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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/2957.rdf" xlink:actuate="onRequest">Cruise event log from R/V Kilo Moana, R/V Roger Revelle 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>&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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  cruise: KM0414 
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    and original hardcopy of cruise event log sheets 
   
  project:  VERTIGO (VERtical Transport In the Global Ocean) 
  cruise:  RR_K2 / ZHNG09RR 
  platform:  R/V Roger Revelle 
  location:  NW Pacific / NP8 / 160E 47N 
  cruise dates:  21 July 2005 to 27 August 2005 
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                <gco:CharacterString>&amp;lt;p&amp;gt;(see platform deployments)&amp;lt;/p&amp;gt;

from Cruise: KM0414 &lt;pre&gt;Methodology: none provided with data
 
 Change history: YYMMDD
    050706: downloaded &lt;a 
href=&quot;http://www.icess.ucsb.edu/~damk2000/VERTIGO/Vertigo_Log.htm&quot;&gt;original&lt;/a&gt; version provided by Damien Ku
nz (ICESS), damk2000@icess.ucsb.edu
    060905: corrected GMT and HST times for CTD event 04185_1421 (per Chief Scientist request)
    090225: changed date_GMT parameter name to date and time_GMT to time; no change to data
 
 Note: HST dates and times are Hawaii Standard Time (HST = GMT -10)
       and represent local time during the cruise at 23 N, 158 W
       This cruise is also referred to as the ALOHA cruise.
 
 Map:  &lt;a href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/sta_map_KM0414.gif&quot;&gt;cruise study area&lt;/a&gt;
 
 Final Daily Cruise Plan with Overview of Sampling Operations: September 2006 version 
    downloaded from VERTIGO Web site 01 August 2007; available as the original 
    &lt;a href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/ALOHA_final_cruise_activities.xls&quot;&gt;Excel format&lt;/a&gt; or &lt;a 
    href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/ALOHA_final_cruise_activities.pdf&quot;&gt;PDF file&lt;/a&gt;
 
 &lt;/pre&gt;

from Cruise: ZHNG09RR &lt;pre&gt; Added: 21 January 2006 by Cyndy Chandler (cchandler@whoi.edu), OCB CDMO
 
 DMO note: original version copied on 19 January 2006 from the August 2005 shipboard DVD
           and verified against the original Event Log sheets and the SIO POSITION DATA SHEETS;
           the CTD event, date, time, latitude and longitude are from CTD cast NMEA header lines;
           T_local (local time at study area) was computed by adjusting GMT time by +11
 
 Cruise track:  &lt;a href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/vertigo_map2.jpg&quot;&gt;cruise study area map&lt;/a&gt;
 
 Final Daily Cruise Plan and Overview of Sampling Activities: 28 September 2005 version 
   downloaded from VERTIGO Web site 01 August 2007; available as the original &lt;a
   href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/RR_K2_planned_activities.xls&quot;&gt;Excel format&lt;/a&gt; or &lt;a 
   href=&quot;http://ocb.whoi.edu/VERTIGO/CRUISES/RR_K2_planned_activities.pdf&quot;&gt;PDF file&lt;/a&gt;
 
 Daily updates:  &lt;a href=&quot;http://cafethorium.whoi.edu/website/cruises/vertigok2_updates.html&quot;
&gt;daily journal entries&lt;/a&gt; contributed by cruise participants
 
 &lt;a href=&quot;http://ocb.whoi.edu/VERTIGO/PI-NOTES/vertigo_ev_codes.html&quot;&gt;Explanation&lt;/a&gt; of sampling event/method abbreviations
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