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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/2811.rdf" xlink:actuate="onRequest">SOFeX Polar Star XBT temperature profiles from USCGC Polar Star cruise PS02_2002 from the Southern Ocean, south of New Zealand in 2002 (SOFeX project)</gmx:Anchor>
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        <gco:CharacterString>SOFeX Polar Star XBT temperature profiles Methods and Sampling: &amp;lt;pre&amp;gt;
Methodology: none contributed with data

Related information:
    Two plots of temperature from transects through the patch, were also
    contributed: &amp;lt;a 
href=&amp;quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_EW_PS.jpg&amp;quot;&amp;gt;EW transect&amp;lt;/a&amp;gt; and &amp;lt;a 
href=&amp;quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_NS_PS.jpg&amp;quot;&amp;gt;NS transect&amp;lt;/a&amp;gt;

DMO note:  The final day in the SOFeX study area was 21 February 2002
    after which the ship headed to Valparaiso, Chile.  The XBT data has not been 
    processed or quality controlled, and contains both test profiles away from the 
    SOFEX site and bad drops. The early part of the Valparaiso transect is included.
&amp;lt;/pre&amp;gt;</gco:CharacterString>
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                            <gco:CharacterString>The two main objectives of the Iron Synthesis program (SCOR Working Group proposal, 2005), are:
1. Data compilation: assembling a common open-access database of the in situ iron experiments, beginning with the first period (1993-2002; Ironex-1, Ironex-2, SOIREE, EisenEx, SEEDS-1; SOFeX, SERIES) where primary articles have already been published, to be followed by the 2004 experiments where primary articles are now in progress (EIFEX, SEEDS-2; SAGE, FeeP); similarly for the natural fertilizations S.O.JGOFS (1992), CROZEX (2004/2005) and KEOPS (2005).
2. Modeling and data synthesis of specific aspects of two or more such experiments for various topics such as physical mixing, phytoplankton productivity, overall ecosystem functioning, iron chemistry, CO2 budgeting, nutrient uptake ratios, DMS(P) processes, and combinations of these variables and processes.
SCOR Working Group proposal, 2005. &quot;The Legacy of in situ Iron Enrichments: Data Compilation and Modeling&quot;.
http://www.scor-int.org/Working_Groups/wg131.htm
See also: SCOR Proceedings Vol. 42 Concepcion, Chile October 2006, pgs: 13-16 2.3.3 Working Group on The Legacy of in situ Iron Enrichments: Data Compilation and Modeling.
The first objective of the Iron Synthesis program involves a data recovery effort aimed at assembling a common, open-access database of data and metadata from a series of in-situ ocean iron fertilization experiments conducted between 1993 and 2005. Initially, funding for this effort is being provided by the Scientific Committee on Oceanic Research (SCOR) and the U.S. National Science Foundation (NSF).
Through the combined efforts of the principal investigators of the individual projects and the staff of Biological and Chemical Oceanography Data Management Office (BCO-DMO), data currently available primarily through individuals, disparate reports and data agencies, and in multiple formats, are being collected and prepared for addition to the BCO-DMO database from which they will be freely available to the community.
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1. Level 1, basic metadata
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2. Level 2, detailed metadata and basic shipboard data and routine ship's operations
(e.g., CTDs, underway measurements, sampling event logs);
3. Level 3, detailed metadata and data from specialized observations
(e.g., discrete observations, experimental results, rate measurements) and
4. Level 4, remaining datasets
(e.g., highest level of detailed data available from each study).
Collaboration with BCO-DMO staff began in March of 2008 and initial efforts have been directed toward basic project descriptions, levels 1 and 2 metadata and basic data, with detailed and more detailed data files being incorporated as they become available and are processed.
Related file
Program Documentation
The Iron Synthesis Program is funded jointly by the Scientific Committee on Oceanic Research (SCOR) and the U.S. National Science Foundation (NSF).</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;Before he passed away in 1993, John Martin suggested that an increase in the flow of iron-rich dust to the ocean causes phytoplankton (single celled algae) to grow. The increased photosynthesis removes carbon dioxide from surface waters as the algae create biomass. This carbon dioxide is replaced by carbon dioxide gas that flows into the sea from the atmosphere. Reduced carbon dioxide in the atmosphere cools the planet (CO2 is a greenhouse gas that warms the earth). The results of this work, funded by the National Science Foundation, the Department of Energy, and the US Coast Guard, will be a much better understanding of how biological processes may regulate climate. (see Related Info: Fe cycle)&lt;/p&gt;
&lt;p&gt;A direct test of the 'Martin Hypothesis' that trace concentrations of Fe are responsible for phytoplankton's ability to grow by direct experimental addition of Fe to the surface waters. Consequently the distribution of bioavailable Fe in the surface waters determines large geographical areas primary production and the following flux of fixed organic matter to the deep sea. The aim of the SOFeX project is to investigate the effects of iron fertilization on the productivity of the Southern Ocean. The results of this work will contribute significantly to our understanding of important biogeochemical processes which bear directly on the global carbon cycle, atmospheric carbon dioxide concentration, and climate control.&lt;/p&gt;
&lt;p&gt;The SOFeX-N and SOFeX-S designations are sometimes used to distinguish between two iron enriched patches - one in low silicate waters north of the polar front (SOFEX-N), and the other in high silicate waters south of the polar front (SOFEX-S). All three ships, Melville (MV), Revelle (RR) and Polar Star (PS), worked in SOFEX-S, but only the Revelle and Melville worked in the SOFeX N patch and shuttled between the two patches.&lt;/p&gt;</gco:CharacterString>
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Related information:
    Two plots of temperature from transects through the patch, were also
    contributed: &amp;lt;a 
href=&amp;quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_EW_PS.jpg&amp;quot;&amp;gt;EW transect&amp;lt;/a&amp;gt; and &amp;lt;a 
href=&amp;quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_NS_PS.jpg&amp;quot;&amp;gt;NS transect&amp;lt;/a&amp;gt;

DMO note:  The final day in the SOFeX study area was 21 February 2002
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    SOFEX site and bad drops. The early part of the Valparaiso transect is included.
&amp;lt;/pre&amp;gt;

from Cruise: PS02_2002 &lt;pre&gt;
Methodology: none contributed with data

Related information:
    Two plots of temperature from transects through the patch, were also
    contributed: &lt;a 
href=&quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_EW_PS.jpg&quot;&gt;EW transect&lt;/a&gt; and &lt;a 
href=&quot;http://ocb.whoi.edu/SOFeX/PI-NOTES/XBT_NS_PS.jpg&quot;&gt;NS transect&lt;/a&gt;

DMO note:  The final day in the SOFeX study area was 21 February 2002
    after which the ship headed to Valparaiso, Chile.  The XBT data has not been 
    processed or quality controlled, and contains both test profiles away from the 
    SOFEX site and bad drops. The early part of the Valparaiso transect is included.
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Change history: YYMMDD
    070305: XBT data file contributed by Ken Buesseler (WHOI)
            added to OCB by Cyndy Chandler (cchandler@whoi.edu)
&amp;lt;/pre&amp;gt;

from Cruise: PS02_2002 &lt;pre&gt;
Change history: YYMMDD
    070305: XBT data file contributed by Ken Buesseler (WHOI)
            added to OCB by Cyndy Chandler (cchandler@whoi.edu)
&lt;/pre&gt;</gco:CharacterString>
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