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Metadata Report for BODC Series Reference Number 1359365


Metadata Summary

Data Description

Data Category CTD or STD cast
Instrument Type
NameCategories
Sea-Bird SBE 43 Dissolved Oxygen Sensor  dissolved gas sensors
Sea-Bird SBE 911plus CTD  CTD; water temperature sensor; salinity sensor
Paroscientific 410K Pressure Transducer  water temperature sensor; water pressure sensors
Sea-Bird SBE 3plus (SBE 3P) temperature sensor  water temperature sensor
Sea-Bird SBE 4C conductivity sensor  salinity sensor
Instrument Mounting lowered unmanned submersible
Originating Country United States
Originator Dr Molly Baringer
Originating Organization NOAA Atlantic Oceanographic and Meteorological Laboratory
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) WBTS
WBTS - Hydrography
 

Data Identifiers

Originator's Identifier AB1209009
BODC Series Reference 1359365
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2012-09-26 12:34
End Time (yyyy-mm-dd hh:mm) -
Nominal Cycle Interval 1.0 decibars
 

Spatial Co-ordinates

Latitude 26.51600 N ( 26° 31.0' N )
Longitude 76.83000 W ( 76° 49.8' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 0.99 m
Maximum Sensor or Sampling Depth 1110.67 m
Minimum Sensor or Sampling Height 17.32 m
Maximum Sensor or Sampling Height 1127.01 m
Sea Floor Depth 1128.0 m
Sea Floor Depth Source CRREP
Sensor or Sampling Distribution Variable common depth - All sensors are grouped effectively at the same depth, but this depth varies significantly during the series
Sensor or Sampling Depth Datum Approximate - Depth is only approximate
Sea Floor Depth Datum Instantaneous - Depth measured below water line or instantaneous water body surface
 

Parameters

BODC CODERankUnitsTitle
ACYCAA011DimensionlessSequence number
DEPHPR011MetresDepth (spatial coordinate) relative to water surface in the water body by profiling pressure sensor and conversion to seawater depth using UNESCO algorithm
DOXYSC011Micromoles per litreConcentration of oxygen {O2 CAS 7782-44-7} per unit volume of the water body [dissolved plus reactive particulate phase] by Sea-Bird SBE 43 sensor and calibration against sample data
OXYSZZ011PercentSaturation of oxygen {O2 CAS 7782-44-7} in the water body [dissolved plus reactive particulate phase]
POTMCV011Degrees CelsiusPotential temperature of the water body by computation using UNESCO 1983 algorithm
PRESPR011DecibarsPressure (spatial coordinate) exerted by the water body by profiling pressure sensor and correction to read zero at sea level
PSALST011DimensionlessPractical salinity of the water body by CTD and computation using UNESCO 1983 algorithm
SIGTPR011Kilograms per cubic metreSigma-theta of the water body by CTD and computation from salinity and potential temperature using UNESCO algorithm
TEMPST011Degrees CelsiusTemperature of the water body by CTD or STD
TOKGPR011Litres per kilogramConversion factor (volume to mass) for the water body by CTD and computation of density (in-situ potential temperature surface pressure) reciprocal from pressure, temperature and salinity

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

Western Boundary Time Series (WBTS) data access

The data from the Western Boundary Time Series (WBTS) project are freely available to all. The project scientists would appreciate it if the following acknowledgment was included in any publications that use this data;

"The Western Boundary Time Series data are made freely available on the Atlantic Oceanographic and Meteorological Laboratory web page (www.aoml.noaa.gov/phod/wbts/) and are funded by the NOAA Climate Observation Division."


Data Policy

Western Boundary Time Series (WBTS) data access

The data from the Western Boundary Time Series (WBTS) project are freely available to all. The project scientists would appreciate it if the following acknowledgment was included in any publications that use this data;

"The Western Boundary Time Series data are made freely available on the Atlantic Oceanographic and Meteorological Laboratory web page (www.aoml.noaa.gov/phod/wbts/) and are funded by the NOAA Climate Observation Division."


Narrative Documents

Sea-Bird Dissolved Oxygen Sensor SBE 43 and SBE 43F

The SBE 43 is a dissolved oxygen sensor designed for marine applications. It incorporates a high-performance Clark polarographic membrane with a pump that continuously plumbs water through it, preventing algal growth and the development of anoxic conditions when the sensor is taking measurements.

Two configurations are available: SBE 43 produces a voltage output and can be incorporated with any Sea-Bird CTD that accepts input from a 0-5 volt auxiliary sensor, while the SBE 43F produces a frequency output and can be integrated with an SBE 52-MP (Moored Profiler CTD) or used for OEM applications. The specifications below are common to both.

Specifications

Housing Plastic or titanium
Membrane

0.5 mil- fast response, typical for profile applications

1 mil- slower response, typical for moored applications

Depth rating

600 m (plastic) or 7000 m (titanium)

10500 m titanium housing available on request

Measurement range 120% of surface saturation
Initial accuracy 2% of saturation
Typical stability 0.5% per 1000 h

Further details can be found in the manufacturer's specification sheet.

Sea-Bird Electronics SBE 911 and SBE 917 series CTD profilers

The SBE 911 and SBE 917 series of conductivity-temperature-depth (CTD) units are used to collect hydrographic profiles, including temperature, conductivity and pressure as standard. Each profiler consists of an underwater unit and deck unit or SEARAM. Auxiliary sensors, such as fluorometers, dissolved oxygen sensors and transmissometers, and carousel water samplers are commonly added to the underwater unit.

Underwater unit

The CTD underwater unit (SBE 9 or SBE 9 plus) comprises a protective cage (usually with a carousel water sampler), including a main pressure housing containing power supplies, acquisition electronics, telemetry circuitry, and a suite of modular sensors. The original SBE 9 incorporated Sea-Bird's standard modular SBE 3 temperature sensor and SBE 4 conductivity sensor, and a Paroscientific Digiquartz pressure sensor. The conductivity cell was connected to a pump-fed plastic tubing circuit that could include auxiliary sensors. Each SBE 9 unit was custom built to individual specification. The SBE 9 was replaced in 1997 by an off-the-shelf version, termed the SBE 9 plus, that incorporated the SBE 3 plus (or SBE 3P) temperature sensor, SBE 4C conductivity sensor and a Paroscientific Digiquartz pressure sensor. Sensors could be connected to a pump-fed plastic tubing circuit or stand-alone.

