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Metadata Report for BODC Series Reference Number 1199408


Metadata Summary

Data Description

Data Category Hydrography time series at depth
Instrument Type
NameCategories
YSI 6-series multiparameter water quality sondes  sea level recorders; fluorometers; radiometers; optical backscatter sensors; water temperature sensor; nutrient analysers; salinity sensor; dissolved gas sensors; pH sensors; redox potential sensors
Instrument Mounting null
Originating Country United Kingdom
Originator Dr Matthew Blackburn
Originating Organization Scottish Environment Protection Agency, Edinburgh
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) -
 

Data Identifiers

Originator's Identifier SEPA_DUNOON_BODC_2010_GMT/100422
BODC Series Reference 1199408
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2010-04-22 07:45
End Time (yyyy-mm-dd hh:mm) 2010-05-13 09:15
Nominal Cycle Interval 900.0 seconds
 

Spatial Co-ordinates

Latitude 55.94267 N ( 55° 56.6' N )
Longitude 4.91903 W ( 4° 55.1' W )
Positional Uncertainty Unspecified
Minimum Sensor or Sampling Depth 1.0 m
Maximum Sensor or Sampling Depth 1.0 m
Minimum Sensor or Sampling Height 19.0 m
Maximum Sensor or Sampling Height 19.0 m
Sea Floor Depth 20.0 m
Sea Floor Depth Source CHART
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 Approximate - Depth is only approximate
Sea Floor Depth Datum Chart reference - Depth extracted from available chart
 

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
CPHLZZXX1Milligrams per cubic metreConcentration of chlorophyll-a {chl-a CAS 479-61-8} per unit volume of the water body [particulate >unknown phase]
DOXYZZ011Micromoles per litreConcentration of oxygen {O2 CAS 7782-44-7} per unit volume of the water body [dissolved plus reactive particulate phase] by in-situ sensor
ODSDM0211Parts per thousandSalinity of the water body
OXYSZZ011PercentSaturation of oxygen {O2 CAS 7782-44-7} in the water body [dissolved plus reactive particulate phase]
TEMPPR011Degrees CelsiusTemperature of the water body
TURBXXXX1Nephelometric Turbidity UnitsTurbidity of water in 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

Dunoon 2009-2012 Quality Report

Screening and QC

The data has had QC applied by SEPA with suspect data being removed. Data then went through BODC QC procedures; BODC's QC practice is to flag suspect data but never delete them.

The BODC QC screening of the data observed some small periods of noisy data with realistic values which were left unflagged. A few spikes have been flagged as 'M' and all data considered to be null values were flagged as 'N' automatically by the transfer and then manually crosschecked.

Ship service visits were taken at a single point in time, where stated in the originator's data.

User's should be aware in June 2011 there are periods when there are extremely high turbidity values which could affect the salinity values.

During September and October 2009 there are periods when the parameters have constant values. These have been flagged suspect as 'M'.

The morning of 06/06/2009, from 05:35 to 07:45 UTC, oxygen saturation takes a while to stabilise after deployment and although some of the data points have been flagged this should still be treated with caution.


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

YSI 6-Series multiparameter water quality sondes

Basic information

Comprehensive multi-parameter, water quality monitoring sondes. Designed for long-term monitoring, profiling and spot sampling. The 6-series may be split into several categories: V2 Sondes, 600 Sondes, Drinking Water Sondes and System. Each category has a slightly different design purpose with V2 Sondes ideal for long-term monitoring with a greater number of parameters, whereas 600 sondes are ideal for specific applications with fewer parameters available.

