http://lod.bco-dmo.org/id/dataset/731092
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2018-03-16
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Data collected from Miniature Autonomous Plume Recorders (MAPRs) deployed near the Axial Seamount on the Juan de Fuca Ridge on R/V Thomas G. Thompson TN327 in August 2015 and collected in July 2017.
2018-03-21
publication
2018-03-21
revision
Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)
2019-04-10
publication
https://doi.org/10.1575/1912/bco-dmo.731092.1
Edward T. Baker
National Oceanic and Atmospheric Administration
principalInvestigator
David A. Butterfield
National Oceanic and Atmospheric Administration
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Baker, E., Butterfield, D. (2018) Data collected from Miniature Autonomous Plume Recorders (MAPRs) deployed near the Axial Seamount on the Juan de Fuca Ridge on R/V Thomas G. Thompson TN327 in August 2015 and collected in July 2017. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2018-03-21 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.731092.1 [access date]
Dataset Description: <p>Data for temperature, pressure, and turbidity collected by Miniature Autonomous Plume Recorders (MAPR's) near the&nbsp;Axial Seamount on the Juan de Fuca Ridge. The MAPR's were&nbsp;equipped with a Seapoint light-backscattering sensor, a temperature sensor, and a pressure sensor. The light-backscattering sensor measures “Nephelometric Turbidity Units”, which are a dimensionless, relative measure of particle mass concentration. The data for each MAPR includes information for elevation above the seafloor and the depth below the surface.</p>
<p>Four MAPR's were deployed at different elevations above the seafloor: M34 at 55m, M12 at 80m, M13 at 105m, and M35 at 130m.&nbsp;&nbsp;</p>
<p>The mooring was deployed at 46.0934°N, 129.9814°W, at a bottom depth of 1780 m , on 27 August 2015, and recovered on 21 July 2017.&nbsp;A MAPR at 30 m above bottom (mab) failed to log. Batteries in MAPRs M12, M13, and M35 failed between early Nov and early Dec 2015. M34 recorded for the entire deployment, but data after ~February 2016 is unusable because of biofouling.<br />
<br />
See details of Mooring operations in the online cruise reports for 2015 and 2017:&nbsp;<br />
<a href="//www.pmel.noaa.gov/eoi/axial/2015/Axial2015-Cruise-Report-with-logs-revised.pdf" target="_blank">https://www.pmel.noaa.gov/eoi/axial/2015/Axial2015-Cruise-Report-with-logs-revised.pdf</a><br />
<a href="https://www.pmel.noaa.gov/eoi/axial/2017/Axial-2017-CruiseReport-final-nologs.pdf" target="_blank">https://www.pmel.noaa.gov/eoi/axial/2017/Axial-2017-CruiseReport-final-nologs.pdf</a></p>
<p>For an example of using moored MAPRs to measure temporal changes in water turbidity, see (Dziak et al., 2015).</p>
<p>Information on NOAA-PMEL MAPR:<br />
<a href="https://www.pmel.noaa.gov/eoi/PlumeStudies/mapr/" target="_blank">https://www.pmel.noaa.gov/eoi/PlumeStudies/mapr/</a></p> Methods and Sampling:
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1546695 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1546695
completed
Edward T. Baker
National Oceanic and Atmospheric Administration
206-526-6251
NOAA/PMEL 7600 Sand Point Way NE
Seattle
WA
98115
United States
Edward.Baker@noaa.gov
pointOfContact
David A. Butterfield
National Oceanic and Atmospheric Administration
206-526-6722
1045 PMEL, Bldg 3 7600 Sand Point Way NE
Seattle
WA
98115
USA
david.a.butterfield@noaa.gov
pointOfContact
asNeeded
Dataset Version: 1
Unknown
MAPR
Elevation
lat
lon
Cruise
ISO_date_time
Press_db
Temp_deg
Depth
Neph_volts
Press_counts
Temp_counts
Neph_counts
MAPR
theme
None, User defined
instrument
depth
latitude
longitude
Cruise identfier
ISO_DateTime_UTC
water pressure
water temperature at measurement depth
turbidity
featureType
BCO-DMO Standard Parameters
Miniature Autonomous Plume Recorder
instrument
BCO-DMO Standard Instruments
TN327
service
Deployment Activity
Axial Seamount, Juan de Fuca Ridge
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Ocean Observatories Initiative
http://oceanobservatories.org/
Ocean Observatories Initiative
The Ocean Observatories Initiative (OOI) is a science-driven ocean observing network that delivers real-time data to address critical science questions regarding the world's oceans. Funded by the National Science Foundation to encourage scientific investigation, OOI data are freely available online to anyone with an Internet connection. OOI was designed as a long-term project to collect ocean data for up to 30 years. This longevity makes it possible to measure and directly observe both short-lived episodic events and longer-term changes occurring in the ocean. Such data make it possible to better understand ocean processes and how the ocean is changing.
