http://lod.bco-dmo.org/id/dataset/2955
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)
Barium VUB - Dissolved Ba; particulate Ba, Sr, Ca, Al from Niskins from VERTIGO cruises KM0414, ZHNG09RR from the Hawaiian Islands HOT Site, NW SubArctic Pacific Ocean K2 Site, 2004-2005 (VERTIGO project)
2008-11-12
publication
2008-11-12
revision
BCO-DMO Linked Data URI
2008-11-12
creation
http://lod.bco-dmo.org/id/dataset/2955
Frank Dehairs
Vrije Universiteit Brussel
principalInvestigator
Stéphanie Jacquet
Vrije Universiteit Brussel
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: Dehairs, F., Jacquet, S. (2008) Barium VUB - Dissolved Ba; particulate Ba, Sr, Ca, Al from Niskins from VERTIGO cruises KM0414, ZHNG09RR from the Hawaiian Islands HOT Site, NW SubArctic Pacific Ocean K2 Site, 2004-2005 (VERTIGO project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 12 November 2008) Version Date 2008-11-12 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/2955 [access date]
Barium VUB - Dissolved Ba; particulate Ba, Sr, Ca, Al from Niskins Methods and Sampling: <pre>
Methodology: <a
href="http://ocb.whoi.edu/VERTIGO/PI-NOTES/multi-ship_bariumVUB_niskin.html">Methodology</a>
Change history: YYMMDD
080710: contributed by Frank Dehairs
081112: Cruise_ID added manually
date, event, ev_code, lon, lat from cruise logs merged with original data
one single multi-ship dataset generated for both KM0414 and RR_K2 data
081112: added to OCB database; Steve Gegg (sgegg@whoi.edu), OCB DMO
DMO Note 1: Comments in cells from original spreadsheets preserved below
KM0414/ALOHA:
date cast bot parameter value Comment
20040704 81 15 Ba_part 6 Frank: suspect data
20040706 80 11 Ba_part 260 Frank: ICP-OES result
20040706 80 11 Sr_part 178 Frank: ICP-OES result
RR_K2/K2:
(none)
DMO Note 2: Used common "cast" id from these data to determine sample
position, date and event code for Niskin data
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/KM0414/log.html0">KM0414 event log</a>
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/RR_K2/log.html0">RR_K2 event log</a>
</pre>
completed
Frank Dehairs
Vrije Universiteit Brussel
32-(0)2-629.32.60
Vrije Universiteit Brussel, Analytical and Environmental Chemistry Pleinlaan 2
Brussels
B-1050
Belgium
fdehairs@vub.ac.be
pointOfContact
Stéphanie Jacquet
Vrije Universiteit Brussel
+33 4 42 97 15 98
CEREGE SE3D, UMR 6635 Europole Mediterraneen de l'Arbois, BP 80,
Aix en Provence, Cedex 04
13545
France
jacquet@cerege.fr
pointOfContact
asNeeded
Dataset Version: 12 November 2008
Unknown
Cruise_ID
date
event
ev_code
lon
lat
date_local
cast
bot
press
Ba_diss
Ba_part
Sr_part
Ca_part
Al_part
theme
None, User defined
cruise id
date
event
No BCO-DMO term
longitude
latitude
date_local
cast
bottle number
water pressure
featureType
BCO-DMO Standard Parameters
KM0414
ZHNG09RR
service
Deployment Activity
Hawaiian Islands, HOT Site
NW, SubArctic Pacific Ocean - K2 Site
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
VERtical Transport In the Global Ocean
https://cafethorium.whoi.edu/projects/vertigo/
VERtical Transport In the Global Ocean
<p><em>NSF Award Abstract:</em><br />
In this study, researchers at the Woods Hole Oceanographic Institution, Virginia Institute of Marine Science, University of California - Santa Cruz, University of California - Santa Barbara, University of Tasmania, and NIWA-Australia will work collaboratively to answer a difficult question in marine biogeochemistry: What controls the efficiency of particle transport between the surface and deep ocean? More specifically, what is the fate of sinking particles leaving the upper ocean and what factors influence remineralization length scales for different sinking particle classes? Knowing the efficiency of particle transport is important for an accurate assessment of the ocean carbon sink. Globally, the magnitude and efficiency of the biological pump will in part modulate levels of atmospheric carbon dioxide.</p>
