http://lod.bco-dmo.org/id/dataset/3223
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
2010-06-16
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
One-meter averaged downcast profile data from RVIB Nathaniel B. Palmer cruises in the Ross Sea Southern Ocean (CORSACS project)
2009-09-21
publication
2009-09-21
revision
BCO-DMO Linked Data URI
2009-09-21
creation
http://lod.bco-dmo.org/id/dataset/3223
Giacomo DiTullio
College of Charleston - Hollings Marine Lab
principalInvestigator
Robert B. Dunbar
Stanford University
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: DiTullio, G., Dunbar, R. B. (2009) One-meter averaged downcast profile data from RVIB Nathaniel B. Palmer cruises in the Ross Sea Southern Ocean (CORSACS project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 21 September 2009) Version Date 2009-09-21 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/3223 [access date]
continuous downcast profile data in 1m bins Dataset Description: <p>Profile CTD data from CORSACS 1 cruise (NBP-0601) and CORSACS2 cruise (NBP-0608) to the Ross Sea in 2005 and 2006.</p>
<p>Collection of these data was funded by the NSF Office of Polar Programs as &quot;Collaborative Research: Interactive Effects of Iron, Light and Carbon Dioxide on Phytoplankton Community Dynamics in the Ross Sea&quot;, NSF Award OPP-0338097.</p> Methods and Sampling: <p>The RVIB Nathaniel B. Palmer is equipped with a SeaBird Electronics Model SBE-911plus conductivity, temperature, and depth instrument, which is mounted on a SeaBird, epoxy coated 24-bottle rosette sampler. The sampler is equipped with a SeaBird pylon and 10-liter Bullister bottles. Data from dual temperature, dual conductivity, pressure, oxygen, and other instruments were transmitted in real-time to the SBE-11 deck unit via conducting cable. Onboard, the data were recorded digitally on a Windows computer running SBE Seasave software (ver.5.37d).</p>
<p>Prior to the start of each hydrocast, the CTD was lowered to a depth of 10 m to allow time for the CTD pumps to activate and the sensors to equilibrate. During this washing period, the differences between the primary and secondary readings of the temperature and conductivity were monitored as well as dissolved O2 levels. Once stability was achieved, the CTD was brought back to the surface in preparation for the hydrocast. During all hydrocasts, the CTD was lowered at a rate of 30 m min-1 through the upper water column (usually 150 m) and then at 50 m min-1 at greater depths. The distance between the sensor package and the bottom was determined using a Datasonics pinger. A mechanical safety switch notified the CTD operator when the package had reached a distance of 3 to 5 m from the bottom. We reached the seabed on about half of the hydrocasts conducted during both NBP0601 and NBP0608. The remaining casts focused on sampling the uppermost, biologically active portion of the water column. Ten-liter Bullister bottles were tripped at selected depths on the upcast to provide in situ sampling of chemical, biological, and physical properties of the water column as well as to provide calibration data for the CTD. Once the CTD was back onboard, the temperature, conductivity, and dissolved oxygen sensors were flushed with deionized water and covered with rubber boots to minimize instrument fouling between casts.</p>
<p>Detailed descriptions of calibration and processing are available in the full cruise reports (see the cruise specific data documentation). Those reports, along with the original data contributions were downloaded from Rob Dunbar's site at Stanford University on 15 May 2009: <a href="ftp://pangea.stanford.edu/pub/dunbar/CORSACSHydrographyReports/">CTD data from Rob Dunbar</a>.</p>
Funding provided by NSF Office of Polar Programs (formerly NSF PLR) (NSF OPP) Award Number: OPP-0338097 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0338097
completed
Giacomo DiTullio
College of Charleston - Hollings Marine Lab
843-953-9196
Hollings Marine Lab 205 Fort Johnson Rd.