Model features/parameters

Features/Parameters V2 Sondes 600 Sondes Drinking Water System
  6600 6600EDS 6920 6820 600OMS 600R 600XL 600XLM 600LS 6920DW 600DW-B 600QS
Field-replaceable probes S S S S S   S S   S S  
RS-232 and SDI-12 standard S S S S S S S S S S S S
Fits 2" wells         S S S S S   S S
Internal memory S S S S S S S S S S S S
Internal power (batteries) S S S   CS     S CS S S  
Flow cell CS SO CS CS   CS CS CS   CS CS CS
Ammonium/ammonia* I   CS CS     SO SO        
Blue green algae CS CS CS CS CS   R1 R1        
Chloride* I   CS CS     SO SO        
Chlorophyll CS CS CS CS CS   R1 R1        
Conductivity S S S S S S S S CS S S S
Depth CS CS CS CS CS   CS CS       CS
Dissolved oxygen I CS R2 R2   CS CS CS       CS
Dissolved oxygen, optical CS CS CS CS CS   R1 R1        
Free chlorine                   CS CS  
Nitrate* I   CS CS     SO SO        
Open channel flow** CS CS CS CS CS   CS CS S      
ORP CS CS CS CS     CS CS   CS CS CS
PAR (Photosynthetically Active Radiation) I I                    
pH CS CS CS CS   CS CS CS   CS CS CS
Resistivity** S S S S S S S S CS S S S
Rhodamine CS CS CS CS CS   R1 R1        
Salinity S S S S S S S S CS S S S
Specific conductance** S S S S S S S S CS S S S
Temperature S S S S S S S S S S S S
Total dissolved solids** S S S S S S S S CS S S S
Turbidity CS CS CS CS CS   R1 R1   CS    
Vented level CS CS CS CS CS   CS CS S      

*Freshwater only**Calculated parameters

Where
S = Standard
CS = Customer Selectable
SO = Special Order
R1 = Available only on 600XL V2 or 600XLM V2
R2 = Available on 6920 V2-1 or 6820 V2-1
I = Available only on 6600 V2-2

 

Sensor Specifications

  Range Resolution Accuracy
Rapid Pulse dissolved oxygen
% air saturation
0 to 500% 0.1% 0 to 200%: ±2% of reading or 2% air saturation saturation, whichever is greater; 200 to 500%: ±6% of reading
Rapid Pulse dissolved oxygen
mg/L
0 to 50 mg/L 0.01 mg/L 0 to 20 mg/L: ±2% of reading or 0.2 mg/L, mg/L whichever is greater; 20 to 50 mg/L: ±6% of reading
ROX optical dissolved oxygena
% air saturation
0 to 500% 0.1% 0 to 200%: ±1% of reading or 1% air % air saturation saturation, whichever is greater; 200 to 500%: ±15% of reading; relative to calibration gases
ROX optical dissolved oxygena
mg/L
0 to 50 mg/L 0.01 mg/L 0 to 20 mg/L: ±1% of reading or 0.1 mg/L, mg/L whichever is greater; 20 to 50 mg/L: ±15% of reading; relative to calibration gases
Conductivityc 0 to 100 mS/cm 0.001 to 0.1 mS/cm ±0.5% of reading + 0.001 mS/cm (range-dependent)
Temperature -5 to 50°C 0.01°C ±0.15°C
pH 0 to 14 units 0.01 unit ±0.2 unit
Shallow depth 0 to 9.1 m (0 to 30 ft) 0.001 m (0.001 ft) ±0.018 m (±0.06 ft)
Medium depth 0 to 61 m (0 to 200 ft) 0.001 m (0.001 ft) ±0.12 m (±0.4 ft)
Deep depth 0 to 200 m (0 to 656 ft) 0.001 m (0.001 ft) ±0.3 m (±1 ft)
Vented level 0 to 9.1 m (0 to 30 ft) 0.001 m (0.001 ft) ±0.003 m (?0.01 ft)
Open-channel flow Calculated measurement, requires vented level
Free chlorine 0 to 3 mg/L 0.01 mg/L ±15% of reading or 0.05 mg/L, whichever is greater
ORP -999 to +999 mV 0.1 mV ±20 mV in Redox standard solutions
Salinity 0 to 70 ppt 0.01 ppt ±1% of reading or 0.1 ppt, whichever is greater
Nitrate/nitrogenb 0 to 200 mg/L-N 0.001 to 1 mg/L-N ±10% of reading or 2 mg/L, (range dependent) whichever is greater
Ammonium/ammoniab 0 to 200 mg/L-N 0.001 to 1 mg/L-N ±10% of reading or 2 mg/L, nitrogen (range dependent) whichever is greater
Chlorideb 0 to 1000 mg/L 0.001 to 1 mg/L ±15% of reading or 5 mg/L, (range dependent) whichever is greater
Turbiditya 0 to 1,000 NTU 0.1 NTU ±2% of reading or 0.3 NTU, whichever is greater in YSI AMCO-AEPA Polymer Standards
Rhodamine WTa 0-200 µg/L 0.1 µg/L ±5% of reading or ±1 µg/L, whichever is greater
Chlorophylla
Range Resolution Linearity
0 to 400 µg/L chl a 0.1 µg/L chl a R2 > 0.9999 for serial dilution of Rhodamine
0 to 100 RFU 0.1% FS; 0.1 RFU WT solution from 0 to 500 µg/L
Blue-green algaea,e
phycocyanin
Range Resolution Linearity
0-280,000 cells/mL 220 cells/mL R2 = 0.9999 for serial dilution of Rhodamine WT from 0 to 400 µg/L
Blue-green algaea,e
phycoerythrin
0-200,000 cells/mL 450 cells/mL R2 = 0.9999 for serial dilution of Rhodamine WT from 0 to 8 µg/L
PAR Range Calibration Stability
400-700 nm waveband ±5% < ±2% change over 1 year
Linearity Sensitivity
Max. deviation of 1% Typically 3µA per 1000 mmol s-1 m-2 in water
a Depth rating for optical probes is 61 m (200 ft); depth rating for anti-fouling optical probes with copper-alloy probe housing is 200 m (656 ft).
b Freshwater only. Maximum depth rating of 15.2 m (50 ft).
c Report outputs of specific conductance (conductivity correct to 25° C), resistivity, and total dissolved solids are also provided. These values are automatically calculated from conductivity according to algorithms found in Standard Methods for the Examination of Water and Wastewater (ed 1989).
d To maintain accuracy specification, flow must be at least 500 mL/min and pH should not change by more than ±0.3 units if mean pH is between 8.5 and 9.3.
e Specification determined using monocultures of Isochrysis sp. and fluorometric extraction of chlorophyll a. Actual detection limits will vary depending on natural algae assemblage.
f Estimated from cultures of Microcystis aeruginosa.
g Estimated from cultures of Synechococcus sp.