Temperature, conductivity and pressure sensors

The conductivity, temperature, and pressure sensors supplied with Sea-Bird CTD systems have outputs in the form of variable frequencies, which are measured using high-speed parallel counters. The resulting count totals are converted to numeric representations of the original frequencies, which bear a direct relationship to temperature, conductivity or pressure. Sampling frequencies for these sensors are typically set at 24 Hz.

The temperature sensing element is a glass-coated thermistor bead, pressure-protected inside a stainless steel tube, while the conductivity sensing element is a cylindrical, flow-through, borosilicate glass cell with three internal platinum electrodes. Thermistor resistance or conductivity cell resistance, respectively, is the controlling element in an optimized Wien Bridge oscillator circuit, which produces a frequency output that can be converted to a temperature or conductivity reading. These sensors are available with depth ratings of 6800 m (aluminium housing) or 10500 m (titanium housing). The Paroscientific Digiquartz pressure sensor comprises a quartz crystal resonator that responds to pressure-induced stress, and temperature is measured for thermal compensation of the calculated pressure.

Additional sensors

Optional sensors for dissolved oxygen, pH, light transmission, fluorescence and others do not require the very high levels of resolution needed in the primary CTD channels, nor do these sensors generally offer variable frequency outputs. Accordingly, signals from the auxiliary sensors are acquired using a conventional voltage-input multiplexed A/D converter (optional). Some Sea-Bird CTDs use a strain gauge pressure sensor (Senso-Metrics) in which case their pressure output data is in the same form as that from the auxiliary sensors as described above.

Deck unit or SEARAM

Each underwater unit is connected to a power supply and data logging system: the SBE 11 (or SBE 11 plus) deck unit allows real-time interfacing between the deck and the underwater unit via a conductive wire, while the submersible SBE 17 (or SBE 17 plus) SEARAM plugs directly into the underwater unit and data are downloaded on recovery of the CTD. The combination of SBE 9 and SBE 17 or SBE 11 are termed SBE 917 or SBE 911, respectively, while the combinations of SBE 9 plus and SBE 17 plus or SBE 11 plus are termed SBE 917 plus or SBE 911 plus.

Specifications

Specifications for the SBE 9 plus underwater unit are listed below:

Parameter Range Initial accuracy Resolution at 24 Hz Response time
Temperature -5 to 35°C 0.001°C 0.0002°C 0.065 sec
Conductivity 0 to 7 S m-1 0.0003 S m-1 0.00004 S m-1 0.065 sec (pumped)
Pressure 0 to full scale (1400, 2000, 4200, 6800 or 10500 m) 0.015% of full scale 0.001% of full scale 0.015 sec

Further details can be found in the manufacturer's specification sheet.

Paroscientific Absolute Pressure Transducers Series 3000 and 4000

Paroscientific Series 3000 and 4000 pressure transducers use a Digiquartz pressure sensor to provide high accuracy and precision data. The sensor comprises a quartz crystal resonator that responds to pressure-induced stress, and temperature is measured for thermal compensation of the calculated pressure.

The 3000 series of transducers includes one model, the 31K-101, whereas the 4000 series includes several models, listed in the table below. All transducers exhibit repeatability of better than ±0.01% full pressure scale, hysteresis of better than ±0.02% full scale and acceleration sensitivity of ±0.008% full scale /g (three axis average). Pressure resolution is better than 0.0001% and accuracy is typically 0.01% over a broad range of temperatures.

Differences between the models lie in their pressure and operating temperature ranges, as detailed below:

Model Max. pressure (psia) Max. pressure (MPa) Temperature range (°C)
31K-101 1000 6.9 -54 to 107
42K-101 2000 13.8 0 to 125
43K-101 3000 20.7 0 to 125
46K-101 6000 41.4 0 to 125
410K-101 10000 68.9 0 to 125
415K-101 15000 103 0 to 50
420K-101 20000 138 0 to 50
430K-101 30000 207 0 to 50
440K-101 40000 276 0 to 50

Further details can be found in the manufacturer's specification sheet.

EN517 CTD Originator's Data Processing

Sampling strategy

In total, 45 CTD stations were completed on cruise EN517 to produce full depth vertical profiles of temperature, salinity and dissolved oxygen concentration. In addition, Lowered Acoustic Doppler Current Profilers (LADCPs) were attached to the CTD frame. CTDs were performed at stations along the 26.5N transect from 69.5W towards Abaco Island and a section across the Straits of Florida at 27N.

Data Acquisition and Initial Processing

A description of all the instruments on the CTD frame, including serial numbers and last calibration dates can be found on page 10 of Hooper and Baringer (2014).

The data were processed using Sea-Bird SBE data processing and AOML Matlab processing software. The temperature, conductivity and dissolved oxygen sensors were calibrated post-cruise against independent discrete samples taken from water bottles attached to the CTD frame. Of the pairs of sensors, it was determined that the primary sensors behaved more stably and are the ones included in the final data files. Further details on the processing and calibrations can be found in Hooper and Baringer (2014).

The processed data were supplied to BODC for banking.

References

Hooper, J.A., and Baringer, M.O. (2014). Hydrographic measurements collected aboard the UNOLS ship R/V Endeavour, 24 September - 10 October 2012: Western Boundary Time Series Cruise EN-517 (AB1209) NOAA Data Report, OAR-AOML-44 Atlantic Oceanographic and Meteorological Laboratory, Miami, FL. doi:10.7289/V5SF2T3R

WBTS Hydrography BODC data processing

The data arrived at BODC in ASCII files representing individual CTD casts. The data contained in the files are the downcast data averaged to a 1db pressure grid. The casts were reformatted to BODC's internal NetCDF format. The following table shows the mapping of variables within the ASCII files to appropriate BODC parameter codes

