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Metadata Report for BODC Series Reference Number 2310321


Metadata Summary

Data Description

Data Category Currents -subsurface Eulerian
Instrument Type
NameCategories
Nortek Aquadopp 3D Doppler current meter  current meters; water temperature sensor
Instrument Mounting subsurface mooring
Originating Country United Kingdom
Originator Dr Lewis Drysdale
Originating Organization Scottish Association for Marine Science
Processing Status QC in progress
Online delivery of data Download not available
Project(s) UK-OSNAP
CLASS Project
AtlantiS
 

Data Identifiers

Originator's Identifier RTWB2_07/6276
BODC Series Reference 2310321
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2022-07-17 15:00
End Time (yyyy-mm-dd hh:mm) 2024-07-11 11:00
Nominal Cycle Interval 3600.0 seconds
 

Spatial Co-ordinates

Latitude 57.47073 N ( 57° 28.2' N )
Longitude 12.31158 W ( 12° 18.7' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 1002.0 m
Maximum Sensor or Sampling Depth 1002.0 m
Minimum Sensor or Sampling Height 787.0 m
Maximum Sensor or Sampling Height 787.0 m
Sea Floor Depth 1789.0 m
Sea Floor Depth Source DATAHEAD
Sensor or Sampling Distribution Fixed common depth - All sensors are grouped effectively at the same depth which is effectively fixed for the duration of the series
Sensor or Sampling Depth Datum Sea floor reference - Depth measured as a height above sea floor but converted into a depth relative to the sea surface according to the same datum as used for sea floor depth (applicable to instrument depths not bathymetric depths)
Sea Floor Depth Datum Instantaneous - Depth measured below water line or instantaneous water body surface
 

Parameters

No Parameters for BODC Reference Number = 2310321

Definition of Rank

  • Rank 1 is a one-dimensional parameter
  • Rank 2 is a two-dimensional parameter
  • Rank 0 is a one-dimensional parameter describing the second dimension of a two-dimensional parameter (e.g. bin depths for moored ADCP data)

Problem Reports

No Problem Report Found in the Database


Data Access Policy

Open Data

These data have no specific confidentiality restrictions for users. However, users must acknowledge data sources as it is not ethical to publish data without proper attribution. Any publication or other output resulting from usage of the data should include an acknowledgment.

If the Information Provider does not provide a specific attribution statement, or if you are using Information from several Information Providers and multiple attributions are not practical in your product or application, you may consider using the following:

"Contains public sector information licensed under the Open Government Licence v1.0."


Narrative Documents

BODC processing of Nortek moored current meter data from cruise JC238, UK-OSNAP / Ellett Array moorings EB1, WB1, and WB2, July 2022 to July 2024

The mooring data were supplied to BODC as ASCII files and converted to BODC internal format (QXF). During transfer the originator's variables were mapped to unique BODC parameter codes. The following table shows the parameter mapping:

Originator's Variable Originator's Units BODC Parameter Code BODC's Units Comments
YY yyyy AADYAA01 Days (UTAA)
MM mm AADYAA01 Days (UTAA)
DD dd AADYAA01 Days (UTAA)
HH hh AAFDZZ01 Days (UTAA)
T °C TEMPPR01 Degrees Celsius (UPAA)
P dbar PREXPR01 Decibars (UPDB)
U cm s-¹ LCEWZZ01 Centimetres per second (UVBB)
V cm s-¹ LCNSZZ01 Centimetres per second (UVBB)
W cm s-¹ LRZAZZZZ Centimetres per second (UVBB)
USS counts ISCMBMA1 Dimensionless (UUUU)
VSS counts ISCMBMA2 Dimensionless (UUUU)
WSS counts ISCMBMA3 Dimensionless (UUUU)
PIT degrees PTCHFG01 Degrees (UAAA) +/- 180 degrees
ROL degrees ROLLFG01 Degrees (UAAA) +/- 180 degrees
IPOW V BTVOLTCM Volts (UVLT)
HDG degrees HEADCMMG Degrees (UAAA)

Following transfer the data were screened using BODC in-house visualisation software. No data quality flags assigned by BODC automatic systems or manually by data manager inspection.