<p>The research team intends to test two basic hypotheses about remineralization control, namely: (1) particle source characteristics are the dominant control on the efficiency of particle transport; and/or that (2) mid-water processing, either by zooplankton or bacteria, controls transport efficiency. To do so, they will conduct process studies at sea focused on particle flux and composition changes in the upper 500-1000m of the ocean. The basic approach is to examine changes in particle composition and flux with depth within a given source region using a combination of approaches, many of which are new to the field. These include neutrally buoyant sediment traps, particle pumps, settling columns and respiration chambers, along with the development of new biological and geochemical tools for an integrated biogeochemical assessment of the biological pump. Two sites will be studied extensively on three-week process study cruises: the Hawaii Ocean Time-series site (HOT) and a new moored time-series site in the subarctic NW Pacific (Japanese site K2; 47oN 160oE). There are strong contrasts between these sites in rates of production, export, particle composition and expected remineralization length scales.</p>
<p>Evidence for variability in the flux vs. depth relationship of sinking particles is not in dispute, but the controls on particle transport efficiency through the twilight zone remain poorly understood. A lack of reliable flux and particle characterization data within the twilight zone has hampered our ability to make progress in this area, and no single approach is likely to resolve these issues. The proposed study will apply quantitative modeling to determine the net effects of the individual particle processes on the effective transport of carbon and other elements and to place the shipboard observations in the context of spatial and temporal variations in these processes</p>
<p>Besides the obvious contributions to the study of the oceanic and planetary carbon cycles, there are broader outcomes and impacts forthcoming from this project. Graduate and undergraduate students will be included in all aspects of the research, and the involvement of non-US PIs will encourage exchange of students and post-docs between labs in different countries. In addition, the component groups will continue to maintain science web sites designed for both public and scientific exchange where the broader and specific goals and outcomes of this work can be communicated.</p>
<p><em>Original PI-provided project description:</em><br />
The main goal of VERTIGO is the investigation of the mechanisms that control the efficiency of particle transport through the mesopelagic portion of the water column.</p>
<p>Question: What controls the efficiency of particle transport between the surface and deep ocean? More specifically, what is the fate of sinking particles leaving the upper ocean and what factors influence remineralization length scales for different sinking particle classes? VERTIGO researchers have set out to test two basic hypotheses regarding remineralization control, namely:<br />
1. particle source characteristics are the dominant control on the efficiency of particle transport; and/or that<br />
2. mid-water processing, either by zooplankton or bacteria, controls transport efficiency.</p>
<p>To test their hypotheses, they will conduct process studies in the field focused on particle flux and composition changes in the upper 500-1000m of the ocean. The basic approach is to examine changes in particle composition and flux with depth within a given source region using a combination of approaches, many of which are new to the field. These include neutrally buoyant sediment traps, particle pumps, settling columns and respiration chambers, along with the development of new biological and geochemical tools for an integrated biogeochemical assessment of the biological pump. Three week process study cruises have been planned at two sites - the Hawaii Ocean Time-series site (HOT) and a new moored time-series site in the subarctic NW Pacific (Japanese site K2; 47oN 160oE) - where there are strong contrasts in rates of production, export, particle composition and expected remineralization length scales.</p>