Originator's Variable Originator's Units Description BODC Parameter Code Units Comments
te deg C Temperature of the water body by CTD or STD TEMPST01 °C -
sa psu Practical salinity of the water body by CTD and computation using UNESCO 1983 algorithm PSALST01 - -
gamma ga Depth below surface of the water body by profiling pressure sensor and converted to seawater depth using UNESCO algorithm DEPHPR01 m -
p dbar Pressure (spatial co-ordinate) exerted by the water body by profiling pressure sensor and corrected to read zero at sea level PRESPR01 dbar -
ox µmol/kg Concentration of oxygen {O2} per unit volume of the water body [dissolved plus reactive particulate phase] by Sea-Bird SBE 43 sensor and calibration against sample data DOXYSC01 µmol l-1 Conversion by BODC to µmol l-1 using TOKGPR01
- - Saturation of oxygen {O2} in the water body [dissolved plus reactive particulate phase] OXYSZZ01 % Derived by BODC using DOXYSC01, TEMPST01 and PSALST01
- - Potential temperature of the water body by computation using unesco 1983 algorithm POTMCV01 °C Derived by BODC using TEMPST01, PSALST01 and PRESPR01.
- - Sigma-theta of the water body by CTD and computation from salinity and potential temperature using UNESCO algorithm SIGTPR01 kg m-3 Derived by BODC using POTMCV01, PSALST01 and PRESPR01
- - Conversion factor (volume to mass) for the water body by CTD and computation of density (in-situ potential temperature surface pressure) reciprocal from pressure, temperature and salinity TOKGPR01 l kg-1 Derived by BODC using SIGTPR01

The reformatted data were visualised using the in-house EDSERPLO software. Suspect data were marked by adding an appropriate quality control flag, and missing data marked by setting both the data to an appropriate value and setting the quality control flag.

Detailed metadata and documentation were compiled and linked to the data.


Project Information

Western Boundary Time Series (WBTS) in the Atlantic Ocean

Introduction

Users of these data are referred to the Western Boundary Time Series (WBTS) in the Atlantic Ocean website for more information. The following text has been taken from the website.

Scientific Rationale

Climate models have shown that variations of the transport of the Meridional Overturning Cell (MOC) in the Atlantic Ocean have significant impacts on the climate at both the national and global level. In the subtropical North Atlantic, the meridional overturning circulation consists primarily of two western boundary components: the northward flowing Gulf Stream and the southward flowing Deep Western Boundary Current.

The Gulf Stream is the strong surface intensified flow along the east coast of the United States that brings warm waters of tropical, including carbon, nutrients and fish, origin along the eastern seaboard of the United States. It supplies warm waters along the coast that impact a multitude of important climate phenomena including hurricane intensification, winter storm formation and moderate European weather. The Gulf Stream includes the bulk of what we call the upper limb of the thermohaline circulation in the subtropical Atlantic, in addition to a strong wind-driven flow. As the Gulf Stream flows northward, it loses heat to the atmosphere until eventually in the subpolar North Atlantic some of it becomes cold enough to sink to the bottom of the ocean. This cold deep water then returns southward along the continental slope of the eastern United States as the Deep Western Boundary Current, completing the circuit of the overturning circulation.

Off the coast of Florida, the Gulf Stream is referred to as the Florida Current and is fortuitously confined within the limited geographic channel between Florida and the Bahamas Islands, thus making a long-term observing system cost effective and sustainable. Similarly, the Deep Western Boundary Current is located within several hundred miles to the east of the Abaco Island, Grand Bahamas. The convenient geometry of the Bahamas Island chain thus allows an effective choke point for establishing a long term monitoring program of this deep limb of the overturning circulation.

Overview

The project consists of several components to monitor the Western Boundary currents in the subtropical Atlantic:


Deep Western Boundary Current (DWBC) Hydrography

Introduction

Users of these data are referred to the Deep Western Boundary Current (DWBC) Hydrography website for more information. The following text has been taken from the website.

Scientific Rationale

Climate models have shown that variations of the transport of the Meridional Overturning Cell (MOC) in the Atlantic Ocean have significant impacts on the climate at both the national and global level. In the subtropical North Atlantic, the meridional overturning circulation consists primarily of two western boundary components: the northward flowing Gulf Stream and the southward flowing Deep Western Boundary Current.

The Gulf Stream is the strong surface intensified flow along the east coast of the United States that brings warm waters of tropical, including carbon, nutrients and fish, origin along the eastern seaboard of the United States. It supplies warm waters along the coast that impact a multitude of important climate phenomena including hurricane intensification, winter storm formation and moderate European weather. The Gulf Stream includes the bulk of what we call the upper limb of the thermohaline circulation in the subtropical Atlantic, in addition to a strong wind-driven flow. As the Gulf Stream flows northward, it loses heat to the atmosphere until eventually in the subpolar North Atlantic some of it becomes cold enough to sink to the bottom of the ocean. This cold deep water then returns southward along the continental slope of the eastern United States as the Deep Western Boundary Current, completing the circuit of the overturning circulation.

Off the coast of Florida, the Gulf Stream is referred to as the Florida Current and is fortuitously confined within the limited geographic channel between Florida and the Bahamas Islands, thus making a long-term observing system cost effective and sustainable. Similarly, the Deep Western Boundary Current is located within several hundred miles to the east of the Abaco Island, Grand Bahamas. The convenient geometry of the Bahamas Island chain thus allows an effective choke point for establishing a long term monitoring program of this deep limb of the overturning circulation.

Overview

Over the past 20 years a variety of snapshot sections and time series moorings have been placed along the continental slope east of Abaco Island, Grand Bahamas, in order to monitor variability of the transport carried by the Deep Western Boundary Current. The Abaco time series began in August 1984 when the NOAA Subtropical Atlantic Climate Studies Program extended its Straits of Florida program to include measurements of western boundary current transports and water mass properties east of Abaco Island, Grand Bahamas. Since 1986, over 20 hydrographic sections have been completed east of Abaco, most including direct velocity observations, and salinity and oxygen bottle samples. Many sections have also included carbon, chlorofluorocarbon, and other tracers.

Stations frequently visited during the Deep Western Boundary Current Hydrography cruise BODC image

The repeated hydrographic and tracer sampling at Abaco has established a high-resolution record of water mass properties in the Deep Western Boundary Current at 26N. Events such as the intense convection period in the Labrador Sea and the renewal of classical Labrador Sea Water in the 1980's are clearly reflected in the cooling and freshening of the Deep Western Boundary Current waters off Abaco, and the arrival of a strong chlorofluorocarbon pulse approximately 10 years later. This data set is unique in that it is not just a single time series site but a transport section, of which very few are available in the ocean that approach a decade in length.