The following observations should be noted:
- The accuracy and resolution of sensors on legacy Aquadopp models is reported by manufacturer to be reduced when instrument pitch/roll exceeds 20 degrees, whereas model 2 units are rated for tilts up to 30 degrees. Some pitch/roll measurements exceed 20 degrees on some sensors therefore resolution on these data may be reduced.
- Potential sensor drift observed in pressure sensors for moorings EB1 sensor 6242 (5-6 dbar), WB2 sensor 6276 (~12 dbar), 6534 (~5 dbar), and 6723 (~6dbar)
- Unusual progressive 5-6 dbar decrease in pressure for mooring WB1 sensor 11997 over the first month of data collection which takes 3-4 months to potentially stabilise
- Significant spikes in pressure recorded on all moorings across data collection period with amplitudes up to or exceeding 100 dbar over periods of days to weeks. These spikes are fairly consistent across sensors on each mooring and likely represent physical oceanographic phenomena rather than sensor malfunction. Data users advised to rely on pressure measurements rather than indicative or nominal instrument deployment depths.

Originator processing of Nortek moored current meter data from cruise JC238, UK-OSNAP / Ellett Array moorings, July 2022 to July 2024

Sampling Strategy

During the RRS James Cook cruise JC238, Nortek Aquadopps were deployed on the UK-OSNAP Rockall Trough moorings: 6 at the RTEB1 site, 5 at the RTWB1 site, and 3 at the RTWB2 site. Additionally, Nortek Aquadopps were deployed on the UK-OSNAP Iceland Basin moorings: 3 at the IB3 site, 3 at the IB4 site, and 2 at the IB5 site.

Prior to deployment, their clocks were synchronised with GPS time, new batteries fitted, and a functional check was performed. They were set to record temperature, pressure, velocity, heading, pitch, and roll every hour.

These moorings were recovered during the RRS Discovery cruise DY181.

Mooring site Mooring location (latitude, longitude) Water depth (m) Deployment time (GMT) Recovery time (GMT)
RTEB1 57.1001, -9.5642 1800 16/07/2022 12:00 10/07/2024 06:50
RTWB1 57.4696, -12.7048 1581 19/07/2022 10:30 12/07/2024 09:10
RTWB2 57.4707, -12.3116 1789 17/07/2022 15:00 11/07/2024 11:40
IB3 58.0155, -24.4220 2822 24/07/2022 15:30 18/07/2024 08:00
IB4 57.9890, -21.1466 2898 22/07/2022 17:30 16/07/2024 07:00
IB5 57.8010, -19.1695 936 21/07/2022 12:00 15/07/2024 08:00

Data Acquisition and Initial Processing

After recovery the data were downloaded from the instruments and the clock offsets checked with no significant drift found. One instrument (Serial Number 11021 on IB4) was flooded and the data could not be retrieved. For the remaining datasets the following processing steps were followed:

  1. Removal of launch and recovery periods from dataset.
  2. Correction for magnetic declination.
  3. Correction for sound speed.
  4. Automatic de-spiking using a spike/mean ratio of 10.

After recovery, the compass data for SN 6273 (1770 m) from EB1 appeared suspicious, therefore all data from this sensor were considered bad. Data for this sensor was subsequently omitted, and the remaining 5 sensors' data were retained.

More detailed information regarding the processing can be found in the DY181 cruise report on pp. 67-70.

The processed data were supplied to BODC for banking.


Project Information

UK - Overturning in the Subpolar North Atlantic Programme (UK-OSNAP) Programme

UK-OSNAP is part of an international collaboration to establish a transoceanic observing system in the subpolar North Atlantic. The aim is to quantify and understand the Subpolar Gyre's response to local and remote forcing of mass, heat and freshwater fluxes, within the conceptual framework of the Atlantic Meridional Overturning Circulation (AMOC).

UK-OSNAP is developing a new observing system to provide a continuous record of full-depth, trans-basin mass, heat, and freshwater fluxes. Combining these sustained measurements with innovative modelling techniques will enable the project to characterise the circulation and fluxes of the North Atlantic Subpolar Gyre.

UK-OSNAP is funded by the Natural Environment Research Council (NERC). The project is led by the National Oceanography Centre (NOC) with partners in the University of Liverpool, the University of Oxford and the Scottish Association for Marine Science (SAMS). It is a part of international OSNAP that is led by USA and includes 10 further partner groups in Canada, France, Germany, the Netherlands and China. The project involves fieldwork at sea and model studies.

The OSNAP observing system consists of two legs: one extending from southern Labrador to the southwestern tip of Greenland across the mouth of the Labrador Sea (OSNAP West), and the second from the southeastern tip of Greenland to Scotland (OSNAP East). The observing system also includes subsurface floats (OSNAP Floats) in order to trace the pathways of overflow waters in the basin and to assess the connectivity of currents crossing the OSNAP line.

