<?xml version="1.0" encoding="utf-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns="http://purl.org/rss/1.0/" xmlns:dc="http://purl.org/dc/elements/1.1/"><channel rdf:about="http://www.earth-syst-sci-data-discuss.net/xml/rss1_0.xml"><title>ESSDD - Latest Articles</title><link>http://www.earth-syst-sci-data-discuss.net/</link><description>Earth System Science Data Discussions Latest Articles</description><items><rdf:Seq><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/231/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/195/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/143/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/131/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/109/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/79/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/55/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/27/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/3/1/2010/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/579/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/555/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/537/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/493/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/477/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/421/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/367/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/331/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/309/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/281/2009/" /><rdf:li resource="http://www.earth-syst-sci-data-discuss.net/2/241/2009/" /></rdf:Seq></items></channel><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/231/2010/"><title>A consistent dataset of Antarctic ice sheet topography, cavity geometry, and global bathymetry</title><link>http://www.earth-syst-sci-data-discuss.net/3/231/2010/</link><description>&lt;b&gt;A consistent dataset of Antarctic ice sheet topography, cavity geometry, and global bathymetry&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 231-257, 2010&lt;br /&gt;&lt;br /&gt;Author(s): R. Timmermann, A. Le Brocq, T. Deen, E. Domack, P. Dutrieux, B. Galton-Fenzi, H. Hellmer, A. Humbert, D. Jansen, A. Jenkins, A. Lambrecht, K. Makinson, F. Niederjasper, F. Nitsche, O. A. Nøst, L. H. Smedsrud, and W. H. F. Smith&lt;br /&gt;&lt;br /&gt;Sub-ice shelf circulation and freezing/melting rates in ocean general
circulation models depend critically on an accurate and consistent
representation of cavity geometry. Existing global or pan-Antarctic data sets
have turned out to contain various inconsistencies and inaccuracies. The goal
of this work is to compile independent regional fields into a global data
set. We use the S-2004 global 1-min bathymetry as the backbone and add an
improved version of the BEDMAP topography (ALBMAP bedrock topography) for an
area that roughly coincides with the Antarctic continental shelf. The
position of the merging line is individually chosen in different sectors in
order to get the best out of each data set. High-resolution gridded data for
ice shelf topography and cavity geometry of the Amery,
Fimbul, Filchner-Ronne, Larsen C and George VI Ice Shelves, and for Pine
Island Glacier are carefully merged into the ambient ice and ocean
topographies. Multibeam survey data for bathymetry in the former Larsen B
cavity and the southeastern Bellingshausen Sea have been obtained from the
data centers of Alfred Wegener Institute (AWI), British Antarctic Survey
(BAS) and Lamont-Doherty Earth Observatory (LDEO), gridded, and blended into
the existing bathymetry map. The resulting global 1-min topography data
set (RTopo-1) contains maps for upper and lower ice surface heights, bedrock topography, and consistent masks for open ocean, grounded ice, floating ice,
and bare land surface. The data set is available in NetCDF format from the
PANGAEA database at doi:10.1594/pangaea.741917.</description><dc:date>2010-07-29T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/195/2010/"><title>An improved Antarctic dataset for high resolution numerical ice sheet models (ALBMAP v1)</title><link>http://www.earth-syst-sci-data-discuss.net/3/195/2010/</link><description>&lt;b&gt;An improved Antarctic dataset for high resolution numerical ice sheet models (ALBMAP v1)&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 195-230, 2010&lt;br /&gt;&lt;br /&gt;Author(s): A. M. Le Brocq, A. J. Payne, and A. Vieli&lt;br /&gt;&lt;br /&gt;The dataset described in this paper (ALBMAP) has been created for the
purposes of high-resolution numerical ice sheet modelling of the Antarctic
Ice Sheet. It brings together data on the ice sheet configuration (e.g. ice
surface and ice thickness) and boundary conditions, such as the surface air
temperature, accumulation and geothermal heat flux. The ice thickness and
basal topography is based on the BEDMAP dataset (Lythe et al., 2001),
however, there are a number of inconsistencies within BEDMAP and, since its
release, more data has become available. The dataset described here
addresses these inconsistencies, including some novel interpolation schemes
for sub ice-shelf cavities, and incorporates some major new datasets. The
inclusion of new datasets is not exhaustive, this considerable task is left
for the next release of BEDMAP, however, the data and procedure documented
here provides another step forward and demonstrates the issues that need
addressing in a continental scale dataset useful for high resolution ice
sheet modelling. The dataset provides an initial condition that is as close
as possible to present-day ice sheet configuration, aiding modelling of the
response of the Antarctic Ice Sheet to various forcings, which are, at
present, not fully understood.</description><dc:date>2010-06-28T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/143/2010/"><title>The Hamburg Ocean Atmosphere Parameters and Fluxes from Satellite Data – HOAPS-3</title><link>http://www.earth-syst-sci-data-discuss.net/3/143/2010/</link><description>&lt;b&gt;The Hamburg Ocean Atmosphere Parameters and Fluxes from Satellite Data – HOAPS-3&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 143-194, 2010&lt;br /&gt;&lt;br /&gt;Author(s): A. Andersson, K. Fennig, C. Klepp, S. Bakan, H. Graßl, and J. Schulz&lt;br /&gt;&lt;br /&gt;The availability of microwave instruments on satellite platforms allows the
retrieval of essential water cycle components at high quality for improved
understanding and evaluation of water processes in climate modelling.