These continued time series observations at Abaco are seen as serving three main purposes for climate variability studies:

  • Monitoring of the DWBC for water mass and transport signatures related to changes in the strengths and regions of high latitude water mass formation in the North Atlantic for the ultimate purpose of assessing rapid climate change.
  • Serving as a western boundary endpoint of a subtropical meridional overturning circulation (MOC)/heat flux monitoring system designed to measure the interior dynamic height difference across the entire Atlantic basin and its associated baroclinic heat transport.
  • Monitoring the intensity of the Antilles Current as an index (together with the Florida Current) of interannual variability in the strength of the subtropical gyre.

Data Activity or Cruise Information

Cruise

Cruise Name EN517
Departure Date 2012-09-24
Arrival Date 2012-10-10
Principal Scientist(s)William E Johns (Rosenstiel School of Marine and Atmospheric Science)
Ship RV Endeavor

Complete Cruise Metadata Report is available here


Fixed Station Information

Fixed Station Information

Station NameWBTS Abaco section
CategoryOffshore area
Latitude26° 30.00' N
Longitude73° 12.60' W
Water depth below MSL

WBTS Abaco section

The Western Boundary Time Series (WBTS) Abaco section is one of four hydrographic sections of the WBTS Hydrography project.

The Abaco section extends from Abaco Island, Grand Bahamas eastwards into the North Atlantic. The measurements made along the Abaco section lie within a box bounded by co-ordinates 26.45°N, 76.96°W at the south west corner and 26.55°N 69.45°W at the north east corner. The section was first occupied in 1984 and continues to be occupied at least once a year.

Most sections have included measurements of temperature, salinity, oxygen and direct current velocities.

The figure below shows a typical section with stations marked with red triangles.

Map of stations

BODC image

Map showing typical locations of stations that make up the WBTS hydrographic sections. Red triangles depict the Abaco section, black circles depict Northwest Providence Channel section, magenta squares depict the North Florida Straits section and purple triangles denote South Florida Straits section.

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
Q value below limit of quantification