NERC have added an extension to UK-OSNAP, until October 2024. This will result in the UK-OSNAP-Decade: 10 years of observing and understanding the overturning circulation in the subpolar North Atlantic (2014-2024). UK-OSNAP Decade forms part of the wider UK-OSNAP programme. Although supported through separate funding streams, including the Collective Funds 'Changing North Atlantic' grant, OSNAP decade (NE/T00858X/1), is considered a continuation of the core programme. In line with this, activities and associated data are grouped under UK-OSNAP, with funding details recorded here rather than as a separate project.


Marine LTSS: CLASS (Climate Linked Atlantic Sector Science)

Introduction

CLASS is a five year (2018 to 2023) programme, funded by the Natural Environment Research Council (NERC) and extended until March 2024.

Scientific Rationale

The ocean plays a vital role in sustaining life on planet Earth, providing us with both living resources and climate regulation. The trajectory of anthropogenically driven climate change will be substantially controlled by the ocean due to its absorption of excess heat and carbon from the atmosphere, with consequent impacts on ocean resources that remain poorly understood. In an era of rapid planetary change, expanding global population and intense resource exploitation, it is vital that there are internationally coordinated ocean observing and prediction systems so policy makers can make sound evidence-based decisions about how to manage our interaction with the ocean. CLASS will underpin the UK contribution to these systems, documenting and understanding change in the marine environment, evaluating the impact of climate change and effectiveness of conservation measures and predicting the future evolution of marine environments. Over the five-year period CLASS will enhance the cost-effectiveness of observing systems by migrating them towards cutting edge autonomous technologies and developing new sensors. Finally, CLASS will create effective engagement activities ensuring academic partners have transparent access to NERC marine science capability through graduate training partnerships and access to shipborne, lab based and autonomous facilities, and modelling capabilities.


Marine LTSS: AtlantiS (Atlantic Climate and Environment Strategic Science)

Introduction

AtlantiS is a five year (2024 to 2029) programme, funded by the Natural Environment Research Council (NERC).

Scientific Rationale

The global ocean is the largest part of the Earth's climate system and acts as a major buffer to climate changes resulting from human activities. By absorbing 90% of excess heat and nearly a quarter of carbon resulting from anthropogenic greenhouse gas emissions, the ocean has already substantially mitigated climate change in the atmosphere and on land. However, this service has come at a cost to the health and resilience of the ocean and by extension the people who depend on it. Significant damage has been caused to biodiversity and productivity of marine ecosystems, to shelf seas and coastal environments, and to inland areas through extremes of weather. The futures of regional climate and ecological systems depend on the response of the ocean to multiple anthropogenic stressors. Understanding and predicting the response is fundamental for sustainable development and to guide adaptation and mitigation.

The challenge is that the ocean is so large and variable that it cannot be completely and fully observed. Achieving adequate knowledge on all scales requires international coordination of observing and modelling over decades. It requires advancement in technology to expand our ability to observe beyond individual ships. It requires expanding the range of variables measured to include biogeochemistry and ecology. The opportunity now is to lead new capability to combine observations from a widening range of platforms and sensors, next-generation ocean and coupled models, and innovation in digital tools to meet the goal above. A range of national and international reviews have identified priority knowledge gaps related to natural and anthropogenically driven changes in the global ocean and the Atlantic and its shelf seas, and their impacts on marine ecosystems and human society:

  • how natural and anthropogenic drivers of basin and decadal changes alter the Atlantic ecosystem, and the consequences for ecosystem functioning and services;
  • the importance of ocean-shelf-coast connectivity in shaping ecosystems, biodiversity, natural hazards and impacts on society;
  • the implications and feedbacks associated with climate mitigation strategies, and the need for improved assessments and advice to policy makers;
  • the sensitivity and timescales of feedbacks that determine the ability of the ocean to continue to mitigate climate change by absorbing excess heat and carbon.

The aim of the AtlantiS programme is to provide evidence, tools and knowledge to support the ambition for healthy, biologically diverse and resilient marine environments, a sustainable blue economy and communities safe from natural hazards. The objectives are to strengthen the capacity of UK marine science to observe, model and predict the ocean through a step change in capability to maximise the value inherent in marine data; to transform the ocean from being data poor to data rich; to provide global syntheses of iconic climate change indicators; to lead an increase in public and government understanding of the role of the ocean in climate; and to communicate actionable knowledge effectively. AtlantiS is the continuation and development of the CLASS programme, enhancing the long-term, large-scale ocean observation systems and the ocean value-chain that contributes to key national and international programmes and priorities.


