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<article language="en">
	<journal>
		<journal_title>Earth System Science Data Discussions</journal_title>
		<journal_url>www.earth-syst-sci-data-discuss.net</journal_url>
		<eissn>1866-3591</eissn>
		<volume_number>2</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/essdd-2-331-2009</doi>
	<article_url>http://www.earth-syst-sci-data-discuss.net/2/331/2009/</article_url>
	<abstract_html>http://www.earth-syst-sci-data-discuss.net/2/331/2009/essdd-2-331-2009.html</abstract_html>
	<fulltext_pdf>http://www.earth-syst-sci-data-discuss.net/2/331/2009/essdd-2-331-2009.pdf</fulltext_pdf>
	<start_page>331</start_page>
	<end_page>365</end_page>
	<publication_date>2009-08-27</publication_date>
	<article_title content_type="html">Consistency of cruise data of the CARINA database in the Atlantic sector of the Southern Ocean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Hoppema</name>
			<email>mario.hoppema@awi.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Velo</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>S. van Heuven</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>T. Tanhu</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>R. M. Key</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>X. Lin</name>
		</author>
		<author numeration="7" affiliations="6">
			<name>D. C. E. Bakker</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>F. F. Perez</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>A. F. Ríos</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>C. Lo Monaco</name>
		</author>
		<author numeration="11" affiliations="8">
			<name>C. L. Sabine</name>
		</author>
		<author numeration="12" affiliations="9">
			<name>M. Álvarez</name>
		</author>
		<author numeration="13" affiliations="10">
			<name>R. G. J. Bellerby</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Alfred Wegener Institute for Polar and Marine Research, Climate Sciences, Postfach 120161, 27515 Bremerhaven, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Instituto de Investigaciones Marinas – CSIC, Eduardo Cabello 6, 36208 Vigo, Spain</affiliation>
		<affiliation numeration="3" content_type="html">University of Groningen, Department of Ocean Ecosystems, Biological Center, P.O.Box 14, 9750 AA Groningen, The Netherlands</affiliation>
		<affiliation numeration="4" content_type="html">Leibniz Institute for Marine Sciences, Marine Biogeochemistry, Kiel, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Atmospheric and Oceanic Sciences Program, Princeton Univ., Princeton, NJ 08544, USA</affiliation>
		<affiliation numeration="6" content_type="html">School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK</affiliation>
		<affiliation numeration="7" content_type="html">LOCEAN-IPSL, Université Pierre et Marie Curie, Paris, France</affiliation>
		<affiliation numeration="8" content_type="html">NOAA Pacific Marine Environmental Lab., 7600 Sand point Way NE, Seattle, WA 98115, USA</affiliation>
		<affiliation numeration="9" content_type="html">IMEDEA (CSIC-UIB), Miquel Marqués 21, 07190 Esporles, Spain</affiliation>
		<affiliation numeration="10" content_type="html">Bjerknes Centre for Climate Research, University of Bergen, Allegaten 55, 5007 Bergen, and Geophysical Institute, University of Bergen, Allegaten 70, 5007 Bergen, Norway</affiliation>
	</affiliations>
	<abstract content_type="html">Initially a North Atlantic project, the CARINA carbon synthesis was extended
to include the Southern Ocean. Carbon and relevant hydrographic and
geochemical ancillary data from cruises all across the Arctic Mediterranean
Seas, Atlantic and Southern Ocean were released to the public and merged
into a new database as part of the CARINA synthesis effort. Of a total of
188 cruises, 37 cruises are part of the Southern Ocean, including 11 from
the Atlantic sector. The variables from the Atlantic sector cruises,
including dissolved inorganic carbon (TCO&lt;sub&gt;2&lt;/sub&gt;), total alkalinity, oxygen,
nitrate, phosphate and silicate, were examined for cruise-to-cruise
consistency. Seawater pH and chlorofluorocarbons (CFCs) are also part of the
database, but the pH quality control (QC) is described in another Earth
System Science Data publication, while the complexity of the Southern Ocean
physics and biogeochemistry prevented a proper QC analysis of the CFCs. The
area-specific procedures of quality control, including crossover analysis
between stations and inversion analysis of all crossover data (i.e. secondary QC), are briefly described for the Atlantic sector of the Southern
Ocean. Data from an existing, quality controlled database (GLODAP) were used
as a reference for our computations – however, the reference data were
included into the analysis without applying the recommended GLODAP
adjustments so the corrections could be independently verified. The outcome
of this effort is an internally consistent, high-quality carbon data set for
all cruises, including the reference cruises. The suggested corrections by
the inversion analysis were allowed to vary within a fixed envelope, thus
accounting for natural variability. The percentage of cruises adjusted
ranged from 31% (for nitrate) to 54% (for phosphate) depending on the
variable.</abstract>
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</article>