Appendix 1: WBTS Abaco section

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
1741963CTD or STD cast2009-04-18 15:05:0026.525 N, 76.892 WNOAA Ship Ronald H. Brown RB0901
1741975CTD or STD cast2009-04-18 17:11:0026.517 N, 76.832 WNOAA Ship Ronald H. Brown RB0901
1741987CTD or STD cast2009-04-18 20:45:0026.5 N, 76.743 WNOAA Ship Ronald H. Brown RB0901
1741999CTD or STD cast2009-04-19 01:25:0026.506 N, 76.654 WNOAA Ship Ronald H. Brown RB0901
1742002CTD or STD cast2009-04-19 06:25:0026.499 N, 76.565 WNOAA Ship Ronald H. Brown RB0901
1742014CTD or STD cast2009-04-19 12:07:0026.502 N, 76.474 WNOAA Ship Ronald H. Brown RB0901
1742026CTD or STD cast2009-04-19 17:22:0026.495 N, 76.347 WNOAA Ship Ronald H. Brown RB0901
1742038CTD or STD cast2009-04-19 22:53:0026.499 N, 76.218 WNOAA Ship Ronald H. Brown RB0901
1742051CTD or STD cast2009-04-20 04:03:0026.5 N, 76.087 WNOAA Ship Ronald H. Brown RB0901
1742063CTD or STD cast2009-04-20 09:06:0026.499 N, 75.897 WNOAA Ship Ronald H. Brown RB0901
1742075CTD or STD cast2009-04-20 14:22:0026.499 N, 75.703 WNOAA Ship Ronald H. Brown RB0901
1742087CTD or STD cast2009-04-20 19:53:0026.499 N, 75.499 WNOAA Ship Ronald H. Brown RB0901
1742099CTD or STD cast2009-04-21 01:48:0026.5 N, 75.3 WNOAA Ship Ronald H. Brown RB0901
1742106CTD or STD cast2009-04-21 06:35:0026.5 N, 75.083 WNOAA Ship Ronald H. Brown RB0901
1742118CTD or STD cast2009-04-21 11:55:0026.5 N, 74.8 WNOAA Ship Ronald H. Brown RB0901
1742131CTD or STD cast2009-04-21 17:38:0026.5 N, 74.517 WNOAA Ship Ronald H. Brown RB0901
1742143CTD or STD cast2009-04-21 23:14:0026.5 N, 74.233 WNOAA Ship Ronald H. Brown RB0901
1742155CTD or STD cast2009-04-22 05:15:0026.5 N, 73.867 WNOAA Ship Ronald H. Brown RB0901
1742167CTD or STD cast2009-04-22 10:49:0026.501 N, 73.498 WNOAA Ship Ronald H. Brown RB0901
1742179CTD or STD cast2009-04-22 17:12:0026.5 N, 73.133 WNOAA Ship Ronald H. Brown RB0901
1742180CTD or STD cast2009-04-22 23:24:0026.498 N, 72.767 WNOAA Ship Ronald H. Brown RB0901
1742192CTD or STD cast2009-04-23 05:20:0026.5 N, 72.383 WNOAA Ship Ronald H. Brown RB0901
1742211CTD or STD cast2009-04-23 11:13:0026.5 N, 72.0 WNOAA Ship Ronald H. Brown RB0901
1742223CTD or STD cast2009-04-23 18:39:0026.5 N, 71.501 WNOAA Ship Ronald H. Brown RB0901
1742235CTD or STD cast2009-04-24 01:43:0026.5 N, 71.0 WNOAA Ship Ronald H. Brown RB0901
1742247CTD or STD cast2009-04-24 08:59:0026.501 N, 70.502 WNOAA Ship Ronald H. Brown RB0901
1742259CTD or STD cast2009-04-24 15:57:0026.5 N, 70.0 WNOAA Ship Ronald H. Brown RB0901
1742260CTD or STD cast2009-04-24 22:59:0026.5 N, 69.502 WNOAA Ship Ronald H. Brown RB0901
1742296CTD or STD cast2009-04-28 06:25:0026.493 N, 76.472 WNOAA Ship Ronald H. Brown RB0901
1742303CTD or STD cast2009-04-29 00:24:0026.453 N, 76.63 WNOAA Ship Ronald H. Brown RB0901
1742315CTD or STD cast2009-04-30 05:25:0026.469 N, 76.727 WNOAA Ship Ronald H. Brown RB0901
1742327CTD or STD cast2009-04-30 21:45:0026.463 N, 76.711 WNOAA Ship Ronald H. Brown RB0901
1760101CTD or STD cast2009-11-23 12:34:0026.524 N, 76.883 WRRS Discovery D345
1760113CTD or STD cast2009-11-23 13:53:0026.514 N, 76.83 WRRS Discovery D345
1760125CTD or STD cast2009-11-23 16:23:0026.5 N, 76.744 WRRS Discovery D345
1760137CTD or STD cast2009-11-23 21:44:0026.498 N, 76.654 WRRS Discovery D345
1760149CTD or STD cast2009-11-24 14:22:0026.5 N, 76.566 WRRS Discovery D345
1760150CTD or STD cast2009-11-24 19:23:0026.499 N, 76.475 WRRS Discovery D345
1760162CTD or STD cast2009-11-25 00:27:0026.5 N, 76.347 WRRS Discovery D345
1760174CTD or STD cast2009-11-25 05:07:0026.495 N, 76.213 WRRS Discovery D345
1760186CTD or STD cast2009-11-25 12:29:0026.498 N, 76.087 WRRS Discovery D345
1760198CTD or STD cast2009-11-25 17:52:0026.495 N, 75.901 WRRS Discovery D345
1760205CTD or STD cast2009-11-25 22:55:0026.495 N, 75.708 WRRS Discovery D345
1760217CTD or STD cast2009-11-26 03:33:0026.498 N, 75.498 WRRS Discovery D345
1760229CTD or STD cast2009-11-26 08:17:0026.497 N, 75.299 WRRS Discovery D345
1760230CTD or STD cast2009-11-26 13:41:0026.505 N, 75.082 WRRS Discovery D345
1760242CTD or STD cast2009-11-26 18:34:0026.505 N, 74.801 WRRS Discovery D345
1760254CTD or STD cast2009-11-26 23:49:0026.504 N, 74.518 WRRS Discovery D345
1760266CTD or STD cast2009-11-27 04:40:0026.51 N, 74.24 WRRS Discovery D345
1760278CTD or STD cast2009-11-27 10:13:0026.501 N, 73.868 WRRS Discovery D345
1760291CTD or STD cast2009-11-27 16:09:0026.49 N, 73.51 WRRS Discovery D345
1760309CTD or STD cast2009-11-27 22:13:0026.499 N, 73.134 WRRS Discovery D345
1760310CTD or STD cast2009-11-28 04:10:0026.504 N, 72.773 WRRS Discovery D345
1760322CTD or STD cast2009-11-28 23:01:0026.498 N, 72.387 WRRS Discovery D345
1760334CTD or STD cast2009-11-29 05:05:0026.498 N, 71.991 WRRS Discovery D345
1760346CTD or STD cast2009-12-01 02:40:0026.502 N, 75.7 WRRS Discovery D345