Charleston
SC
29412
USA
ditullioj@cofc.edu
pointOfContact
Robert B. Dunbar
Stanford University
(650) 725-6830
Department of Environmental Earth Systems Science (Braun Hall, bldg 320) Stanford University
Stanford
CA
94305-2115
USA
dunbar@stanford.edu
pointOfContact
asNeeded
Dataset Version: 21 September 2009
Unknown
cruise_id
lat
lon
sta
date
time
year_day
depth
temp_0
temp_1
cond_0
cond_1
sal_0
sal_1
sigma_t
density
density_S
fluor
PAR
PAR_surface
O2_0
O2_1
O2_0_umol_kg
O2_1_umol_kg
O2sat
O2_0_PS
O2_1_PS
O2_volts_0
O2_volts_1
CTD Seabird 911
theme
None, User defined
Cruise identfier
latitude
longitude
station number
date
time of day
year day (Day of Year, or day of year and decimal time)
depth
water temperature at measurement depth
temperature (temp2) from secondary sensor
conductivity
conductivity from the CTD secondary sensor
salinity
salinity calculated from the CTD secondary sensors
sigma-t
density
fluorescence
PAR
dissolved Oxygen
dissolved Oxygen
O2 saturation
No BCO-DMO term
featureType
BCO-DMO Standard Parameters
CTD Sea-Bird 911
instrument
BCO-DMO Standard Instruments
NBP0601
NBP0608
service
Deployment Activity
Ross Sea Southern Ocean
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 Carbon and Biogeochemistry
http://us-ocb.org/
Ocean Carbon and Biogeochemistry
The Ocean Carbon and Biogeochemistry (OCB) program focuses on the ocean's role as a component of the global Earth system, bringing together research in geochemistry, ocean physics, and ecology that inform on and advance our understanding of ocean biogeochemistry. The overall program goals are to promote, plan, and coordinate collaborative, multidisciplinary research opportunities within the U.S. research community and with international partners. Important OCB-related activities currently include: the Ocean Carbon and Climate Change (OCCC) and the North American Carbon Program (NACP); U.S. contributions to IMBER, SOLAS, CARBOOCEAN; and numerous U.S. single-investigator and medium-size research projects funded by U.S. federal agencies including NASA, NOAA, and NSF.
The scientific mission of OCB is to study the evolving role of the ocean in the global carbon cycle, in the face of environmental variability and change through studies of marine biogeochemical cycles and associated ecosystems.
The overarching OCB science themes include improved understanding and prediction of: 1) oceanic uptake and release of atmospheric CO2 and other greenhouse gases and 2) environmental sensitivities of biogeochemical cycles, marine ecosystems, and interactions between the two.
The OCB Research Priorities (updated January 2012) include: ocean acidification; terrestrial/coastal carbon fluxes and exchanges; climate sensitivities of and change in ecosystem structure and associated impacts on biogeochemical cycles; mesopelagic ecological and biogeochemical interactions; benthic-pelagic feedbacks on biogeochemical cycles; ocean carbon uptake and storage; and expanding low-oxygen conditions in the coastal and open oceans.
OCB
largerWorkCitation
program
Controls of Ross Sea Algal Community Structure
http://www.whoi.edu/sites/corsacs
Controls of Ross Sea Algal Community Structure
<h3>Project summary</h3>
<p>The Controls of Ross Sea Algal Community Structure (CORSACS) project was funded by the NSF Office of Polar Programs as "Collaborative Research: Interactive Effects of Iron, Light and Carbon Dioxide on Phytoplankton Community Dynamics in the Ross Sea". Two cruises were completed in 2006 to investigate the interactions between the primary productivity of the Ross Sea and pCO2, iron and other trace elements. Data sets of carbon, nutrient, metal, and biological measurements will be reported.</p>
