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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/2925.rdf" xlink:actuate="onRequest">VERTIGO cruise data inventory of expected VERTIGO data from cruises KM0414, ZHNG09RR from the Hawaiian Islands HOT Site, NW SubArctic Pacific Ocean K2 Site, 2004-2005 (VERTIGO project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Buesseler, K. O., Buesseler, K. O. (2009) VERTIGO cruise data inventory of expected VERTIGO data from 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 24 February 2009) Version Date 2009-02-24 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/2925 [access date]</gco:CharacterString>
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        <gco:CharacterString>VERTIGO Cruise Data Inventory - Status of expected VERTIGO data contributions Dataset Description: &amp;lt;p&amp;gt;VERTIGO Cruise Data Inventory - Status of expected VERTIGO data contributions&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;pre&amp;gt;
 &amp;lt;strong&amp;gt;PI:&amp;lt;/strong&amp;gt;              VERTIGO Project Office
 &amp;lt;strong&amp;gt;of:&amp;lt;/strong&amp;gt;              Woods Hole Oceanographic Institution (WHOI)
 &amp;lt;strong&amp;gt;dataset:&amp;lt;/strong&amp;gt;         Inventory of expected results from cruises
 &amp;lt;strong&amp;gt;dates:&amp;lt;/strong&amp;gt;           2004 - 2005
 &amp;lt;strong&amp;gt;location:&amp;lt;/strong&amp;gt;        NW Pacific / NP8 / 160E 47N
 &amp;lt;strong&amp;gt;project/cruise:&amp;lt;/strong&amp;gt;  all VERTIGO cruises
 &amp;lt;strong&amp;gt;platform:&amp;lt;/strong&amp;gt;        R/V Kilo Moana and Roger Revelle
 
 
 The Cruise INVENTORY offers a dynamic view of the data status for each cruise.
 The Ocean Carbon Biogeochemistry Data Management Office (OCB DMO) maintains
 this information as part of the process of building the OCB data collection.
 
 If you are a participating PI and believe the information to be inaccurate,
 PLEASE contact the office so we may update our information.

 
 Thank you, Cyndy Chandler (cchandler AT whoi.edu), (OCB DMO, WHOI)

 Status of expected VERTIGO data contributions: 
   Investigators contribute results to the VERTIGO project office.
   (Contributed=p indicates preliminary data)
   Following QA, final data are added to the OCB data system.
   When complete, processing status column links to data.
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 &amp;lt;/pre&amp;gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;&lt;em&gt;NSF Award Abstract:&lt;/em&gt;&lt;br /&gt;
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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;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&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;&lt;em&gt;Original PI-provided project description:&lt;/em&gt;&lt;br /&gt;
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.&lt;/p&gt;
&lt;p&gt;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:&lt;br /&gt;
1. particle source characteristics are the dominant control on the efficiency of particle transport; and/or that&lt;br /&gt;
2. mid-water processing, either by zooplankton or bacteria, controls transport efficiency.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;&lt;em&gt;VERTIGO Acknowledgments: (&lt;/em&gt;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.&lt;/p&gt;</gco:CharacterString>
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	Description: &lt;p&gt;data availability flag where O = open access and R = restricted access&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/16795.rdf
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 &amp;lt;strong&amp;gt;PI:&amp;lt;/strong&amp;gt;              VERTIGO Project Office
 &amp;lt;strong&amp;gt;of:&amp;lt;/strong&amp;gt;              Woods Hole Oceanographic Institution (WHOI)
 &amp;lt;strong&amp;gt;dataset:&amp;lt;/strong&amp;gt;         Inventory of expected results from cruises
 &amp;lt;strong&amp;gt;dates:&amp;lt;/strong&amp;gt;           2004 - 2005
 &amp;lt;strong&amp;gt;location:&amp;lt;/strong&amp;gt;        NW Pacific / NP8 / 160E 47N
 &amp;lt;strong&amp;gt;project/cruise:&amp;lt;/strong&amp;gt;  all VERTIGO cruises
 &amp;lt;strong&amp;gt;platform:&amp;lt;/strong&amp;gt;        R/V Kilo Moana and Roger Revelle
 
 
 The Cruise INVENTORY offers a dynamic view of the data status for each cruise.
 The Ocean Carbon Biogeochemistry Data Management Office (OCB DMO) maintains
 this information as part of the process of building the OCB data collection.
 