Data Activity or Cruise Information

Data Activity

Start Date (yyyy-mm-dd) 2022-07-17
End Date (yyyy-mm-dd) 2024-07-11
Organization Undertaking ActivityNational Oceanography Centre, Southampton
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierRTWB2_07_2022
Platform Categorysubsurface mooring

Ellett Array Moored Instruments RTWB2 2022-2024

This rig was deployed as part of the Rockall Trough array of the "Overturning in the Subpolar North Atlantic Programme" (UK-OSNAP).

Deployment Cruise RRS James Cook cruise JC238
Recovery Cruise RRS Discovery cruise DY181

The rig was held down by a 700 kilogram anchor on the seabed at 1799 metres depth.

The instruments deployed on the rig were as follows:

Approximate Depth(m) Instrument Serial Number
1000 Nortek Aquadopp, SBE37 SMP MicroCAT 6276, 7290
1350 Nortek Aquadopp 6534
1575 SBE37 SMP MicroCAT 3244
1765 Nortek Aquadopp 6723
1770 SBE37 SMP MicroCAT 3231

Related Data Activity activities are detailed in Appendix 1

Cruise

Cruise Name JC238
Departure Date 2022-07-12
Arrival Date 2022-07-31
Principal Scientist(s)Ben I Moat (National Oceanography Centre, Southampton), Kristin Burmeister (Scottish Association for Marine Science)
Ship RRS James Cook

Complete Cruise Metadata Report is available here


Fixed Station Information

Fixed Station Information

Station NameUK-OSNAP/Ellett Array Mooring RTWB2 (OM56)
CategoryOffshore location
Latitude57° 28.22' N
Longitude12° 19.87' W
Water depth below MSL1800.0 m

UK-OSNAP/Ellett Array Mooring RTWB2 (OM56)

Mooring RTWB2 (called OM56 by the International OSNAP Community) forms part of the OSNAP-East Transect and, from 2018, the Ellett Array. It was first deployed on 17th July 2014 by the UK-OSNAP Community.

It is located at 57.4703°N, 12.3312°W where there is a water depth of 1800m

Between 2014 and 2018 this mooring was funded by UK-OSNAP, from 2018 it was funded as part of the Ellett Array by CLASS (Climate Linked Atlantic Sector Science).

Related Fixed Station activities are detailed in Appendix 2


BODC Quality Control Flags

The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:

Flag Description
Blank Unqualified
< Below detection limit
> In excess of quoted value
A Taxonomic flag for affinis (aff.)
B Beginning of CTD Down/Up Cast
C Taxonomic flag for confer (cf.)
D Thermometric depth
E End of CTD Down/Up Cast
G Non-taxonomic biological characteristic uncertainty
H Extrapolated value
I Taxonomic flag for single species (sp.)
K Improbable value - unknown quality control source
L Improbable value - originator's quality control
M Improbable value - BODC quality control
N Null value
O Improbable value - user quality control
P Trace/calm
Q Indeterminate
R Replacement value
S Estimated value
T Interpolated value
U Uncalibrated
W Control value
X Excessive difference

SeaDataNet Quality Control Flags

The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:

Flag Description
0 no quality control
1 good value
2 probably good value
3 probably bad value
4 bad value
5 changed value
6 value below detection
7 value in excess
8 interpolated value
9 missing value
A value phenomenon uncertain
B nominal value
Q value below limit of quantification

Appendix 1: RTWB2_07_2022

Related series for this Data Activity are presented in the table below. Further information can be found by following the appropriate links.

If you are interested in these series, please be aware we offer a multiple file download service. Should your credentials be insufficient for automatic download, the service also offers a referral to our Enquiries Officer who may be able to negotiate access.

Series IdentifierData CategoryStart date/timeStart positionCruise
2310322Currents -subsurface Eulerian2022-07-17 15:00:0057.47073 N, 12.31158 WRRS James Cook JC238
2310323Currents -subsurface Eulerian2022-07-17 15:00:0057.47073 N, 12.31158 WRRS James Cook JC238
2230576Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238
2230588Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238
2230607Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238

Appendix 2: UK-OSNAP/Ellett Array Mooring RTWB2 (OM56)

Related series for this Fixed Station are presented in the table below. Further information can be found by following the appropriate links.

If you are interested in these series, please be aware we offer a multiple file download service. Should your credentials be insufficient for automatic download, the service also offers a referral to our Enquiries Officer who may be able to negotiate access.