For further information, please see the manufacturer's manual and data sheet.

SEPA Mooring Instrumentation

The SEPA long-term monitoring project has obtained hydrographic data across various moorings through the deployment of a YSI 6600 multi-parameter-sonde attached to a fixed mooring buoy at the surface of the water column.

These mooring sites include: Dunoon, Gunnet Ledge, Inner Clyde Estuary, Campbelltown, Loch Striven, Ythan, Loch Sunart, South Alloa, and Moray Firth.

The South Alloa site had two Hydrolab MS5 probes up until the 3rd of March 2011, at which point a YSI 6600 probe was used.

The Inner Clyde Estuary site also has a probe attached approximately 1 m from the sea floor in addition to the probe at the surface.

The Moray Firth site was monitored solely between July and December 2018.

The depth of the sensors at the time of measurement at each site is available upon request for the 2016 and 2017 data.

The turbidity sensors are deemed, by the manufacturer, to be used as guidance in events such as observing storm events or spotting discharges. SEPA rely on a suspended solids laboratory procedure for their turbidity reported data. The same situation occurs for chlorophyll, SEPA have a lab method they use to report it as high turbidity can interfere with the readings. This is not generally an issue in low turbidity areas.

BODC image

BODC processing of SEPA's long-term monitoring buoys

Data Acquisition and Transfer

The data were sent by SEPA as yearly .csv files and following BODC's procedures the files were checked for consistency and subsequently archived.

The data were reformatted to QXF format using BODC's established procedures. During the transfer process each yearly file was split into cruise-to-cruise series events. The table below shows how the originator's parameters were mapped to BODC parameters and their units:

Originator's Parameter Originator's Units BODC Parameter Code BODC Units Comments
Temp deg C TEMPPR01 °C  
pH pH Units PHXXZZXX pH Units  
Salin ppt ODSDM021 ppt  
DO% % Sat OXYSZZ01 % For legacy data Oxygen saturation is not derived by BODC but taken from the data supplied.
DO mg/l DOXYZZ01 µmol/l Conversion of * 31.252 was applied during transfer (Bittig et al., 2018)
Turb NTU TURBXXXX NTU  
Chl µg/l CPHLZZXX mg/m3  
Depth m PPSBPS01 m Depth has been transferred for 2018 onwards, and is available on request for 2016 and 2017. Depth is not available for data previous to 2016.

Data Quality and Screening

Not all parameters occur in all series, particularly pH, turbidity and chlorophyll.