<p>Evidence for variability in the flux vs. depth relationship of sinking particles is not in dispute but the controls on particle transport efficiency through the twilight zone remain poorly understood. A lack of reliable flux and particle characterization data within the twilight zone has hampered our ability to make progress in this area, and no single approach is likely to resolve these issues. The proposed study will apply quantitative modeling to determine the net effects of the individual particle processes on the effective transport of carbon and other elements, and to place the shipboard observations in the context of spatial and temporal variations in these processes. For rapid progress in this area, we have organized this effort as a group proposal taking advantage of expertise in the US and international community.</p>
<p>The efficiency of particle transport is important for an accurate assessment of the ocean C sink. Globally, the magnitude and efficiency of the biological pump will in part modulate levels of atmospheric CO2. We maintain that to understand present day ocean C sequestration and to evaluate potential strategies for enhancing sequestration, we need to assess possible changes in the efficiency of particle transport due to climate variability or via purposeful manipulations of C uptake, such as via iron fertilization.</p>
<p><em>VERTIGO Acknowledgments: (</em>from K.O. Buesseler, et al / Deep-Sea Research II 55 (2008) 1522-1539) We thank the officers, crew and shore-based support teams for the R/V Kilo Moana (2004) and R/V Roger Revelle (2005). Funding for VERTIGO was provided primarily by research grants from the US National Science Foundation Programs in Chemical and Biological Oceanography (KOB, CHL, MWS, DKS, DAS). Additional US and non-US grants included: US Department of Energy, Office of Science, Biological and Environmental Research Program (JKBB); the Gordon and Betty Moore Foundation (DMK); the Australian Cooperative Research Centre program and Australian Antarctic Division (TWT); Chinese NSFC and MOST programs (NZJ); Research Foundation Flanders and Vrije Universiteit Brussel (FD, ME); JAMSTEC (MCH); New Zealand Public Good Science Foundation (PWB); and internal WHOI sources and a contribution from the John Aure and Cathryn Ann Hansen Buesseler Foundation (KOB). A number of individuals at sea and on shore, helped make the VERTIGO project a success, including: J. Andrews, C. Bertrand, R. Bidigare III, S. Bray, K. Casciotti, M. Charette, R. Condon, J. Cope, E. Fields, M. Gall, M. Gonneea, P. Henderson, T. Kobari, D. Kunz, S. Saitoh, S. Manganini, C. Moy, S. Okamoto, S. Pike, L. Robertson, D. Ruddick and Y. Zhang. Suggestions by three anonymous reviewers and help by the editor, R. Lampitt, are also greatly appreciated.</p>
VERTIGO
largerWorkCitation
project
eng; USA
oceans
Hawaiian Islands, HOT Site; NW, SubArctic Pacific Ocean - K2 Site
2008-11-12
HOT site and subarctic NW Pacific
0
BCO-DMO catalogue of parameters from Barium VUB - Dissolved Ba; particulate Ba, Sr, Ca, Al from Niskins from VERTIGO cruises KM0414, ZHNG09RR from the Hawaiian Islands HOT Site, NW SubArctic Pacific Ocean K2 Site, 2004-2005 (VERTIGO 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/15528.rdf
Name: Cruise_ID
Units: text
Description: VERTIGO cruise name
http://lod.bco-dmo.org/id/dataset-parameter/15529.rdf
Name: date
Units: YYYYMMDD
Description: date sampling began (GMT)
http://lod.bco-dmo.org/id/dataset-parameter/15530.rdf
Name: event
Units: dimensionless
Description: unique sampling event
http://lod.bco-dmo.org/id/dataset-parameter/15531.rdf
Name: ev_code
Units: alphanumeric
Description: event code from cruise log
http://lod.bco-dmo.org/id/dataset-parameter/15532.rdf
Name: lon
Units: decimal degs
Description: longitude, negative denotes West
http://lod.bco-dmo.org/id/dataset-parameter/15533.rdf
Name: lat
Units: decimal degs
Description: latitude, negative denotes South
http://lod.bco-dmo.org/id/dataset-parameter/15534.rdf
Name: date_local
Units: YYYYMMDD
Description: date sampling began (local)
http://lod.bco-dmo.org/id/dataset-parameter/15535.rdf
Name: cast
Units: text
Description: CTD cast id
http://lod.bco-dmo.org/id/dataset-parameter/15536.rdf
Name: bot
Units: dimensionless
Description: Niskin bottle number
http://lod.bco-dmo.org/id/dataset-parameter/15537.rdf
Name: press
Units: decibars
Description: pressure, from CTD
http://lod.bco-dmo.org/id/dataset-parameter/15538.rdf
Name: Ba_diss
Units: Nanomoles per liter (nmol/l)
Description: Dissloved Ba
http://lod.bco-dmo.org/id/dataset-parameter/15539.rdf