HOAPS-3, the latest version of the satellite climatology &quot;Hamburg Ocean
Atmosphere Parameters and Fluxes from Satellite Data&quot; provides fields of
turbulent heat fluxes, evaporation, precipitation, freshwater flux and
related atmospheric variables over the global ice-free ocean. This paper
describes the content, methodology and retrievals of the HOAPS climatology. A
sophisticated processing chain, including all available &lt;i&gt;Special Sensor
Microwave Imager&lt;/i&gt; (SSM/I) instruments aboard the satellites of the
Defense Meteorological Satellites Program (DMSP) and careful inter-sensor
calibration, ensures a homogeneous time-series with dense data sampling and
hence detailed information of the underlying weather situations. The
completely reprocessed data set with a continuous time series from 1987 to
2005 contains neural network based algorithms for precipitation and wind
speed and &lt;i&gt;Advanced Very High Resolution Radiometer&lt;/i&gt; (AVHRR) based SST
fields. Additionally, a new 85 GHz synthesis procedure for the defective
SSM/I channels on DMSP F08 from 1989 on has been implemented. Freely
available monthly and pentad means, twice daily composites and scan-based
data make HOAPS-3 a versatile data set for studying ocean-atmosphere
interaction on different temporal and spatial scales. HOAPS-3 data products
are available via &lt;a href=&quot;http://www.hoaps.org&quot; target=&quot;_blank&quot;&gt;http://www.hoaps.org&lt;/a&gt;.</description><dc:date>2010-05-19T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/131/2010/"><title>Data of hydraulic properties of North East and Central German soils</title><link>http://www.earth-syst-sci-data-discuss.net/3/131/2010/</link><description>&lt;b&gt;Data of hydraulic properties of North East and Central German soils&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 131-142, 2010&lt;br /&gt;&lt;br /&gt;Author(s): U. Schindler and L. Müller&lt;br /&gt;&lt;br /&gt;The paper presents a data base of soil hydrological
properties of North East and Central German soils. Included are measured
data of the soil water retention curve and the unsaturated hydraulic
conductivity function. Information to geo reference, soil type and horizon
are given. Additional soil physical data like particle size distribution,
dry bulk density, organic matter content and other variables are presented
and its measurement is methodically described. The data base includes
original measurement results of 278 organic and of 497 mineral soil samples
from 103 sites. The mineral soils cover a wide range of texture classes and
dry bulk densities. The organic soils and samples vary in dependence on the
degree of decomposition and mineralization, the dry bulk density and the
total porosity.</description><dc:date>2010-05-11T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/109/2010/"><title>EPOCA/EUR-OCEANS data-mining compilation on the impacts of ocean acidification</title><link>http://www.earth-syst-sci-data-discuss.net/3/109/2010/</link><description>&lt;b&gt;EPOCA/EUR-OCEANS data-mining compilation on the impacts of ocean acidification&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 109-130, 2010&lt;br /&gt;&lt;br /&gt;Author(s): A.-M. Nisumaa, S. Pesant, R. G. J. Bellerby, B. Delille, J. Middelburg, J. C. Orr, U. Riebesell, T. Tyrrell, D. Wolf-Gladrow, and J.-P. Gattuso&lt;br /&gt;&lt;br /&gt;The uptake of anthropogenic CO&lt;sub&gt;2&lt;/sub&gt; by the oceans has led to a rise in the
oceanic partial pressure of CO&lt;sub&gt;2&lt;/sub&gt;, and to a decrease in pH and carbonate
ion concentration. This modification of the marine carbonate system is
referred to as ocean acidification. Numerous papers report the effects of
ocean acidification on marine organisms and communities but few have
provided details concerning full carbonate chemistry and complementary
observations. Additionally, carbonate system variables are often reported in
different units, calculated using different sets of dissociation constants
and on different pH scales. Hence the direct comparison of experimental