1760358CTD or STD cast2009-12-03 13:45:0026.487 N, 76.474 WRRS Discovery D345
1760371CTD or STD cast2009-12-03 23:33:0026.515 N, 76.832 WRRS Discovery D345
1760383CTD or STD cast2009-12-04 02:33:0026.528 N, 76.766 WRRS Discovery D345
1814954CTD or STD cast2010-04-07 03:02:0026.529 N, 76.888 WRV Oceanus OC459-2
1814966CTD or STD cast2010-04-07 04:18:0026.516 N, 76.834 WRV Oceanus OC459-2
1814978CTD or STD cast2010-04-07 08:31:0026.504 N, 76.737 WRV Oceanus OC459-2
1814991CTD or STD cast2010-04-07 13:12:0026.495 N, 76.654 WRV Oceanus OC459-2
1815005CTD or STD cast2010-04-07 17:51:0026.499 N, 76.564 WRV Oceanus OC459-2
1815017CTD or STD cast2010-04-07 22:42:0026.499 N, 76.478 WRV Oceanus OC459-2
1815029CTD or STD cast2010-04-08 03:22:0026.5 N, 76.344 WRV Oceanus OC459-2
1815030CTD or STD cast2010-04-08 07:50:0026.498 N, 76.216 WRV Oceanus OC459-2
1815042CTD or STD cast2010-04-08 12:21:0026.493 N, 76.084 WRV Oceanus OC459-2
1815054CTD or STD cast2010-04-08 21:24:0026.497 N, 75.905 WRV Oceanus OC459-2
1815066CTD or STD cast2010-04-09 01:50:0026.519 N, 75.702 WRV Oceanus OC459-2
1815078CTD or STD cast2010-04-09 08:59:0026.51 N, 75.505 WRV Oceanus OC459-2
1815091CTD or STD cast2010-04-09 13:20:0026.504 N, 75.296 WRV Oceanus OC459-2
1815109CTD or STD cast2010-04-09 17:45:0026.501 N, 75.083 WRV Oceanus OC459-2
1815110CTD or STD cast2010-04-09 22:30:0026.497 N, 74.804 WRV Oceanus OC459-2
1815122CTD or STD cast2010-04-10 03:30:0026.498 N, 74.52 WRV Oceanus OC459-2
1815134CTD or STD cast2010-04-10 08:12:0026.498 N, 74.237 WRV Oceanus OC459-2
1815146CTD or STD cast2010-04-10 13:14:0026.512 N, 73.866 WRV Oceanus OC459-2
1815158CTD or STD cast2010-04-10 18:23:0026.504 N, 73.507 WRV Oceanus OC459-2
1815171CTD or STD cast2010-04-10 23:47:0026.494 N, 73.139 WRV Oceanus OC459-2
1815183CTD or STD cast2010-04-11 05:36:0026.504 N, 72.77 WRV Oceanus OC459-2
1815195CTD or STD cast2010-04-11 11:15:0026.508 N, 72.394 WRV Oceanus OC459-2
1815202CTD or STD cast2010-04-11 19:25:0026.499 N, 72.005 WRV Oceanus OC459-2
1815214CTD or STD cast2010-04-12 01:51:0026.496 N, 71.505 WRV Oceanus OC459-2
1815226CTD or STD cast2010-04-12 08:17:0026.499 N, 71.003 WRV Oceanus OC459-2
1815238CTD or STD cast2010-04-12 14:38:0026.506 N, 70.497 WRV Oceanus OC459-2
1815251CTD or STD cast2010-04-12 21:07:0026.498 N, 69.997 WRV Oceanus OC459-2
1815263CTD or STD cast2010-04-13 03:42:0026.51 N, 69.493 WRV Oceanus OC459-2
1358153CTD or STD cast2011-04-15 10:32:0026.525 N, 76.884 WRV Knorr KN200-4
1358165CTD or STD cast2011-04-15 11:42:0026.517 N, 76.833 WRV Knorr KN200-4
1358177CTD or STD cast2011-04-15 13:26:0026.501 N, 76.742 WRV Knorr KN200-4
1358189CTD or STD cast2011-04-15 17:54:0026.501 N, 76.654 WRV Knorr KN200-4
1358190CTD or STD cast2011-04-15 22:17:0026.5 N, 76.565 WRV Knorr KN200-4
1358208CTD or STD cast2011-04-16 03:21:0026.498 N, 76.477 WRV Knorr KN200-4
1358221CTD or STD cast2011-04-16 08:08:0026.497 N, 76.347 WRV Knorr KN200-4
1358233CTD or STD cast2011-04-16 12:37:0026.498 N, 76.219 WRV Knorr KN200-4
1358245CTD or STD cast2011-04-16 17:01:0026.495 N, 76.091 WRV Knorr KN200-4
1358257CTD or STD cast2011-04-16 21:32:0026.493 N, 75.904 WRV Knorr KN200-4
1358269CTD or STD cast2011-04-17 03:36:0026.503 N, 75.704 WRV Knorr KN200-4
1358270CTD or STD cast2011-04-17 07:53:0026.503 N, 75.502 WRV Knorr KN200-4
1358282CTD or STD cast2011-04-17 12:13:0026.505 N, 75.3 WRV Knorr KN200-4
1358294CTD or STD cast2011-04-17 18:11:0026.501 N, 75.077 WRV Knorr KN200-4
1358301CTD or STD cast2011-04-17 22:42:0026.501 N, 74.795 WRV Knorr KN200-4
1358313CTD or STD cast2011-04-18 03:21:0026.501 N, 74.517 WRV Knorr KN200-4
1358325CTD or STD cast2011-04-18 08:29:0026.502 N, 74.233 WRV Knorr KN200-4
1358337CTD or STD cast2011-04-18 13:36:0026.506 N, 73.86 WRV Knorr KN200-4
1358349CTD or STD cast2011-04-18 18:58:0026.504 N, 73.489 WRV Knorr KN200-4
1358350CTD or STD cast2011-04-19 00:06:0026.497 N, 73.131 WRV Knorr KN200-4
1358362CTD or STD cast2011-04-19 05:34:0026.501 N, 72.769 WRV Knorr KN200-4
1358374CTD or STD cast2011-04-19 11:05:0026.497 N, 72.388 WRV Knorr KN200-4
1358386CTD or STD cast2011-04-19 16:58:0026.51 N, 71.996 WRV Knorr KN200-4
1358398CTD or STD cast2011-04-19 23:16:0026.502 N, 71.502 WRV Knorr KN200-4
1358405CTD or STD cast2011-04-20 05:48:0026.502 N, 71.002 WRV Knorr KN200-4
1358417CTD or STD cast2011-04-20 12:44:0026.514 N, 70.498 WRV Knorr KN200-4
1358429CTD or STD cast2011-04-20 19:32:0026.538 N, 70.522 WRV Knorr KN200-4
1358430CTD or STD cast2011-04-21 02:27:0026.507 N, 70.501 WRV Knorr KN200-4
1358442CTD or STD cast2011-04-24 00:35:0026.486 N, 75.813 WRV Knorr KN200-4
1358454CTD or STD cast2011-04-25 04:01:0026.503 N, 75.713 WRV Knorr KN200-4
1358466CTD or STD cast2011-04-26 03:35:0026.501 N, 76.088 WRV Knorr KN200-4
1358478CTD or STD cast2011-04-27 01:37:0026.491 N, 76.469 WRV Knorr KN200-4