The OOI has five active research arrays that comprise the three major observatory elements linked together by instrument, infrastructure, and information management systems. Global Ocean Arrays consist of moored arrays and autonomous vehicles that provide time-series observations and mesoscale spatial sampling at sparsely sampled, high-latitude regions critical to our understanding of climate, the carbon cycle, and ocean circulation. The Regional Cabled Array consists of fiber-optic cables off the Oregon coast that provide unprecedented power, bandwidth, and communication to seafloor instrumentation and profiler moorings, enabling monitoring of volcanic and hydrothermal activity, methane seeps, earthquakes, and myriad ocean processes in coastal and blue water environments. Coastal Arrays consist of cross-shelf moored arrays and autonomous vehicles that observe the dynamic coastal environment, enabling examination of upwelling, shelf break fronts, and cross-shelf exchanges.
These marine arrays are outfitted with more than 900 instruments — of 45 different types — measuring more than 200 different parameters. These instruments gather physical, chemical, geological, and biological data – from the air-sea interface to the seafloor. The data collected are transmitted through a cyberinfrastructure, an information management system that allows users to access real- to near real-time data from suites of sensors. The OOI provides annotations and automated quality control for data streams and is working to meet the IOOS Quality Assurance of Real Time Ocean Data (QARTOD) standards.
OOI
largerWorkCitation
program
Event response to an eruption at Axial Seamount
http://axial2015.blogspot.com
Event response to an eruption at Axial Seamount
<p>On 24 April 2015, the NSF-funded Ocean Observatories Initiative's (OOI) Cabled Array detected the onset of a probable eruption at Axial Seamount, heralded by a swarm of >8000 small earthquakes and a rapid subsidence of the seafloor by >2.4 meters at the center of the caldera. Evidence that lava was erupted in or near the summit caldera includes a dramatic temperature rise recorded by instruments on the OOI Cabled Array-- up to 0.6-0.7°C above ambient sustained for weeks after the event. This eruption is likely to have significantly perturbed the hydrothermal and biological systems in and around the summit caldera, and provides the rare opportunity to address time-critical scientific questions that can only be investigated with the near-term seafloor investigations. A currently scheduled NSF and NOAA funded cruise to Axial Seamount on R/V Thompson with ROV Jason and AUV Sentry in August 2015 provides an excellent opportunity for such a response. This study adds 3 days onto this cruise to facilitate time-critical event response science.</p>
<p>Detailed seafloor mapping with shipboard multi-beam sonar and near-bottom Sentry surveys will cover areas of the caldera and adjacent rift zones that are expected eruption site(s). Fresh rock, if located, will be sampled and dated using the 210Po-210Pb technique. Hydrothermal plumes will be discerned with CTD casts and sensor tows. A mooring will be deployed with Miniature Autonomous Plume Recorders to measure temperature, light attenuation, and redox potential. The at-sea team plans to make samples and data available to the broader science community for targeted research on seafloor processes.</p>
NeMO2015
largerWorkCitation
project
eng; USA
oceans
Axial Seamount, Juan de Fuca Ridge
-129.9814
-129.9814
46.0934
46.0934
2015-08-27
2016-02-29
Axial Seamount, Juan de Fuca Ridge, northeastern Pacific Ocean (46.06°N 130.00°W)
0
BCO-DMO catalogue of parameters from Data collected from Miniature Autonomous Plume Recorders (MAPRs) deployed near the Axial Seamount on the Juan de Fuca Ridge on R/V Thomas G. Thompson TN327 in August 2015 and collected in July 2017.