results has been problematic and often misleading. The need was identified
to (1) gather data on carbonate chemistry, biological and biogeochemical
properties, and other ancillary data from published experimental data, (2) transform
the information into common framework, and (3) make data freely
available. The present paper is the outcome of an effort to integrate ocean
carbonate chemistry data from the literature which has been supported by the
European Network of Excellence for Ocean Ecosystems Analysis (EUR-OCEANS)
and the European Project on Ocean Acidification (EPOCA). A total of 166
papers were identified, 86 contained enough information to readily compute
carbonate chemistry variables, and 67 datasets were archived at PANGAEA –
The Publishing Network for Geoscientific &amp; Environmental Data. This data
compilation is regularly updated as an ongoing mission of EPOCA.

&lt;br&gt;&lt;br&gt;
Data access: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.735138&quot; target=&quot;_blank&quot;&gt;http://doi.pangaea.de/10.1594/PANGAEA.735138&lt;/a&gt;</description><dc:date>2010-03-30T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/79/2010/"><title>Measuring hydrodynamics and sediment transport processes in the Dee estuary</title><link>http://www.earth-syst-sci-data-discuss.net/3/79/2010/</link><description>&lt;b&gt;Measuring hydrodynamics and sediment transport processes in the Dee estuary&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 79-107, 2010&lt;br /&gt;&lt;br /&gt;Author(s): R. Bolaños and A. Souza&lt;br /&gt;&lt;br /&gt;The capability of monitoring and predicting the marine environment leads to
a more sustainable development of coastal and offshore regions. Therefore,
the continuous measurement of environmental processes become an important
source of information. The present paper shows data collected during 6 years, and in particular during 2008, in the Dee Estuary. The data aims to
improve the observations of the mobile sediments in coastal areas and its
forcing hydrodynamics and turbulence. Data involves the deployment of
instrumented rigs measuring sediment in suspension, currents, waves, sea
level, sediment size and bedforms as well as cruise work including grab
sampling, CTD profiles and side-scan sonar. The data covers flood and ebb
tides during spring and neap periods with moderate and mild wave events,
thus, having a good coverage of the processes needed to improve knowledge of
sediment transport and the parameterizations used in numerical modelling.
The data, in raw and treated, is being banked at BODC (British Oceanographic
Data Centre, &lt;a href=&quot;http://www.bodc.ac.uk/&quot; target=&quot;_blank&quot;&gt;http://www.bodc.ac.uk/&lt;/a&gt;) which is the formal
British organization for looking after and distributing data concerning the
marine environment.</description><dc:date>2010-03-03T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/55/2010/"><title>Nordic Seas nutrients data in CARINA</title><link>http://www.earth-syst-sci-data-discuss.net/3/55/2010/</link><description>&lt;b&gt;Nordic Seas nutrients data in CARINA&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 55-78, 2010&lt;br /&gt;&lt;br /&gt;Author(s): J. Olafsson and A. Olsen&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon relevant hydrographic and
hydrochemical parameters from 188 previously non-publicly available cruises
in the Arctic, Atlantic, and Southern Ocean have been retrieved and merged
into a new database: CARINA (CARbon IN the Atlantic). The data have been
subject to rigorous quality control (QC) in order to ensure highest possible
quality and consistency. The data for most of the parameters included were
examined in order to quantify systematic biases in the reported values, i.e.
secondary quality control. Significant biases have been corrected for in the
data products, i.e.~the three merged files with measured, calculated and
interpolated values for each of the three CARINA regions; the Arctic
Mediterranean Seas (AMS), the Atlantic (ATL) and the Southern Ocean (SO).
