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Metadata Report for BODC Series Reference Number 1718628


Metadata Summary

Data Description

Data Category Hydrography time series at depth
Instrument Type
NameCategories
Star-Oddi DST centi-T Temperature Recorder  water temperature sensor
Instrument Mounting subsurface mooring
Originating Country United Kingdom
Originator Dr Phil Hosegood
Originating Organization University of Plymouth School of Marine Science and Engineering
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) NERC Discovery - NE/I001832/1
 

Data Identifiers

Originator's Identifier STRATSHELFSEAS_7C5690
BODC Series Reference 1718628
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2012-08-10 13:56
End Time (yyyy-mm-dd hh:mm) 2012-08-22 15:16
Nominal Cycle Interval 60.0 seconds
 

Spatial Co-ordinates

Latitude 50.34548 N ( 50° 20.7' N )
Longitude 5.60097 W ( 5° 36.1' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 40.5 m
Maximum Sensor or Sampling Depth 40.5 m
Minimum Sensor or Sampling Height 15.0 m
Maximum Sensor or Sampling Height 15.0 m
Sea Floor Depth 55.5 m
Sea Floor Depth Source SCILOG
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 Approximate - Depth is only approximate
 

Parameters

BODC CODERankUnitsTitle
AADYAA011DaysDate (time from 00:00 01/01/1760 to 00:00 UT on day)
AAFDZZ011DaysTime (time between 00:00 UT and timestamp)
ACYCAA011DimensionlessSequence number
TEMPPR011Degrees CelsiusTemperature of the water body

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

Celtic Sea temperature logger mooring August 2012: Quality Report

The data recorded by the Star-Oddi DST CTD and Star-Oddi DST centi-TD produced suspect pressure and salinity values. The pressure readings reported values that did not correspond to the deployed depths and in one of the files were showing higher pressure readings that the sea water depth at high water. The salinity values in one file were >40 in one file and more than >37 in the other. Due to these suspicious values, BODC have flagged all the values from the pressure and salinity channels from these instruments. Therefore BODC recommend that the data from these channels are used with caution.


Data Access Policy

Open Data supplied by Natural Environment Research Council (NERC)

You must always use the following attribution statement to acknowledge the source of the information: "Contains data supplied by Natural Environment Research Council."


Narrative Documents

Star-Oddi DST centi-T Temperature Recorder

Description

The Data Storage Tag (DST) centi-T is a small submersible data logger with a temperature sensor. Recorded data is stored in its internal memory with a real-time clock reference for each measurement.

The sensors are housed in a strong waterproof cylinder made of alumina (an implantable biocompatible ceramic).

Specifications

Memory 174,000 measurements in total; 261,819 bytes / temperature 1.5 bytes
Data Retention 25 years
Temperature Data Temperature resolution 0.032 °C
Temperature accuracy ± 0.1 °C
Temperature range - 1 °C to + 40 °C
Temperature response time Time constant (63%) reached in 20 sec.
Dimensions 15 mm x 46 mm
Communication Link Downloaded via PC interface box. Connects to a computer via a RS-232C standard serial interface.
Battery A 3.6 V lithium battery with a life of 7 years for a sampling interval of 10 minutes or greater.

Further details are available in the manufacturer's centi-T specification document.

Celtic Sea temperature logger mooring August 2012: Originator's processing

The temperature logger instruments were deployed on the 10 August 2012 to 22 August 2012 using the Plymouth University vessel, RV Falcon Spirit which is a 14 m catamaran.

Data Processing

No post-processing was applied to the files. They were submitted to BODC as raw ASCII format from the instrumentation.

Field Calibrations

No field calibrations were undertaken.

Celtic Sea temperature logger mooring August 2012: Processing by BODC

Data from three instruments arrived at BODC in ASCII files. This includes 2 Star-Oddi DST CTD files, 6 Star-Oddi DST centi-TD files and 9 Star-Oddi DST centi-T files with one file for each sensor used. The following table shows how the variables within the files were mapped to appropriate BODC parameter codes:

Originator's Variable Units Description BODC Parameter Code Units Comment
Temperature °C Temperature of the water body TEMPPR01 °C Applies to all files supplied.
Pressure Bars Pressure (measured variable) exerted by the water body by semi-fixed in-situ pressure sensor and corrected to read zero at sea level PREXPR01 Dbars Conversion applied to data to convert from bars to dbars (multiply by 10). Applies to only files linked to the DST centi-TD instrument
Salinity psu Practical salinity of the water body by CTD and computation using UNESCO 1983 algorithm PSALST01 dimensionless Applies to only files linked to the DST CTD instrument

The reformatted data were visualised using the in-house visualisation software. Suspect data were marked by adding an appropriate quality control flag. Missing data are set to an appropriate value and the corresponding flag added. The data files have been modified to remove data points that were gathered when the instruments were being deployed and recovered.


Project Information

NERC Discovery Science - Assessing the sensitivity of marginally stratified shelf seas within a changing climate

Background

Continental shelf seas are extremely important because of the high levels of primary productivity that they sustain and their ability to absorb and sequester atmospheric gases including climatically important greenhouse gases. The key physical aspect of shelf seas that enables them to do so is the vertical density stratification, established throughout spring and summer when the stabilizing influence of solar radiation or fresh water overcomes the destabilizing influence of turbulent mixing.