<p>The main objective in the proposed research was to investigate the relative importance and potential interactive effects of iron, light and CO2 levels in structuring algal assemblages and growth rates in the Ross Sea. The investigators hypothesized that the interaction of these three variables largely determines the bottom-up control on these two dominant Southern Ocean phytoplankton taxa. While grazing and other loss processes are important variables in determining the relative dominance of these two taxa, the CORSACS research project was designed to focus on the bottom-up control mechanisms. It is important to understand such environmentally-driven taxonomic shifts in primary production, since they are expected to impact the fixation and export of carbon and nutrients, and the production of DMS, thus potentially providing both positive and negative feedbacks on climate.</p>
<p>The CORSACS investigators considered a range of ambient iron, light and pCO2 levels that span those typically observed in the Ross Sea during the growing season. That is, dissolved iron ranging from ~0.1 nM (low iron) to greater than 1 nM (high iron) (Fitzwater et al. 2000; Sedwick et al. 2000); mean irradiance (resulting from vertical mixing/self shading) ranging from less than 10% Io (low light) to greater than 40% (high light) (Arrigo et al., 1998, 1999), possibly adjusted based on field observations during the CORSACS cruises; and pCO2 ranging (Sweeney et al. 2001) from ~150 ppm (low CO2) to the probable higher levels of pCO2 - 750 ppm as a conservative estimate - that are likely to be attained later this century due to anthropogenic perturbation of the global carbon cycle (IPCC, 2001).</p>
<p>From the information previously available from both field observations and experiments, the investigators formulated the following specific hypotheses regarding the interactive role of iron, light and CO2 in regulating algal composition in the Ross Sea: diatoms bloom in the southern Ross Sea only under optimum conditions of high iron, light and pCO2; colonial Phaeocystis dominate under conditions of high iron with either (or both) low light or low pCO2; and solitary Phaeocystis are predominant under conditions of low iron with either (or both) low light or low pCO2.</p>
<h4>References:</h4>
<p>Fitzwater, S.E., K.S. Johnson, R.M. Gordon, K.H. Coale, and W.O. Smith, Jr. (2000). Trace metal concentrations in the Ross Sea and their relationship with nutrients and growth. Deep-Sea Research II, 47: 3159-3179.</p>
<p>Martin JH, Gordon RM, Fitzwater SE. Iron in Antarctic waters. Nature 1990 ;345(6271):156-158. Martin JH. 1990. Glacial-interglacial CO2 change: The iron hypothesis. Paleoceanography 5(1):1-13</p>
<p>P. N. Sedwick, G. R. DiTullio, and D. J. Mackey, Iron and manganese in the Ross Sea, Antarctica: Seasonal iron limitation in Antarctic shelf waters, Journal of Geophysical Research, 105 (C5), 11,321-11,336, 2000.</p>
<p>Sweeney, C. K. Arrigo, and G. van Gijken (2001). Prediction of seasonal changes in surface pCO2 in the Ross Sea, Antarctica using ocean color satellite data. 2001 Annual AGU meeting, San Fransisco, CA Dec. 10-15.</p>
<p>IPCC, 2001: Climate Change 2001: Synthesis Report. A Contribution of Working Groups I, II, and III to the Third Assessment Report of theIntegovernmental Panel on Climate Change [Watson, R.T. and the Core Writing Team (eds.)]. Cambridge University Press, Cambridge,United Kingdom, and New York, NY, USA, 398 pp.</p>
<p><strong>Publications</strong></p>
<p>Saito, M. A., Goepfert, T. J., Noble, A. E., Bertrand, E. M., Sedwick, P. N., and DiTullio, G. R.: A seasonal study of dissolved cobalt in the Ross Sea, Antarctica: micronutrient behavior, absence of scavenging, and relationships with Zn, Cd, and P, Biogeosciences, 7, 4059-4082, doi:10.5194/bg-7-4059-2010, 2010 (<a href="http://www.biogeosciences.net/7/4059/2010/bg-7-4059-2010.html">http://www.biogeosciences.net/7/4059/2010/bg-7-4059-2010.html</a>)</p>