With the adjustments, the CARINA database is consistent both internally as
well as with GLODAP (Key et al., 2004) and is suitable
for accurate assessments of, for example, oceanic carbon inventories and
uptake rates, and for model validation. The Arctic Mediterranean Seas is the
collective term for the Arctic Ocean and the Nordic Seas, and the quality
control was carried out separately in these two areas. This contribution
presents an account of the quality control of the nutrients (nitrate,
phosphate, and silicate) data from the Nordic Seas in CARINA. Out of the 35
cruises from the Nordic Seas included in CARINA, 33 had nutrients data. The
nitrate data from 4 of these appeared to be of so poor quality that they
should not be used, for phosphate this number is 7 and for silicate it is 3.
We also recommend that the nitrate data from 4 of the cruises should be
adjusted, for phosphate and silicate only data from one cruise should be
adjusted. The final data appears consistent to 5% based on evaluation of
deep data. For nitrate this corresponds to 0.6 &amp;mu;mol kg&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, and for
phosphate and silicate it corresponds to 0.04 and 0.6 &amp;mu;mol kg&lt;sup&gt;&amp;minus;1&lt;/sup&gt;,
respectively.</description><dc:date>2010-03-03T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/27/2010/"><title>NORPERM, the Norwegian Permafrost Database – a TSP NORWAY IPY legacy</title><link>http://www.earth-syst-sci-data-discuss.net/3/27/2010/</link><description>&lt;b&gt;NORPERM, the Norwegian Permafrost Database – a TSP NORWAY IPY legacy&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 27-54, 2010&lt;br /&gt;&lt;br /&gt;Author(s): H. Juliussen, H. H. Christiansen, G. S. Strand, S. Iversen, K. Midttømme, and J. S. Rønning&lt;br /&gt;&lt;br /&gt;NORPERM – The Norwegian Permafrost Database was developed at the Geological
Survey of Norway during the International Polar Year (IPY) 2007–2009 as the
main data legacy of the IPY research project &lt;i&gt;Permafrost Observatory Project: A Contribution to the Thermal State of Permafrost in Norway and Svalbard&lt;/i&gt; (TSP NORWAY). This paper
describes the structural and technical design of NORPERM. NORPERM follows
the IPY data policy of open, free, full and timely release of IPY data, and
the borehole metadata description follows the Global Terrestrial Network for
Permafrost (GTN-P) standard. The ground temperature data infrastructure in
Norway and Svalbard is also presented, focussing on the TSP NORWAY
permafrost observatory installations in the &lt;i&gt;North Scandinavian Permafrost Observatory&lt;/i&gt; and &lt;i&gt;Nordenskiöld Land Permafrost Observatory&lt;/i&gt;, as the data providers for
NORPERM. Further developments of the database, possibly towards a regional
database for the Nordic area, are also discussed.