Series IdentifierData CategoryStart date/timeStart positionCruise
1786343Currents -subsurface Eulerian2014-07-17 16:20:0057.47033 N, 12.33117 WRV Knorr KN221-2
1786355Currents -subsurface Eulerian2014-07-17 16:20:0057.47033 N, 12.33117 WRV Knorr KN221-2
1778761Hydrography time series at depth2014-07-17 16:30:0057.47033 N, 12.33117 WRV Knorr KN221-2
1778773Hydrography time series at depth2014-07-17 16:30:0057.47033 N, 12.33117 WRV Knorr KN221-2
1787045Currents -subsurface Eulerian2015-06-22 11:35:0057.47067 N, 12.33117 WRV Pelagia PE399 (OSNAP East Leg1)
1787057Currents -subsurface Eulerian2015-06-22 11:35:0057.47067 N, 12.33117 WRV Pelagia PE399 (OSNAP East Leg1)
1787069Currents -subsurface Eulerian2015-06-22 11:35:0057.47067 N, 12.33117 WRV Pelagia PE399 (OSNAP East Leg1)
1789341Hydrography time series at depth2015-06-22 11:45:0057.47067 N, 12.33117 WRV Pelagia PE399 (OSNAP East Leg1)
1789328Hydrography time series at depth2015-06-22 11:45:0157.47067 N, 12.33117 WRV Pelagia PE399 (OSNAP East Leg1)
1795101Hydrography time series at depth2016-07-04 13:00:0057.4679 N, 12.3122 WRRS Discovery DY053
1795113Hydrography time series at depth2016-07-04 13:00:0057.4679 N, 12.3122 WRRS Discovery DY053
1795414Currents -subsurface Eulerian2016-07-04 14:00:0057.4679 N, 12.3122 WRRS Discovery DY053
1795426Currents -subsurface Eulerian2016-07-04 14:00:0057.4679 N, 12.3122 WRRS Discovery DY053
1795438Currents -subsurface Eulerian2016-07-04 14:00:0057.4679 N, 12.3122 WRRS Discovery DY053
2025836Currents -subsurface Eulerian2017-05-11 12:00:0057.47167 N, 12.31167 WRRS Discovery DY078 (DY079)
2025848Currents -subsurface Eulerian2017-05-11 12:00:0057.47167 N, 12.31167 WRRS Discovery DY078 (DY079)
2025861Currents -subsurface Eulerian2017-05-11 12:00:0057.47167 N, 12.31167 WRRS Discovery DY078 (DY079)
2025560Hydrography time series at depth2017-05-11 12:30:0157.47167 N, 12.31167 WRRS Discovery DY078 (DY079)
2025572Hydrography time series at depth2017-05-11 12:30:0157.47167 N, 12.31167 WRRS Discovery DY078 (DY079)
2042170Hydrography time series at depth2018-07-09 22:30:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2042182Hydrography time series at depth2018-07-09 22:30:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2042194Hydrography time series at depth2018-07-09 22:30:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2027972Currents -subsurface Eulerian2018-07-09 23:00:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2027984Currents -subsurface Eulerian2018-07-09 23:00:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2027996Currents -subsurface Eulerian2018-07-09 23:00:0057.46933 N, 12.3135 WRV Neil Armstrong AR30-04 (F2018-007, OSNAP East 2018)
2207266Currents -subsurface Eulerian2020-10-14 18:00:0057.4715 N, 12.31433 WRRS Discovery DY120
2207278Currents -subsurface Eulerian2020-10-14 18:00:0057.4715 N, 12.31433 WRRS Discovery DY120
2207291Currents -subsurface Eulerian2020-10-14 18:00:0057.4715 N, 12.31433 WRRS Discovery DY120
2206681Hydrography time series at depth2020-10-14 18:00:0157.4715 N, 12.31433 WRRS Discovery DY120
2206693Hydrography time series at depth2020-10-14 18:00:0157.4715 N, 12.31433 WRRS Discovery DY120
2206700Hydrography time series at depth2020-10-14 18:00:0157.4715 N, 12.31433 WRRS Discovery DY120
2310322Currents -subsurface Eulerian2022-07-17 15:00:0057.47073 N, 12.31158 WRRS James Cook JC238
2310323Currents -subsurface Eulerian2022-07-17 15:00:0057.47073 N, 12.31158 WRRS James Cook JC238
2230576Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238
2230588Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238
2230607Hydrography time series at depth2022-07-17 15:00:0157.47073 N, 12.31159 WRRS James Cook JC238