<p>Bertrand EM, Saito MA, Lee PA, Dunbar RB, Sedwick PN and DiTullio GR (2011) Iron limitation of a springtime bacterial and phytoplankton community in the Ross Sea: implications for vitamin B12 nutrition. Front. Microbio. 2:160. doi: 10.3389/fmicb.2011.00160 (<a href="http://www.frontiersin.org/Aquatic_Microbiology/10.3389/fmicb.2011.00160/abstract">http://www.frontiersin.org/Aquatic_Microbiology/10.3389/fmicb.2011.00160/abstract</a>)</p>
CORSACS
largerWorkCitation
project
eng; USA
oceans
Ross Sea Southern Ocean
2009-09-21
Ross Sea Southern Ocean
0
BCO-DMO catalogue of parameters from One-meter averaged downcast profile data from RVIB Nathaniel B. Palmer cruises in the Ross Sea Southern Ocean (CORSACS 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
http://lod.bco-dmo.org/id/dataset-parameter/19122.rdf
Name: cruise_id
Units: dimensionless
Description: <p>ship's cruise designation</p>
http://lod.bco-dmo.org/id/dataset-parameter/19123.rdf
Name: lat
Units: decimal degrees
Description: <p>latitude; North is positive, South is negative</p>
http://lod.bco-dmo.org/id/dataset-parameter/19124.rdf
Name: lon
Units: decimal degrees
Description: <p>longitude; East is positive, West is negative</p>
http://lod.bco-dmo.org/id/dataset-parameter/19125.rdf
Name: sta
Units: dimensionless
Description: <p>station number</p>
http://lod.bco-dmo.org/id/dataset-parameter/19126.rdf
Name: date
Units: YYYYMMDD
Description: <p>date of sampling; local or UTC unknown</p>
http://lod.bco-dmo.org/id/dataset-parameter/19127.rdf
Name: time
Units: hhmm
Description: <p>time of sampling; local or UTC unknown</p>
http://lod.bco-dmo.org/id/dataset-parameter/19128.rdf
Name: year_day
Units: dimensionless
Description: <p>day of year for a specified year as a decimal; note that noon on Jan 1 is 1.5; range 1 to 366</p>
http://lod.bco-dmo.org/id/dataset-parameter/19129.rdf
Name: depth
Units: meters
Description: <p>sample depth, in meters</p>
http://lod.bco-dmo.org/id/dataset-parameter/19130.rdf
Name: temp_0
Units: degrees Celsius
Description: <p>temperature, from the CTD 'primary sensor', in degrees Celsius.</p>
http://lod.bco-dmo.org/id/dataset-parameter/19131.rdf
Name: temp_1
Units: degrees Celsius
Description: <p>temperature, from the CTD 'secondary sensor', in degrees Celsius.</p>
http://lod.bco-dmo.org/id/dataset-parameter/19132.rdf
Name: cond_0
Units: Siemens per meter
Description: <p>conductivity, from the CTD 'primary sensor', in Siemens/meter.</p>
http://lod.bco-dmo.org/id/dataset-parameter/19133.rdf
Name: cond_1
Units: Siemens per meter
Description: <p>conductivity, from the CTD 'secondary sensor', in Siemens/meter.</p>
http://lod.bco-dmo.org/id/dataset-parameter/19134.rdf
Name: sal_0
Units: dimensionless
Description: <p>salinity, calculated from the CTD 'primary sensor' in Practical Salinity Units (PSU)</p>
http://lod.bco-dmo.org/id/dataset-parameter/19135.rdf
Name: sal_1
Units: dimensionless
Description: <p>salinity, calculated from the CTD 'secondary sensor' in Practical Salinity Units (PSU)</p>
http://lod.bco-dmo.org/id/dataset-parameter/19136.rdf
Name: sigma_t
Units: kilograms per meter cubed - 1000
Description: <p>sigma-t density</p>
http://lod.bco-dmo.org/id/dataset-parameter/19137.rdf
Name: density
Units: kilograms per meter cubed
Description: <p>density, from the CTD 'primary sensor'</p>
http://lod.bco-dmo.org/id/dataset-parameter/19138.rdf
Name: density_S
Units: kilograms per meter cubed
Description: <p>density, from the CTD 'secondary sensor'</p>
http://lod.bco-dmo.org/id/dataset-parameter/19139.rdf
Name: fluor
Units: volts
Description: <p>fluorescence, FIECO-AFL</p>
http://lod.bco-dmo.org/id/dataset-parameter/19140.rdf
Name: PAR