&lt;br&gt;&lt;br&gt;
The purpose of NORPERM is to store ground temperature data safely and in a
standard format for use in future research. NORPERM stores temperature time
series from various depths in boreholes and from the air, snow cover,
ground-surface or upper ground layer recorded by miniature temperature
data-loggers, and temperature profiles with depth in boreholes obtained by
occasional manual logging. It contains all the temperature data from the TSP
NORWAY research project, totalling 32 boreholes and 98 sites with miniature
temperature data-loggers for continuous monitoring of micrometeorological
conditions, and 6 temperature depth profiles obtained by manual borehole
logging. The amount of data in the database will gradually increase as data
from older, previous projects are added. NORPERM also provides links to near
real-time permafrost temperatures obtained by GSM data transfer.</description><dc:date>2010-02-23T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/3/1/2010/"><title>CARINA TCO&lt;sub&gt;2&lt;/sub&gt; data in the Atlantic Ocean</title><link>http://www.earth-syst-sci-data-discuss.net/3/1/2010/</link><description>&lt;b&gt;CARINA TCO&lt;sub&gt;2&lt;/sub&gt; data in the Atlantic Ocean&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 3, 1-26, 2010&lt;br /&gt;&lt;br /&gt;Author(s): D. Pierrot, P. Brown, S. Van Heuven, T. Tanhua, U. Schuster, R. Wanninkhof, and R. M. Key&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon-relevant hydrographic and
hydrochemical parameters from 188 cruises in the Arctic, Atlantic and
Southern Ocean have been retrieved and merged in a new data base: the CARINA
(CARbon IN the Atlantic) Project. These data have gone through rigorous
quality control (QC) procedures to assure the highest possible quality and
consistency. Secondary quality control, which involved objective study of
data in order to quantify systematic differences in the reported values, was
performed for the pertinent parameters in the CARINA data base. Systematic
biases in the data have been corrected in the data products. The products
are three merged data files with measured, adjusted and interpolated data of
all cruises for each of the three CARINA regions (Arctic, Atlantic and
Southern Ocean). Ninety-eight cruises were conducted in the &quot;Atlantic&quot;
defined as the region south of the Greenland-Iceland-Scotland Ridge and
north of about 30&amp;deg; S. Here we report the details of the secondary QC
which was done on the total dissolved inorganic carbon (TCO&lt;sub&gt;2&lt;/sub&gt;) data and
the adjustments that were applied to yield the final data product in the
Atlantic. Procedures of quality control – including crossover analysis
between stations and inversion analysis of all crossover data – are briefly
described. Adjustments were applied to TCO&lt;sub&gt;2&lt;/sub&gt; measurements for 17 of the
cruises in the Atlantic Ocean region. With these adjustments, the CARINA
data base is consistent both internally as well as with GLODAP data, an
oceanographic data set based on the WOCE Hydrographic Program in the 1990s,
and is now suitable for accurate assessments of, for example, regional
oceanic carbon inventories, uptake rates and model validation.</description><dc:date>2010-01-11T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/579/2009/"><title>The CARINA data synthesis project: introduction and overview</title><link>http://www.earth-syst-sci-data-discuss.net/2/579/2009/</link><description>&lt;b&gt;The CARINA data synthesis project: introduction and overview&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 579-624, 2009&lt;br /&gt;&lt;br /&gt;Author(s): R. M. Key, T. Tanhua, A. Olsen, M. Hoppema, S. Jutterström, C. Schirnick, S. van Heuven, A. Kozyr, X. Lin, A. Velo, D. W. R. Wallace, and L. Mintrop&lt;br /&gt;&lt;br /&gt;The original goal of the CARINA (Carbon in Atlantic Ocean) data synthesis
project was to create a merged calibrated data set from open ocean
subsurface measurements by European scientists that would be generally
useful for biogeochemical investigations in the North Atlantic and in
particular, studies involving the carbon system. Over time the geographic
extent expanded to include the entire Atlantic, the Arctic and the Southern
Ocean and the international collaboration broadened significantly. In this
paper we give a brief history of the project, a general overview of data
included and an outline of the procedures used during the synthesis.

&lt;br&gt;&lt;br&gt;
The end result of this project was a set of 3 data products, one for each of
the listed ocean regions. It is critical that anyone who uses any of the
CARINA data products recognize that the data products are not simply
concatenations of the originally measured values. Rather, the data have been
through an extensive calibration procedure designed to remove measurement
bias and bad data. Also a significant fraction of the individual values in
the data products were derived either by direct calculation or some means of
approximation. These data products were constructed for basin scale
biogeochemical investigations and may be inappropriate for investigations
involving small areal extent or similar detailed analyses. More information
on specific parts of this project can be found in companion articles in this
issue. In particular, Tanhua et al. (2009) and Tanhua (2009) describe the
procedures and software used to remove measurement bias from the original
data.