1358491CTD or STD cast2011-04-28 22:48:0026.497 N, 76.65 WRV Knorr KN200-4
1358626CTD or STD cast2012-02-18 05:09:0026.499 N, 69.666 WNOAA Ship Ronald H. Brown RB1201
1358638CTD or STD cast2012-02-18 12:10:0026.498 N, 70.085 WNOAA Ship Ronald H. Brown RB1201
1358651CTD or STD cast2012-02-18 23:43:0026.499 N, 70.498 WNOAA Ship Ronald H. Brown RB1201
1358663CTD or STD cast2012-02-19 06:03:0026.5 N, 70.998 WNOAA Ship Ronald H. Brown RB1201
1358675CTD or STD cast2012-02-19 12:28:0026.5 N, 71.501 WNOAA Ship Ronald H. Brown RB1201
1358687CTD or STD cast2012-02-19 19:45:0026.5 N, 71.999 WNOAA Ship Ronald H. Brown RB1201
1358699CTD or STD cast2012-02-20 01:39:0026.5 N, 72.381 WNOAA Ship Ronald H. Brown RB1201
1358706CTD or STD cast2012-02-20 08:03:0026.5 N, 72.766 WNOAA Ship Ronald H. Brown RB1201
1358718CTD or STD cast2012-02-20 13:51:0026.499 N, 73.132 WNOAA Ship Ronald H. Brown RB1201
1358731CTD or STD cast2012-02-20 19:36:0026.499 N, 73.501 WNOAA Ship Ronald H. Brown RB1201
1358743CTD or STD cast2012-02-21 01:47:0026.5 N, 73.863 WNOAA Ship Ronald H. Brown RB1201
1358755CTD or STD cast2012-02-21 07:11:0026.502 N, 74.233 WNOAA Ship Ronald H. Brown RB1201
1358767CTD or STD cast2012-02-21 11:58:0026.5 N, 74.516 WNOAA Ship Ronald H. Brown RB1201
1358779CTD or STD cast2012-02-21 16:44:0026.5 N, 74.801 WNOAA Ship Ronald H. Brown RB1201
1358780CTD or STD cast2012-02-21 21:55:0026.5 N, 75.083 WNOAA Ship Ronald H. Brown RB1201
1358792CTD or STD cast2012-02-22 02:07:0026.5 N, 75.29 WNOAA Ship Ronald H. Brown RB1201
1358811CTD or STD cast2012-02-22 06:41:0026.5 N, 75.503 WNOAA Ship Ronald H. Brown RB1201
1358823CTD or STD cast2012-02-22 11:36:0026.499 N, 75.704 WNOAA Ship Ronald H. Brown RB1201
1358835CTD or STD cast2012-02-22 15:53:0026.503 N, 75.901 WNOAA Ship Ronald H. Brown RB1201
1358847CTD or STD cast2012-02-22 21:20:0026.501 N, 76.087 WNOAA Ship Ronald H. Brown RB1201
1358859CTD or STD cast2012-02-23 01:29:0026.5 N, 76.203 WNOAA Ship Ronald H. Brown RB1201
1358860CTD or STD cast2012-02-23 06:06:0026.501 N, 76.347 WNOAA Ship Ronald H. Brown RB1201
1358872CTD or STD cast2012-02-23 10:41:0026.5 N, 76.479 WNOAA Ship Ronald H. Brown RB1201
1358884CTD or STD cast2012-02-23 15:38:0026.5 N, 76.565 WNOAA Ship Ronald H. Brown RB1201
1358896CTD or STD cast2012-02-23 19:45:0026.508 N, 76.654 WNOAA Ship Ronald H. Brown RB1201
1358903CTD or STD cast2012-02-23 23:36:0026.5 N, 76.742 WNOAA Ship Ronald H. Brown RB1201
1358915CTD or STD cast2012-02-24 03:35:0026.516 N, 76.831 WNOAA Ship Ronald H. Brown RB1201
1358927CTD or STD cast2012-02-24 05:45:0026.525 N, 76.892 WNOAA Ship Ronald H. Brown RB1201
1358939CTD or STD cast2012-02-24 23:36:0026.5 N, 75.704 WNOAA Ship Ronald H. Brown RB1201
1358940CTD or STD cast2012-02-26 00:06:0026.5 N, 76.088 WNOAA Ship Ronald H. Brown RB1201
1358952CTD or STD cast2012-02-28 02:32:0026.503 N, 76.538 WNOAA Ship Ronald H. Brown RB1201
1358964CTD or STD cast2012-02-29 01:23:0026.5 N, 76.743 WNOAA Ship Ronald H. Brown RB1201
1358976CTD or STD cast2012-02-29 23:51:0026.499 N, 76.743 WNOAA Ship Ronald H. Brown RB1201
1359353CTD or STD cast2012-09-26 10:57:0026.525 N, 76.884 WRV Endeavor EN517
1359377CTD or STD cast2012-09-26 14:53:0026.492 N, 76.746 WRV Endeavor EN517
1359389CTD or STD cast2012-09-26 19:24:0026.502 N, 76.662 WRV Endeavor EN517
1359390CTD or STD cast2012-09-27 00:01:0026.492 N, 76.566 WRV Endeavor EN517
1359408CTD or STD cast2012-09-27 04:54:0026.5 N, 76.48 WRV Endeavor EN517
1359421CTD or STD cast2012-09-27 09:54:0026.5 N, 76.353 WRV Endeavor EN517
1359433CTD or STD cast2012-09-27 14:41:0026.5 N, 76.222 WRV Endeavor EN517
1359445CTD or STD cast2012-09-27 19:29:0026.498 N, 76.091 WRV Endeavor EN517
1359457CTD or STD cast2012-09-28 00:44:0026.494 N, 75.905 WRV Endeavor EN517
1359469CTD or STD cast2012-09-28 05:39:0026.5 N, 75.702 WRV Endeavor EN517
1359470CTD or STD cast2012-09-28 10:21:0026.503 N, 75.5 WRV Endeavor EN517
1359482CTD or STD cast2012-09-28 15:09:0026.503 N, 75.296 WRV Endeavor EN517
1359494CTD or STD cast2012-09-28 19:58:0026.503 N, 75.072 WRV Endeavor EN517
1359501CTD or STD cast2012-09-29 00:49:0026.504 N, 74.795 WRV Endeavor EN517
1359513CTD or STD cast2012-09-29 05:42:0026.506 N, 74.51 WRV Endeavor EN517
1359525CTD or STD cast2012-09-29 10:38:0026.5 N, 74.233 WRV Endeavor EN517
1359537CTD or STD cast2012-09-29 16:15:0026.502 N, 73.86 WRV Endeavor EN517
1359549CTD or STD cast2012-09-29 21:24:0026.505 N, 73.495 WRV Endeavor EN517
1359550CTD or STD cast2012-09-30 02:46:0026.504 N, 73.128 WRV Endeavor EN517
1359562CTD or STD cast2012-09-30 08:34:0026.509 N, 72.764 WRV Endeavor EN517
1359574CTD or STD cast2012-09-30 14:26:0026.511 N, 72.382 WRV Endeavor EN517
1359586CTD or STD cast2012-09-30 20:22:0026.503 N, 71.98 WRV Endeavor EN517