Name: Ba_part
Units: Picomoles per liter (pmol/l)
Description: Particulate Ba
http://lod.bco-dmo.org/id/dataset-parameter/15540.rdf
Name: Sr_part
Units: Picomoles per liter (pmol/l)
Description: Particulate Sr
http://lod.bco-dmo.org/id/dataset-parameter/15541.rdf
Name: Ca_part
Units: Nanomoles per liter (nmol/l)
Description: Particulate Ca
http://lod.bco-dmo.org/id/dataset-parameter/15542.rdf
Name: Al_part
Units: Nanomoles per liter (nmol/l)
Description: Particulate Al
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
16077
https://datadocs.bco-dmo.org/file/oAAmBzPUvn82oM/bariumVUB_niskin.csv
bariumVUB_niskin.csv
Primary data file for dataset ID 2955
download
https://www.bco-dmo.org/dataset/2955/data/download
download
onLine
dataset
<pre>
Methodology: <a
href="http://ocb.whoi.edu/VERTIGO/PI-NOTES/multi-ship_bariumVUB_niskin.html">Methodology</a>
Change history: YYMMDD
080710: contributed by Frank Dehairs
081112: Cruise_ID added manually
date, event, ev_code, lon, lat from cruise logs merged with original data
one single multi-ship dataset generated for both KM0414 and RR_K2 data
081112: added to OCB database; Steve Gegg (sgegg@whoi.edu), OCB DMO
DMO Note 1: Comments in cells from original spreadsheets preserved below
KM0414/ALOHA:
date cast bot parameter value Comment
20040704 81 15 Ba_part 6 Frank: suspect data
20040706 80 11 Ba_part 260 Frank: ICP-OES result
20040706 80 11 Sr_part 178 Frank: ICP-OES result
RR_K2/K2:
(none)
DMO Note 2: Used common "cast" id from these data to determine sample
position, date and event code for Niskin data
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/KM0414/log.html0">KM0414 event log</a>
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/RR_K2/log.html0">RR_K2 event log</a>
</pre>
from Cruise: KM0414 <pre>
Methodology: <a
href="http://ocb.whoi.edu/VERTIGO/PI-NOTES/multi-ship_bariumVUB_niskin.html">Methodology</a>
Change history: YYMMDD
080710: contributed by Frank Dehairs
081112: Cruise_ID added manually
date, event, ev_code, lon, lat from cruise logs merged with original data
one single multi-ship dataset generated for both KM0414 and RR_K2 data
081112: added to OCB database; Steve Gegg (sgegg@whoi.edu), OCB DMO
DMO Note 1: Comments in cells from original spreadsheets preserved below
KM0414/ALOHA:
date cast bot parameter value Comment
20040704 81 15 Ba_part 6 Frank: suspect data
20040706 80 11 Ba_part 260 Frank: ICP-OES result
20040706 80 11 Sr_part 178 Frank: ICP-OES result
DMO Note 2: Used common "cast" id from these data to determine sample
position, date and event code for Niskin data
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/KM0414/log.html0">KM0414 event log</a>
</pre>
from Cruise: ZHNG09RR <pre>
Methodology: <a
href="http://ocb.whoi.edu/VERTIGO/PI-NOTES/multi-ship_bariumVUB_niskin.html">Methodology</a>
Change history: YYMMDD
080710: contributed by Frank Dehairs
081112: Cruise_ID added manually
date, event, ev_code, lon, lat from cruise logs merged with original data
one single multi-ship dataset generated for both KM0414 and RR_K2 data
081112: added to OCB database; Steve Gegg (sgegg@whoi.edu), OCB DMO
DMO Note 2: Used common "cast" id from these data to determine sample
position, date and event code for Niskin data
<a href="http://ocb.whoi.edu/jg/serv/OCB/VERTIGO/RR_K2/log.html0">RR_K2 event log</a>
</pre>
Specified by the Principal Investigator(s)
from Cruise: KM0414 <a href=http://ocb.whoi.edu/VERTIGO/PI-NOTES/multi-ship_bariumVUB_niskin.html>PI notes for Dissolved Ba; particulate Ba, Sr, Ca, Al from Niskins</a>
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
Cruise: KM0414
KM0414
R/V Kilo Moana
Community Standard Description
International Council for the Exploration of the Sea
R/V Kilo Moana
vessel
KM0414
Kenneth O. Buesseler
Woods Hole Oceanographic Institution
Cruise: ZHNG09RR
ZHNG09RR
R/V Roger Revelle
Community Standard Description
International Council for the Exploration of the Sea
R/V Roger Revelle
vessel
ZHNG09RR
Kenneth O. Buesseler
Woods Hole Oceanographic Institution
R/V Kilo Moana
Community Standard Description
International Council for the Exploration of the Sea
R/V Kilo Moana
vessel
R/V Roger Revelle
Community Standard Description
International Council for the Exploration of the Sea
R/V Roger Revelle
vessel