Oxygen saturation is not derived by BODC for consistency across all years and due to missing channels as mentioned in the originator's processing document.

The standard unit conversion factor of * 31.252 was applied to oxygen concentration during transfer to obtain the BODC units of µmol/l. (Bittig et al., 2018)

Post transfer analysis and crosschecks were applied according to BODC procedures. This involved the screening of data to check flags were appropriately applied whilst also applying further quality control flags where appropriate. Originator flags for "No sensor; Quality Control failure; Quality Control Spike Removed; Quality Control Spike removed, wiper incorrectly parking over sensor; Power Failure, Sensor failure" were all flagged as 'Null' as no data were available when these were applied.

References

Bittig, H., Körtzinger, A., Johnson, K., Claustre, H., Emerson, S., Fennel, K., ... & Xing, X. 2018. SCOR WG 142: Quality Control Procedures for Oxygen and Other Biogeochemical Sensors on Floats and Gliders. Recommendations on the conversion between oxygen quantities for Bio-Argo floats and other autonomous sensor platforms.

SEPA originator's processing document for Dunoon long-term monitoring buoy

Data Acquisition and Analysis

Data were obtained from a YSI probe attached to a mooring deployed in the Clyde Estuary just off Dunoon. The mooring was serviced and deployed by the Scottish Environment Protection Agency (SEPA) for the purpose of long-term monitoring. The raw data were downloaded directly from the instruments sometimes remotely. This initially caused problems as sometimes data strings would be overwritten if the function was set up incorrectly leading to one parameter being downloaded at the expense of another. Data were downloaded in local time and following discussion with BODC these data were then corrected to GMT before being submitted.

Quality and Screening

Once downloaded the data went through SEPA data quality checks with suspect data removed and relevant flags attached to inform future users of the reason for any missing data.

Submission

The data were then submitted to BODC through ftp as yearly .csv files.


Project Information


No Project Information held for the Series

Data Activity or Cruise Information

Cruise

Cruise Name SJM 20100422
Departure Date 2010-04-22
Arrival Date 2010-04-22
Principal Scientist(s)Matthew V Blackburn (Scottish Environment Protection Agency, Edinburgh)
Ship Sir John Murray

Complete Cruise Metadata Report is available here


Fixed Station Information

Fixed Station Information

Station NameSEPA_Dunoon
CategoryCoastal location
Latitude55° 56.56' N
Longitude4° 55.14' W
Water depth below MSL20.0 m

SEPA Dunoon Fixed Station Mooring

Location Name Dunoon
Nominal Latitude (+ve N) 55.94267
Nominal Longitude (+ve E) -4.91903
Water depth 20 m
Period of data collection Initiated in 2009

The buoy is located in the Clyde estuary, near Dunoon and provides measurements of dissolved oxygen, salinity, temperature, pH, chlorophyll and turbidity.

Maintenance takes place on a monthly basis using one of SEPA's support vessels.

Samples are mostly collected every 15 minutes, with occasional periods where a 10 or 30 minute sampling interval was collected.

The water depth where the buoy is moored was retrieved from a nautical chart. The depth should be used with caution.

More information may be found at the SEPA monitoring buoy network page for Dunoon.