Units: microeinsteins per meter^2 per second
Description: <p>Photosynthetically Available Radiation (PAR)</p>
http://lod.bco-dmo.org/id/dataset-parameter/19141.rdf
Name: PAR_surface
Units: microeinsteins per meter^2 per second
Description: <p>surface PAR</p>
http://lod.bco-dmo.org/id/dataset-parameter/19142.rdf
Name: O2_0
Units: milliliters per liter
Description: <p>oxygen; CTD sensor 0 (primary)</p>
http://lod.bco-dmo.org/id/dataset-parameter/19143.rdf
Name: O2_1
Units: milliliters per liter
Description: <p>oxygen; CTD sensor 1 (secondary)</p>
http://lod.bco-dmo.org/id/dataset-parameter/19144.rdf
Name: O2_0_umol_kg
Units: micromoles per kilogram
Description: <p>dissolved oxygen; CTD sensor 0 (primary) in micromoles per kilogram</p>
http://lod.bco-dmo.org/id/dataset-parameter/19145.rdf
Name: O2_1_umol_kg
Units: micromoles per kilogram
Description: <p>dissolved oxygen; CTD sensor 1 (secondary) in micromoles per kilogram</p>
http://lod.bco-dmo.org/id/dataset-parameter/19146.rdf
Name: O2sat
Units: milliliters per liter
Description: <p>oxygen saturation</p>
http://lod.bco-dmo.org/id/dataset-parameter/19147.rdf
Name: O2_0_PS
Units: unknown
Description: <p>unknown; primary sensor; percent saturation?</p>
http://lod.bco-dmo.org/id/dataset-parameter/19148.rdf
Name: O2_1_PS
Units: unknown
Description: <p>unknown; secondary sensor; percent saturation?</p>
http://lod.bco-dmo.org/id/dataset-parameter/19149.rdf
Name: O2_volts_0
Units: volts
Description: <p>oxygen in volts; primary sensor</p>
http://lod.bco-dmo.org/id/dataset-parameter/19150.rdf
Name: O2_volts_1
Units: volts
Description: <p>oxygen in volts; secondary sensor</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
8104558
https://datadocs.bco-dmo.org/file/93Nlx0kfMO6Y45/CTD_NBP0601.csv
CTD_NBP0601.csv
Version September 2009
PI: Giacomo DiTullio
Co-PI: Robert B. Dunbar
Final Post Processed Qced Downcast CTD 1m bins
Controls on Ross Sea Algal Community Structure (CORSACS)
NBP06-01; R/V Nathaniel B. Palmer; December 2005 to January 2006
download
7046585
https://datadocs.bco-dmo.org/file/KAy0W3JiqLwl0R/CTD_NBP0608.csv
CTD_NBP0608.csv
Version September 2009
PI: Giacomo DiTullio
Co-PI: Robert B. Dunbar
Final Post Processed Qced Downcast CTD 1m bins
Controls on Ross Sea Algal Community Structure (CORSACS)
NBP06-08; R/V Nathaniel B. Palmer; November-December, 2006
download
https://osprey.bco-dmo.org/dataset/3223/data/download
download
onLine
dataset
<p>The RVIB Nathaniel B. Palmer is equipped with a SeaBird Electronics Model SBE-911plus conductivity, temperature, and depth instrument, which is mounted on a SeaBird, epoxy coated 24-bottle rosette sampler. The sampler is equipped with a SeaBird pylon and 10-liter Bullister bottles. Data from dual temperature, dual conductivity, pressure, oxygen, and other instruments were transmitted in real-time to the SBE-11 deck unit via conducting cable. Onboard, the data were recorded digitally on a Windows computer running SBE Seasave software (ver.5.37d).</p>
<p>Prior to the start of each hydrocast, the CTD was lowered to a depth of 10 m to allow time for the CTD pumps to activate and the sensors to equilibrate. During this washing period, the differences between the primary and secondary readings of the temperature and conductivity were monitored as well as dissolved O2 levels. Once stability was achieved, the CTD was brought back to the surface in preparation for the hydrocast. During all hydrocasts, the CTD was lowered at a rate of 30 m min-1 through the upper water column (usually 150 m) and then at 50 m min-1 at greater depths. The distance between the sensor package and the bottom was determined using a Datasonics pinger. A mechanical safety switch notified the CTD operator when the package had reached a distance of 3 to 5 m from the bottom. We reached