure effect (see p_fac and correction of instantaneous pressure effect in Miller et al., 2024; 10.3389/fmars.2024.1441976)</p>
http://lod.bco-dmo.org/id/dataset-parameter/990209.rdf
Name: G_1
Units: unitless
Description: <p>Gain correction factor 1 used to correct for irreversible drift. Derived from the deployment cruise cal-dip cast for all optodes except those in which reversible drift was detected. In these cases, the deployment cruise cal-cast was used instead. (See cal-dip, cal-cast, irreversible drift, reversible drift, and drift correction steps in Miller et al., 2024; 10.3389/fmars.2024.1441976)</p>
http://lod.bco-dmo.org/id/dataset-parameter/990210.rdf
Name: G_2
Units: unitless
Description: <p>Gain correction factor 2 used to correct for irreversible drift. Derived from the recovery cruise cal-cast. (See cal-cast, irreversible drift, and drift correction steps in Miller et al., 2024; 10.3389/fmars.2024.1441976)</p>
http://lod.bco-dmo.org/id/dataset-parameter/990211.rdf
Name: reversible_drift
Units: unitless
Description: <p>Flag for the presence and correction of reversible drift (See reversible drift and drift correction steps in Miller et al., 2024; 10.3389/fmars.2024.1441976). 1 is true, 0 is false</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
https://doi.org/10.26008/1912/bco-dmo.986667.1
download
onLine
dataset
<p>Optodes were deployed on moorings within the boundary currents entering and exiting the Labrador Sea, specifically, the Labrador Current in the western Labrador Sea (moorings C1_b, C2_b, C3_b, K7, K8, K9, K10, DSOW 2, and DSOW5), the West Greenland Current in the eastern Labrador Sea (LS1, LS3, LS4, LS5, LS6, LS7, and LS8), and the East Greenland Current in the western Irminger Sea (moorings &nbsp;CF1, CF3, CF4, CF5, CF6, CF7, M1, M2, and M3). These moorings were part of the Overturning in the Subpolar North Atlantic Program (OSNAP) mooring array. &nbsp;Optodes were set to sample every 15 minutes and were deployed from June 2020 - June 2022. &nbsp;LS1, LS3, LS4, LS5, LS6, LS7, and LS8 in the eastern Labrador Sea. Depths of oxygen data collection on the moorings ranged from as shallow as 50 m to as deep as 3500 m, selected to cover the seasonally-stratified, near-surface waters, Labrador Sea Water, Northeast Atlantic Deep Water, and Denmark Strait&nbsp;Overflow Water masses.</p>
Specified by the Principal Investigator(s)
<p>Moored optode oxygen time series processing, calibration, and validation protocols are described in detail in Miller et al. (2024; 10.3389/fmars.2024.1441976). All oxygen time series were corrected for the instantaneous pressure response (Bittig et al., 2018; 10.3389/fmars.2017.00429) and "irreversible" drift using calibrated oxygen profiles collected on "cal-dip" casts, which are shipboard conductivity-temperature-depth-oxygen (CTD-oxygen) casts on which the optodes are strapped to the CTD rosette and dual CTD-oxygen and optode-oxygen profiles are obtained, and &nbsp;"cal-casts", calibrated CTD-oxygen casts taken in the vicinity of the in-water optodes both upon mooring deployment and upon mooring recovery. Optodes deployed at depths greater than 1000 m were checked and where applicable, corrected for pressure-related "reversible" drift. Calibrated oxygen time series were validated against cal-cast profiles external to the calibration process as well as BGC-Argo oxygen profiles collated within a 100 km radius of each mooring.</p>
Specified by the Principal Investigator(s)
* 60 csv files for the oxygen time series were zipped and attached to this dataset as a supplemental file Oxygen_time_series-per-instrument.zip.
* The tables within the 60 csv files were concatenated into the combined table
In the combined table 986667_v1_oxygen-time-series.csv the following changes were also made:
* Additional metadata added from a supplied file "Metadata_with_added_filenames.xlsx"
* Date converted to ISO 8601 format
* Column "TIME" converted to ISO 8601 DateTime with timezone (UTC) format and renamed "ISO_DateTime_UTC"
Supplemental file "deployment_metadata.csv" added from contents of submitted file "Metadata_with_added_filenames.xlsx"
* Duplicate serial number column removed
* Dates converted to ISO format
* Space removed from value in Filename column "CF6_ 1500m_sn204363.csv" so it matches the provided file
Specified by BCO-DMO Data Managers
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
Aanderaa 4330 optodes integrated with RBR loggers
Aanderaa 4330 optodes integrated with RBR loggers
PI Supplied Instrument Name: Aanderaa 4330 optodes integrated with RBR loggers Instrument Name: Optode Instrument Short Name: Instrument Description: An optode or optrode is an optical sensor device that optically measures a specific substance usually with the aid of a chemical transducer.
Cruise: AR46
AR46
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
AR46
Sébastien Bigorre
Woods Hole Oceanographic Institution
Cruise: AR69-01
AR69-01
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
AR69-01
Sheri White
Woods Hole Oceanographic Institution
Cruise: AR45
AR45
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
AR45
Robert S. Pickart
Woods Hole Oceanographic Institution
https://doi.org/10.35090/gatech/66767
Report describing AR45
Cruise: AR69-03
AR69-03
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
AR69-03
Fiamma Straneo
University of California-San Diego Scripps
https://cchdo.ucsd.edu/cruise/33VB20220819
Report describing AR69-03
Cruise: MSM94
MSM94
R/V Maria S. Merian
Community Standard Description
International Council for the Exploration of the Sea
R/V Maria S. Merian
vessel
MSM94
Johannes Karstensen
GEOMAR Kiel
https://www.ldf.uni-hamburg.de/merian/wochenberichte/wochenberichte-merian/msm94-msm97-2/exp-msm94.pdf
Report describing MSM94
Cruise: M184
M184
Community Standard Description
International Council for the Exploration of the Sea
R/V Meteor
vessel
M184
Johannes Karstensen
GEOMAR Kiel
https://www.ldf.uni-hamburg.de/meteor/wochenberichte/wochenberichte-meteor/m181-m190/scr-m184.pdf
Report describing M184
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
R/V Maria S. Merian
Community Standard Description
International Council for the Exploration of the Sea
R/V Maria S. Merian
vessel