 If you are a participating PI and believe the information to be inaccurate,
 PLEASE contact the office so we may update our information.

 
 Thank you, Cyndy Chandler (cchandler AT whoi.edu), (OCB DMO, WHOI)

 Status of expected VERTIGO data contributions: 
   Investigators contribute results to the VERTIGO project office.
   (Contributed=p indicates preliminary data)
   Following QA, final data are added to the OCB data system.
   When complete, processing status column links to data.
   A parameter value of n indicates 'no' and y indicates 'yes'.
 &amp;lt;/pre&amp;gt;

from Cruise: KM0414 &lt;pre&gt;
 &lt;b&gt;PI:&lt;/b&gt;              Ken Buesseler (project lead PI)
 &lt;b&gt;of:&lt;/b&gt;              Woods Hole Oceanographic Institution (WHOI)
 &lt;b&gt;dataset:&lt;/b&gt;         Inventory of expected results from cruise
 &lt;b&gt;dates:&lt;/b&gt;           20 June 2004 to 10 July 2004
 &lt;b&gt;location:&lt;/b&gt;        N: 23.75  S: 22.08  W: -159.08  E: -156.92
 &lt;b&gt;project/cruise:&lt;/b&gt;  VERTIGO/KM0414
 &lt;b&gt;platform:&lt;/b&gt;        R/V Kilo Moana
  
 The Cruise INVENTORY offers a dynamic view of the data status for each cruise.
 The Ocean Carbon and Biogeochemistry Data Management Office (OCB DMO) maintains
 this information as part of the process of building the OCB data collection.
 
 If you are a participating PI and believe the information to be inaccurate,
 PLEASE contact the office so we may update our information.

 Thank you, Cyndy Chandler (cchandler AT whoi.edu), (OCB DMO, WHOI)

 Status of expected VERTIGO data contributions: 
   Investigators contribute results to the VERTIGO project office.
   (Contributed=p indicates preliminary data)
   Following QA, final data are added to the OCB data system.
   When complete, processing status column links to data.
   A parameter value of n indicates 'no' and y indicates 'yes'.
 &lt;/pre&gt;

from Cruise: ZHNG09RR &lt;pre&gt;
 &lt;b&gt;PI:&lt;/b&gt;              Ken Buesseler (Chief Scientist)
 &lt;b&gt;of:&lt;/b&gt;              Woods Hole Oceanographic Institution (WHOI)
 &lt;b&gt;dataset:&lt;/b&gt;         Inventory of expected results from cruise
 &lt;b&gt;cruise dates:&lt;/b&gt;    21 July 2005 to 27 August 2005 (20050721-20050827)
 &lt;b&gt;location:&lt;/b&gt;        NW Pacific / NP8 / 160E 47N
 &lt;b&gt;project/cruise:&lt;/b&gt;  VERTIGO/RR_K2
 &lt;b&gt;platform:&lt;/b&gt;        R/V Roger Revelle
 
 
 The Cruise INVENTORY offers a dynamic view of the data status for each cruise.
 The Ocean Carbon and Biogeochemistry Data Management Office (OCB DMO) maintains
 this information as part of the process of building the OCB data collection.
 
 If you are a participating PI and believe the information to be inaccurate,
 PLEASE contact the office so we may update our information.

 Thank you, Cyndy Chandler (cchandler AT whoi.edu), (OCB DMO, WHOI)

 Status of expected VERTIGO data contributions: 
   Investigators contribute results to the VERTIGO project office.
   (Contributed=p indicates preliminary data)
   Following QA, final data are added to the OCB data system.
   When complete, processing status column links to data.
   A parameter value of n indicates 'no' and y indicates 'yes'.
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