Related Fixed Station activities are detailed in Appendix 1


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: SEPA_Dunoon

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
1199328Hydrography time series at depth2009-02-11 11:45:0055.94267 N, 4.91903 WSir John Murray SJM 20090211
1199341Hydrography time series at depth2009-05-11 16:15:0055.94267 N, 4.91903 WSir John Murray SJM 20090511
1199353Hydrography time series at depth2009-06-06 05:35:0055.94267 N, 4.91903 WSir John Murray SJM 20090606
1199365Hydrography time series at depth2009-09-02 12:45:0055.94267 N, 4.91903 WSir John Murray SJM 20090902
1199377Hydrography time series at depth2009-09-22 17:45:0055.94267 N, 4.91903 WSir John Murray SJM 20090922
1199389Hydrography time series at depth2009-11-16 13:15:0055.94267 N, 4.91903 WSir John Murray SJM 20091116
1199390Hydrography time series at depth2010-01-01 00:00:0055.94267 N, 4.91903 WSir John Murray SJM 20091210
1199421Hydrography time series at depth2010-05-13 09:30:0055.94267 N, 4.91903 WSir John Murray SJM 20100513
1199433Hydrography time series at depth2010-06-17 10:00:0055.94267 N, 4.91903 WSir John Murray SJM 20100617
1199445Hydrography time series at depth2010-07-18 11:30:0055.94267 N, 4.91903 WSir John Murray SJM 20100718
1199457Hydrography time series at depth2010-08-25 11:45:0055.94267 N, 4.91903 WSir John Murray SJM 20100825
1199469Hydrography time series at depth2010-09-10 10:00:0055.94267 N, 4.91903 WSir John Murray SJM 20100910
1199470Hydrography time series at depth2010-10-14 09:45:0055.94267 N, 4.91903 WSir John Murray SJM 20101014
1199482Hydrography time series at depth2010-11-01 12:30:0055.94267 N, 4.91903 WSir John Murray SJM 20101101
1199494Hydrography time series at depth2010-12-10 12:30:0055.94267 N, 4.91903 WSir John Murray SJM 20101210
1199501Hydrography time series at depth2011-01-01 00:00:0055.94267 N, 4.91903 WSir John Murray SJM 20101210
1199513Hydrography time series at depth2011-01-10 11:00:0055.94267 N, 4.91903 WSir John Murray SJM 20110110
1199525Hydrography time series at depth2011-02-08 11:15:0055.94267 N, 4.91903 WSir John Murray SJM 20110208
1199537Hydrography time series at depth2011-03-15 11:30:0055.94267 N, 4.91903 WSir John Murray SJM 20110315
1199549Hydrography time series at depth2011-04-06 10:45:0055.94267 N, 4.91903 WSir John Murray SJM 20110406
1199550Hydrography time series at depth2011-05-11 09:45:0055.94267 N, 4.91903 WSir John Murray SJM 20110511
1199562Hydrography time series at depth2011-06-09 11:00:0055.94267 N, 4.91903 WSir John Murray SJM 20110609
1199574Hydrography time series at depth2011-08-08 12:00:0055.94267 N, 4.91903 WSir John Murray SJM 20110808
1199586Hydrography time series at depth2011-09-01 11:00:0055.94267 N, 4.91903 WSir John Murray SJM 20110901
1199598Hydrography time series at depth2011-09-25 11:15:0055.94267 N, 4.91903 WSir John Murray SJM 20110925
1199605Hydrography time series at depth2011-10-23 08:15:0055.94267 N, 4.91903 WSir John Murray SJM 20111023
1199617Hydrography time series at depth2011-11-22 12:00:0055.94267 N, 4.91903 WSir John Murray SJM 20111122
1199629Hydrography time series at depth2011-12-12 14:00:0055.94267 N, 4.91903 WSir John Murray SJM 20111212
1199630Hydrography time series at depth2012-01-01 00:00:0055.94267 N, 4.91903 WSir John Murray SJM 20111212
1199642Hydrography time series at depth2012-01-10 11:00:0055.94267 N, 4.91903 WSir John Murray SJM 20120110
1199654Hydrography time series at depth2012-02-21 12:00:0055.94267 N, 4.91903 WSir John Murray SJM 20120221
1199666Hydrography time series at depth2012-03-20 12:00:0055.94267 N, 4.91903 WSir John Murray SJM 20120320
1199691Hydrography time series at depth2012-05-28 12:15:0055.94267 N, 4.91903 WSir John Murray SJM 20120528
1199709Hydrography time series at depth2012-06-25 09:00:0055.94267 N, 4.91903 WSir John Murray SJM 20120625
1199710Hydrography time series at depth2012-07-17 10:30:0055.94267 N, 4.91903 WSir John Murray SJM 20120717
1199722Hydrography time series at depth2012-08-06 11:00:0055.94267 N, 4.91903 WSir John Murray SJM 20120806