1359598CTD or STD cast2012-10-01 02:32:0026.505 N, 71.501 WRV Endeavor EN517
1359605CTD or STD cast2012-10-01 09:20:0026.501 N, 71.0 WRV Endeavor EN517
1359617CTD or STD cast2012-10-01 15:52:0026.5 N, 70.494 WRV Endeavor EN517
1359629CTD or STD cast2012-10-01 22:19:0026.501 N, 69.999 WRV Endeavor EN517
1359630CTD or STD cast2012-10-05 04:01:0026.486 N, 76.109 WRV Endeavor EN517
1359642CTD or STD cast2012-10-07 03:00:0026.488 N, 76.473 WRV Endeavor EN517
1357094CTD or STD cast2014-03-16 23:17:0026.529 N, 76.882 WRV Atlantic Explorer AE1404
1357101CTD or STD cast2014-03-17 00:53:0026.521 N, 76.823 WRV Atlantic Explorer AE1404
1357113CTD or STD cast2014-03-17 03:20:0026.503 N, 76.745 WRV Atlantic Explorer AE1404
1357125CTD or STD cast2014-03-17 15:36:0026.506 N, 76.655 WRV Atlantic Explorer AE1404
1357137CTD or STD cast2014-03-17 20:25:0026.502 N, 76.55 WRV Atlantic Explorer AE1404
1357149CTD or STD cast2014-03-18 01:45:0026.5 N, 76.474 WRV Atlantic Explorer AE1404
1357150CTD or STD cast2014-03-18 07:13:0026.501 N, 76.344 WRV Atlantic Explorer AE1404
1357162CTD or STD cast2014-03-19 05:04:0026.496 N, 76.222 WRV Atlantic Explorer AE1404
1357174CTD or STD cast2014-03-19 10:26:0026.498 N, 76.084 WRV Atlantic Explorer AE1404
1357186CTD or STD cast2014-03-19 16:02:0026.504 N, 75.9 WRV Atlantic Explorer AE1404
1357198CTD or STD cast2014-03-19 21:09:0026.499 N, 75.703 WRV Atlantic Explorer AE1404
1357205CTD or STD cast2014-03-20 03:08:0026.501 N, 75.499 WRV Atlantic Explorer AE1404
1357217CTD or STD cast2014-03-20 08:39:0026.498 N, 75.302 WRV Atlantic Explorer AE1404
1357229CTD or STD cast2014-03-20 14:49:0026.507 N, 75.081 WRV Atlantic Explorer AE1404
1357230CTD or STD cast2014-03-20 19:48:0026.503 N, 74.799 WRV Atlantic Explorer AE1404
1357242CTD or STD cast2014-03-21 01:07:0026.506 N, 74.519 WRV Atlantic Explorer AE1404
1357254CTD or STD cast2014-03-21 06:22:0026.502 N, 74.229 WRV Atlantic Explorer AE1404
1357266CTD or STD cast2014-03-21 12:19:0026.502 N, 73.868 WRV Atlantic Explorer AE1404
1357278CTD or STD cast2014-03-21 18:18:0026.496 N, 73.501 WRV Atlantic Explorer AE1404
1357291CTD or STD cast2014-03-22 00:12:0026.499 N, 73.134 WRV Atlantic Explorer AE1404
1357309CTD or STD cast2014-03-22 06:23:0026.501 N, 72.77 WRV Atlantic Explorer AE1404
1357310CTD or STD cast2014-03-22 12:36:0026.502 N, 72.378 WRV Atlantic Explorer AE1404
1357322CTD or STD cast2014-03-22 22:21:0026.503 N, 71.988 WRV Atlantic Explorer AE1404
1357334CTD or STD cast2014-03-26 00:50:0026.501 N, 76.094 WRV Atlantic Explorer AE1404
1357346CTD or STD cast2014-03-27 03:53:0026.49 N, 76.467 WRV Atlantic Explorer AE1404
1357358CTD or STD cast2014-03-28 03:41:0026.502 N, 76.744 WRV Atlantic Explorer AE1404
1876731CTD or STD cast2015-10-05 16:21:0026.513 N, 76.884 WRV Endeavor EN570
1876743CTD or STD cast2015-10-05 18:10:0026.492 N, 76.833 WRV Endeavor EN570
1876755CTD or STD cast2015-10-05 20:12:0026.494 N, 76.748 WRV Endeavor EN570
1876767CTD or STD cast2015-10-06 00:20:0026.494 N, 76.657 WRV Endeavor EN570
1876779CTD or STD cast2015-10-06 04:49:0026.497 N, 76.57 WRV Endeavor EN570
1876780CTD or STD cast2015-10-06 09:36:0026.494 N, 76.467 WRV Endeavor EN570
1876792CTD or STD cast2015-10-06 14:19:0026.489 N, 76.349 WRV Endeavor EN570
1876811CTD or STD cast2015-10-06 19:40:0026.482 N, 76.219 WRV Endeavor EN570
1876823CTD or STD cast2015-10-06 23:37:0026.489 N, 76.085 WRV Endeavor EN570
1876835CTD or STD cast2015-10-07 04:15:0026.485 N, 75.898 WRV Endeavor EN570
1876847CTD or STD cast2015-10-07 08:56:0026.49 N, 75.718 WRV Endeavor EN570
1876859CTD or STD cast2015-10-07 13:47:0026.49 N, 75.512 WRV Endeavor EN570
1876860CTD or STD cast2015-10-07 19:30:0026.492 N, 75.308 WRV Endeavor EN570
1876872CTD or STD cast2015-10-07 23:54:0026.493 N, 75.087 WRV Endeavor EN570
1876884CTD or STD cast2015-10-08 04:45:0026.488 N, 74.804 WRV Endeavor EN570
1876896CTD or STD cast2015-10-08 09:41:0026.492 N, 74.518 WRV Endeavor EN570
1876903CTD or STD cast2015-10-08 14:26:0026.494 N, 74.229 WRV Endeavor EN570
1876915CTD or STD cast2015-10-08 19:31:0026.504 N, 73.868 WRV Endeavor EN570
1876927CTD or STD cast2015-10-09 00:56:0026.5 N, 73.49 WRV Endeavor EN570
1876939CTD or STD cast2015-10-09 06:15:0026.501 N, 73.134 WRV Endeavor EN570
1876940CTD or STD cast2015-10-09 11:56:0026.496 N, 72.773 WRV Endeavor EN570
1876952CTD or STD cast2015-10-09 17:40:0026.502 N, 72.383 WRV Endeavor EN570
1876964CTD or STD cast2015-10-09 23:51:0026.502 N, 71.99 WRV Endeavor EN570
1876976CTD or STD cast2015-10-10 08:20:0026.503 N, 71.496 WRV Endeavor EN570
1876988CTD or STD cast2015-10-10 14:35:0026.506 N, 70.988 WRV Endeavor EN570
1877003CTD or STD cast2015-10-10 20:56:0026.493 N, 70.479 WRV Endeavor EN570
1877015CTD or STD cast2015-10-11 03:14:0026.493 N, 69.988 WRV Endeavor EN570
1877027CTD or STD cast2015-10-11 09:48:0026.503 N, 69.494 WRV Endeavor EN570