the seabed on about half of the hydrocasts conducted during both NBP0601 and NBP0608. The remaining casts focused on sampling the uppermost, biologically active portion of the water column. Ten-liter Bullister bottles were tripped at selected depths on the upcast to provide in situ sampling of chemical, biological, and physical properties of the water column as well as to provide calibration data for the CTD. Once the CTD was back onboard, the temperature, conductivity, and dissolved oxygen sensors were flushed with deionized water and covered with rubber boots to minimize instrument fouling between casts.</p>
<p>Detailed descriptions of calibration and processing are available in the full cruise reports (see the cruise specific data documentation). Those reports, along with the original data contributions were downloaded from Rob Dunbar's site at Stanford University on 15 May 2009: <a href="ftp://pangea.stanford.edu/pub/dunbar/CORSACSHydrographyReports/">CTD data from Rob Dunbar</a>.</p>
from Cruise: NBP0601 <h3>CORSACS I</h3>
<p>The RVIB Nathaniel B. Palmer departed Lyttleton, New Zealand at December 18,
2005 and arrived at station #000 on December 24, 2005 at 00:07 UTC.</p>
<p>
The cruise track proceeded into the Ross Sea polynya where a total
of 102 hydrographic stations were occupied through late January, 2006.
</p><p>
Sampling and analytical methods are described in full in the
CORSACS-I Cruise Hydrographic Report
</p><p>
<a href="http://data.bco-dmo.org/CORSACS/cruises/Dunbar_Hydrography_report_NBP0601.pdf">CORSACS I Hydrography Report</a>
</p>
from Cruise: NBP0608 <p>
<h3>CORSACS II</h3>
The RVIB Nathaniel B. Palmer departed Lyttleton, New Zealand at November 1,
2006 and arrived at station #001 on November 8, 2006 at 00:51 UTC.
</p><p>
The cruise track proceeded into the Ross Sea polynya where a total of 74
hydrographic stations were occupied through December 6, 2006.
</p><p>
Sampling and analytical methods are described in full in the CORSACS-II Cruise Hydrography Report
</p><p>
<a href="http://data.bco-dmo.org/CORSACS/cruises/Dunbar_Hydrography_report_NBP0608.pdf">CORSACS II Hydrography Report</a>
</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
CTD Seabird 911
CTD Seabird 911
PI Supplied Instrument Name: CTD Seabird 911 Instrument Name: CTD Sea-Bird 911 Instrument Short Name:CTD SBE 911 Instrument Description: The Sea-Bird SBE 911 is a type of CTD instrument package. The SBE 911 includes the SBE 9 Underwater Unit and the SBE 11 Deck Unit (for real-time readout using conductive wire) for deployment from a vessel. The combination of the SBE 9 and SBE 11 is called a SBE 911. The SBE 9 uses Sea-Bird's standard modular temperature and conductivity sensors (SBE 3 and SBE 4). The SBE 9 CTD can be configured with auxiliary sensors to measure other parameters including dissolved oxygen, pH, turbidity, fluorescence, light (PAR), light transmission, etc.). More information from Sea-Bird Electronics. Community Standard Description: http://vocab.nerc.ac.uk/collection/L22/current/TOOL0035/
Cruise: NBP0601
NBP0601
Community Standard Description
International Council for the Exploration of the Sea
RVIB Nathaniel B. Palmer
vessel
NBP0601
Giacomo DiTullio
College of Charleston - Hollings Marine Lab
http://data.bco-dmo.org/CORSACS/cruises/Dunbar_Hydrography_report_NBP0601.pdf
Report describing NBP0601
Cruise: NBP0608
NBP0608
Community Standard Description
International Council for the Exploration of the Sea
RVIB Nathaniel B. Palmer
vessel
NBP0608
Giacomo DiTullio
College of Charleston - Hollings Marine Lab
http://data.bco-dmo.org/CORSACS/cruises/Dunbar_Hydrography_report_NBP0608.pdf
Report describing NBP0608
Community Standard Description
International Council for the Exploration of the Sea
RVIB Nathaniel B. Palmer
vessel