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/731463.rdf
Name: MAPR
Units: no units
Description: <p>Name of MAPR</p>
http://lod.bco-dmo.org/id/dataset-parameter/731464.rdf
Name: Elevation
Units: meters
Description: <p>Depth above the seafloor</p>
http://lod.bco-dmo.org/id/dataset-parameter/731465.rdf
Name: lat
Units: decimal degrees
Description: <p>Latidude of mooring</p>
http://lod.bco-dmo.org/id/dataset-parameter/731466.rdf
Name: lon
Units: decimal degrees
Description: <p>Longitude of mooring</p>
http://lod.bco-dmo.org/id/dataset-parameter/731467.rdf
Name: Cruise
Units: no units
Description: <p>Cruise ID</p>
http://lod.bco-dmo.org/id/dataset-parameter/731468.rdf
Name: ISO_date_time
Units: no units
Description: <p>ISO Date-Time UTC YYYY-MM-DDThh:mm:ss</p>
http://lod.bco-dmo.org/id/dataset-parameter/731469.rdf
Name: Press_db
Units: decibars
Description: <p>Pressure</p>
http://lod.bco-dmo.org/id/dataset-parameter/731470.rdf
Name: Temp_deg
Units: degrees Celsius
Description: <p>Temperature</p>
http://lod.bco-dmo.org/id/dataset-parameter/731471.rdf
Name: Depth
Units: meters
Description: <p>Depth below surface</p>
http://lod.bco-dmo.org/id/dataset-parameter/731472.rdf
Name: Neph_volts
Units: volts
Description: <p>Raw voltage reading of the light-backscattering sensor; 0-5 V scale</p>
http://lod.bco-dmo.org/id/dataset-parameter/731473.rdf
Name: Press_counts
Units: counts
Description: <p>Sensor pressure reading</p>
http://lod.bco-dmo.org/id/dataset-parameter/731474.rdf
Name: Temp_counts
Units: counts
Description: <p>Sensor temperature reading</p>
http://lod.bco-dmo.org/id/dataset-parameter/731475.rdf
Name: Neph_counts
Units: counts
Description: <p>Light backscattering sensor reading</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
3439776
https://darchive.mblwhoilibrary.org/bitstream/1912/23993/1/dataset-731092_tn327-axial-2015-mapr-mooring-data__v1.tsv
download
https://doi.org/10.1575/1912/bco-dmo.731092.1
download
onLine
dataset
<p><strong>Calibration information for MAPR sensors:</strong><br />
<a href="http://datadocs.bco-dmo.org/docs/302/NeMO2015/data_docs/731092/MAPR_calibration.txt" target="_blank">MAPR_calibration.txt</a></p>
<p><strong>BCO-DMO processing notes:</strong><br />
-Changed parameter names to BCO-DMO naming conventions<br />
-Changed date-time to ISO format<br />
-Added fields for latitude and longitude</p>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
MAPR
MAPR
PI Supplied Instrument Name: MAPR PI Supplied Instrument Description:The PMEL MAPR is an inexpensive, lightweight yet rugged, simple to use self-contained instrument for recording light-backscattering (for suspended particle concentrations), oxidation-reduction potential (ORP, for detecting the presence of reduced chemical species such as H2S and Fe+2), temperature, and pressure during a wide variety of seagoing operations. MAPRs especially target operations where hydrothermal plume data are not normally collected: rock cores, dredges, or deep-towed geophysical and bottom imaging are some examples. To make these operations multi-disciplinary requires an instrument that is sensitive enough to detect hydrothermal optical anomalies yet simple enough for untrained researchers to use as an ancillary program without detracting from the time or efforts of the main sampling programs. With such an instrument, the opportunities to collect hydrothermal plume data through collaborations with other researchers, and without the need for additional dedicated technicians, expand to the global ocean.
https://www.pmel.noaa.gov/eoi/PlumeStudies/mapr/ Instrument Name: Miniature Autonomous Plume Recorder Instrument Short Name:MAPR Instrument Description: The PMEL MAPR is an inexpensive, lightweight yet rugged, simple to use self-contained instrument for recording light-backscattering (for suspended particle concentrations), oxidation-reduction potential (ORP, for detecting the presence of reduced chemical species such as H2S and Fe+2), temperature, and pressure during a wide variety of seagoing operations. MAPRs especially target operations where hydrothermal plume data are not normally collected: rock cores, dredges, or deep-towed geophysical and bottom imaging are some examples. To make these operations multi-disciplinary requires an instrument that is sensitive enough to detect hydrothermal optical anomalies yet simple enough for untrained researchers to use as an ancillary program without detracting from the time or efforts of the main sampling programs. With such an instrument, the opportunities to collect hydrothermal plume data through collaborations with other researchers, and without the need for additional dedicated technicians, expand to the global ocean.
https://www.pmel.noaa.gov/eoi/PlumeStudies/mapr/
Cruise: TN327
TN327
R/V Thomas G. Thompson
Community Standard Description
International Council for the Exploration of the Sea
R/V Thomas G. Thompson
vessel
TN327
William Chadwick
National Oceanic and Atmospheric Administration
R/V Thomas G. Thompson
Community Standard Description
International Council for the Exploration of the Sea
R/V Thomas G. Thompson
vessel