1199734Hydrography time series at depth2012-09-04 10:45:0055.94267 N, 4.91903 WSir John Murray SJM 20120904
1199746Hydrography time series at depth2012-10-29 19:30:0055.94267 N, 4.91903 WSir John Murray SJM 20121029
1199758Hydrography time series at depth2012-11-29 12:00:0055.94267 N, 4.91903 WSir John Murray SJM 20121129
1777850Hydrography time series at depth2013-01-01 00:01:0055.94267 N, 4.91903 WSir John Murray SJM 20121129
1777862Hydrography time series at depth2013-01-24 13:00:0055.94267 N, 4.91903 WSir John Murray SJM20130124
1777874Hydrography time series at depth2013-02-12 12:46:0055.94267 N, 4.91903 WSir John Murray SJM20130212
1777886Hydrography time series at depth2013-04-08 12:45:0055.94267 N, 4.91903 WSir John Murray SJM20130408
1777898Hydrography time series at depth2013-06-13 12:15:0055.94267 N, 4.91903 WSir John Murray SJM20130613
1777905Hydrography time series at depth2013-07-03 10:30:0055.94267 N, 4.91903 WSir John Murray SJM20130703
1777917Hydrography time series at depth2013-08-06 11:30:0055.94267 N, 4.91903 WSir John Murray SJM20130806
1777929Hydrography time series at depth2013-08-24 16:30:0055.94267 N, 4.91903 WSir John Murray SJM20130824
1777930Hydrography time series at depth2013-09-09 09:30:0055.94267 N, 4.91903 WSir John Murray SJM20130909
1777942Hydrography time series at depth2013-10-28 13:31:0055.94267 N, 4.91903 WSir John Murray SJM20131028
1777954Hydrography time series at depth2013-12-11 13:31:0055.94267 N, 4.91903 WSir John Murray SJM20131211
1362858Hydrography time series at depth2014-02-18 18:31:0055.94267 N, 4.91903 WSir John Murray SJM 20140218
1362871Hydrography time series at depth2014-03-05 11:01:0055.94267 N, 4.91903 WSir John Murray SJM 20140305
1362883Hydrography time series at depth2014-04-01 11:31:0055.94267 N, 4.91903 WSir John Murray SJM 20140401
1362895Hydrography time series at depth2014-05-05 14:01:0055.94267 N, 4.91903 WSir John Murray SJM 20140505
1362902Hydrography time series at depth2014-07-10 08:01:0055.94267 N, 4.91903 WSir John Murray SJM 20140710
1362914Hydrography time series at depth2014-08-19 12:01:0055.94267 N, 4.91903 WSir John Murray SJM 20140819
1362926Hydrography time series at depth2014-09-10 12:01:0055.94267 N, 4.91903 WSir John Murray SJM 20140910
1362938Hydrography time series at depth2014-10-08 10:31:0055.94267 N, 4.91903 WSir John Murray SJM 20141008
1362951Hydrography time series at depth2014-12-12 10:30:0055.94267 N, 4.91903 WSir John Murray SJM 20141212
1765074Hydrography time series at depth2015-01-01 00:01:0055.94267 N, 4.91903 WSir John Murray SJM 20141212
1765086Hydrography time series at depth2015-01-20 12:16:0055.94267 N, 4.91903 WSir John Murray SJM 20150120
1765098Hydrography time series at depth2015-02-02 11:46:0055.94267 N, 4.91903 WSir John Murray SJM 20150202
1765105Hydrography time series at depth2015-03-20 10:16:0055.94267 N, 4.91903 WSir John Murray SJM 20150320
1765117Hydrography time series at depth2015-04-14 11:46:0055.94267 N, 4.91903 WSir John Murray SJM 20150414
1765129Hydrography time series at depth2015-05-18 11:16:0055.94267 N, 4.91903 WSir John Murray SJM 20150518
1765130Hydrography time series at depth2015-06-03 09:31:0055.94267 N, 4.91903 WSir John Murray SJM 20150603
1765142Hydrography time series at depth2015-07-20 10:46:0055.94267 N, 4.91903 WSir John Murray SJM 20150720
1765154Hydrography time series at depth2015-08-11 10:01:0055.94267 N, 4.91903 WSir John Murray SJM 20150811
1765166Hydrography time series at depth2015-09-14 11:01:0055.94267 N, 4.91903 WSir John Murray SJM 20150914
1765178Hydrography time series at depth2015-10-06 10:16:0055.94267 N, 4.91903 WSir John Murray SJM 20151006
1765191Hydrography time series at depth2015-11-23 11:46:0055.94267 N, 4.91903 WSir John Murray SJM 20151123
1765209Hydrography time series at depth2015-12-14 11:31:0055.94267 N, 4.91903 WSir John Murray SJM 20151214
1806493Hydrography time series at depth2016-01-01 00:00:0055.94267 N, 4.91903 WSir John Murray SJM 20151214
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