&lt;br&gt;&lt;br&gt;
The three data products and a significant volume of supporting information
are available from the CARINA web site hosted by the Carbon Dioxide
Information Analysis Center (CDIAC: 
&lt;a href=&quot;http://cdiac.esd.ornl.gov/oceans/CARINA/Carina_inv.html&quot; target=&quot;_blank&quot;&gt;http://cdiac.esd.ornl.gov/oceans/CARINA/Carina_inv.html&lt;/a&gt;). Anyone
wanting to use the data is advised to get the highest version number of each
data product. Incremental versions represent either corrections or
additions. The web site documents specifics of the changes.</description><dc:date>2009-12-03T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/555/2009/"><title>Assessing the internal consistency of the CARINA data base in the Pacific sector of the Southern Ocean</title><link>http://www.earth-syst-sci-data-discuss.net/2/555/2009/</link><description>&lt;b&gt;Assessing the internal consistency of the CARINA data base in the Pacific sector of the Southern Ocean&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 555-578, 2009&lt;br /&gt;&lt;br /&gt;Author(s): C. L. Sabine, M. Hoppema, R. M. Key, B. Tilbrook, S. van Heuven, C. Lo Monaco, N. Metzl, M. Ishii, A. Murata, and S. Musielewicz&lt;br /&gt;&lt;br /&gt;The CARINA project is aimed at gathering and providing secondary quality
control checks on carbon and carbon-relevant hydrographic and geochemical
data from cruises all across the Atlantic, Arctic and Southern Ocean. In
total the project gathered 188 cruises that were not previously available to
the public. Of these 188 cruises, 37 are part of the Southern Ocean.
Parameters from the Southern Ocean cruises, including total carbon dioxide
(TCO&lt;sub&gt;2&lt;/sub&gt;), total alkalinity, oxygen, nitrate, phosphate and silicate, were
examined for cruise-to-cruise consistency. pH and chlorofluorocarbons (CFCs)
are also part of the data base, but are not discussed here. This paper
focuses on the quality control of the Southern Ocean data from the Pacific
sector which consisted of 29 cruises of which 17 were included in a previous
synthesis called GLODAP, 11 were new cruises from the CARINA dataset, and
one cruise was included in GLODAP but was updated with new data and
therefore also included in CARINA. The Pacific sector quality control
procedures included crossover analysis between stations and inversion
analysis of all crossover data. The GLODAP data were included into the
analysis as reference cruises but without applying the GLODAP recommended
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.</description><dc:date>2009-11-11T00:00:00+01:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/537/2009/"><title>Nordic Seas dissolved oxygen data in CARINA</title><link>http://www.earth-syst-sci-data-discuss.net/2/537/2009/</link><description>&lt;b&gt;Nordic Seas dissolved oxygen data in CARINA&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 537-553, 2009&lt;br /&gt;&lt;br /&gt;Author(s): E. Falck and A. Olsen&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon relevant hydrographic and
hydrochemical parameters from 188 previously non-publicly available cruises
in the Arctic, Atlantic, and Southern Ocean have been retrieved and merged
into a new database: CARINA (CARbon IN the Atlantic). The data have been
subject to rigorous quality control (QC) in order to ensure highest possible
quality and consistency. The data for most of the parameters included were
examined in order to quantify systematic biases in the reported values,
i.e. secondary quality control. Significant biases have been corrected for in the
data products, i.e. the three merged files with measured, calculated, and
interpolated values for each of the three CARINA regions; the Arctic
Mediterranean Seas (AMS), the Atlantic (ATL), and the Southern Ocean (SO).
With the adjustments the CARINA database is consistent both internally as
well as with GLODAP (Key et al., 2004) and is suitable for accurate
assessments of, for example, oceanic carbon inventories and uptake rates and
for model validation. The Arctic Mediterranean Seas includes the Arctic
Ocean and the Nordic Seas (Greenland, Norwegian, and Iceland Seas), and the
quality control was carried out separately in these two areas. This
contribution presents an account of the quality control of the dissolved
oxygen data from the Nordic Seas in CARINA. Out of the 35 cruises from the
Nordic Seas included in CARINA, 32 had oxygen data. The data from 4 of these
were found to be biased low and were subject to adjustment. Thus the final
CARINA data product contains oxygen data from 32 cruises from the Nordic
Seas, and these data appear consistent to &amp;plusmn;1% (corresponds to &amp;plusmn;3 μmol kg&lt;sup&gt;&amp;minus;1&lt;/sup&gt; in the deep water).</description><dc:date>2009-10-22T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/493/2009/"><title>Nordic Seas and Arctic Ocean CFC data in CARINA</title><link>http://www.earth-syst-sci-data-discuss.net/2/493/2009/</link><description>&lt;b&gt;Nordic Seas and Arctic Ocean CFC data in CARINA&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 493-536, 2009&lt;br /&gt;&lt;br /&gt;Author(s): E. Jeansson, K. A. Olsson, T. Tanhua, and J. L. Bullister&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon relevant hydrographic and
hydrochemical parameters from 188 previously non-publicly available cruises
in the Arctic, Atlantic, and Southern Ocean have been retrieved and merged
into a new database: CARINA (CARbon IN the Atlantic). The data have been
subject to rigorous quality control (QC) in order to ensure highest possible
quality and consistency. The data for most of the parameters included were
examined in order to quantify systematic biases in the reported values, i.e. secondary quality control. Significant biases have been corrected for in the
data products, i.e. the three merged files with measured, calculated and
interpolated values for each of the three CARINA regions; the Arctic
Mediterranean Seas (AMS), the Atlantic (ATL) and the Southern Ocean (SO).