In several places around the UK, such as the Irish Sea, well-established fronts form between stratified and vertically well-mixed water due to the well-understood dominant effect of friction generated at the sea bed by strong tidal currents whose influence extends throughout the water column. Throughout the majority of UK coastal waters tidal mixing is less dominant, however, and the competition between turbulent mixing and restratification is more delicately poised. Stratification and the resulting ephemeral fronts are transient in space and intermittent in time.

We are currently hindered in our ability to predict how these marginally stratified shelf seas will respond to change, however, because we do not fully understand the details of the turbulent mixing and restratification processes that govern the dynamic balance. Amongst these, surface and internal waves both exert an important but unclear influence over mixing, whilst lateral density gradients near the surface and seabed have recently been shown to modulate mixing and restratification. This lack of understanding is apparent from our inability to accurately simulate shelf sea dynamics in numerical models that are used to predict future changes.

The importance of this project stems from the realization that future changes to the Earth system are now inevitable due to climate change and will be particularly felt within marginally stratified shelf seas for which the balance between turbulent mixing and restratification is so sensitive to external perturbations. Furthermore, in order to produce 40% of the UK's electricity from renewable sources as required by EU law, a huge expansion into the marine environment to exploit its energy resources is expected.

This project was funded by the NERC Discovery Science grant NE/I001832/1 - Assessing the sensitivity of marginally stratified shelf seas within a changing climate.

Scientific Objectives

  • To identify the processes involved in the existence and intensity of the front displays that are not governed by tidal periodicities.
  • To test whether the processes that were identified as important to changes in shelf sea stratification through in-situ measurements are indeed responsible for the observed changes.
  • To incorporate new knowledge into state-of-the-art numerical models that can up-scale the processes observed within this project to the shelf sea environment.

Fieldwork

To better understand which processes are most important within marginally stratified shelf seas, the plan is to conduct a rigorous field study and monitoring campaign in the southern Celtic Sea.

  • Conduct a series of in-situ measurements of turbulence throughout the water column and by mapping the frontal structure.
  • Monitor the long term trends in the forcing mechanisms and frontal integrity using seabed sensors and land-based radar that measures surface waves and currents over a broad spatial area.

The data were acquired from the RV Falcon Spirit, the Plymouth University vessel. The small 14m catamaran was used on a daily basis from 10 August 2012 to 22 August 2012.

Instrumentation

Types of instruments/measurements:

  • Turbulence microstructure
  • Moored temperature loggers
  • VMADCP
  • Moored ADCPs
  • Minibat towed undulator transects

Contacts

Collaborator Organisation
Dr Phil Hosegood (lead) University of Plymouth School of Marine Science and Engineering
Dr Ricardo Torres Plymouth Marine Laboratory, U.K

Data Activity or Cruise Information

Data Activity

Start Date (yyyy-mm-dd) 2012-08-10
End Date (yyyy-mm-dd) 2012-08-24
Organization Undertaking ActivityUniversity of Plymouth School of Marine Science and Engineering
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierCeltic Sea
Platform Categorysubsurface mooring

Celtic Sea temperature logger mooring August 2012

Deployment Plymouth University vessel, RV Falcon Spirit (2012-08-10 12:00)
Recovery Plymouth University vessel, RV Falcon Spirit (2012-08-24 17:20)
Deployment Position 50.3454770°N, 5.6009730°W
Water Depth (m) 55.5

The thermistor string was kept upright by a large sub-surface float.

Instruments deployed on the mooring

The DST CTD recorded temperature, conductivity and pressure.

The centi-T recorded temperature.

The centi-TD recorded temperature and pressure.

The Originator has advised that salinity and pressure recordings from the Star-Oddi instruments are not of good quality and are to be used with caution.

Instrument codes

DST CTD - Star-Oddi DST CTD

centi-T - Star-Oddi DST centi-T Temperature Recorder

centi-TD - Star-Oddi DST centi-TD Temperature and Depth Recorder

Height above bed (m) Instrument type Instrument serial number
46 centi-T 5744
44 DST CTD 6090
42 centi-T 5743
40 centi-TD 5749
38 centi-T 5742
35 centi-TD 5748
33 centi-T 5741
30 centi-TD 5747
27 centi-T 5696
23 centi-TD 6011
19 centi-T 5695
15 centi-T 5690
11 centi-TD 5605
8 centi-T 5510
5 centi-TD 5604
2 centi-T 5509
1 DST CTD 6091

Related Data Activity activities are detailed in Appendix 1

Cruise

Cruise Name 2012-08
Departure Date 2012-08-10
Arrival Date 2012-08-24
Principal Scientist(s)Phil Hosegood (University of Plymouth School of Marine Science and Engineering)
Ship RV Falcon Spirit

Complete Cruise Metadata Report is available here


Fixed Station Information


No Fixed Station Information held for the Series


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: Celtic Sea

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
1718585Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718597Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718604Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718616Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718641Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718653Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718665Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718677Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718689Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718690Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718708Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718721Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718733Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718745Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718757Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08
1718769Hydrography time series at depth2012-08-10 13:56:0050.34548 N, 5.60097 WRV Falcon Spirit 2012-08