The Arctic Mediterranean Seas is comprised of the Arctic Ocean and the
Nordic Seas, and the quality control was carried out separately in these two
areas.

&lt;br&gt;&lt;br&gt;
Here we present an overview of the QC of the CFC data for the Arctic
Mediterranean Seas, including the chlorofluorocarbons CFC-11, CFC-12 and
CFC-113, as well as carbon tetrachloride (CCl&lt;sub&gt;4&lt;/sub&gt;). For the secondary QC
of the CFCs we used a combination of tools, including the evaluation of
depth profiles and CFC ratios, surface saturations and a crossover analysis.
This resulted in a multiplicative adjustment of some cruise data, while some
other cruises were flagged with questionable quality, which excluded them
from the final data product.</description><dc:date>2009-10-16T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/477/2009/"><title>The Irminger Sea and the Iceland Sea time series measurements of sea water carbon and nutrient chemistry 1983–2006</title><link>http://www.earth-syst-sci-data-discuss.net/2/477/2009/</link><description>&lt;b&gt;The Irminger Sea and the Iceland Sea time series measurements of sea water carbon and nutrient chemistry 1983–2006&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 477-492, 2009&lt;br /&gt;&lt;br /&gt;Author(s): J. Olafsson, S. R. Olafsdottir, A. Benoit-Cattin, and T. Takahashi&lt;br /&gt;&lt;br /&gt;This paper describes the ways and means of assembling and quality controling
the Irminger Sea and Iceland Sea time-series biogeochemical data which are
included in the CARINA data set. The Irminger Sea and the Iceland Sea are
hydrographically different regions where measurements of sea water carbon
and nutrient chemistry were started in 1983. The sampling is seasonal, four
times a year. The carbon chemistry is studied with measurements of the
partial pressure of carbon dioxide in seawater, &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;, and total
dissolved inorganic carbon, TCO&lt;sub&gt;2&lt;/sub&gt;. The carbon chemistry data are for
surface waters only until 1994 when water column sampling was initiated.
Other measured parameters are salinity, dissolved oxygen and the inorganic
nutrients nitrate, phosphate and silicate. Because of the CARINA criteria
for secondary quality control, depth &amp;gt;1500 m, the IRM-TS could not be
included in the routine QC and the IS-TS only in a limited way. However,
with the information provided here, the quality of the data can be assessed
e.g. on the basis of the results obtained with the use of reference
materials.</description><dc:date>2009-10-16T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/421/2009/"><title>CARINA data synthesis project: pH data scale unification and cruise adjustments</title><link>http://www.earth-syst-sci-data-discuss.net/2/421/2009/</link><description>&lt;b&gt;CARINA data synthesis project: pH data scale unification and cruise adjustments&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 421-475, 2009&lt;br /&gt;&lt;br /&gt;Author(s): A. Velo, F. F. Pérez, X. Lin, R. M. Key, T. Tanhua, M. de la Paz, S. van Heuven, S. Jutterström, and A. F. Ríos&lt;br /&gt;&lt;br /&gt;Data on carbon and carbon-relevant hydrographic and hydrochemical parameters
from previously non-publicly available cruise data sets in the Artic
Mediterranean Seas (AMS), Atlantic and Southern Ocean have been retrieved
and merged to a new database: CARINA (CARbon IN the Atlantic).

&lt;br&gt;&lt;br&gt;
These data have gone through rigorous quality control (QC) procedures to
assure the highest possible quality and consistency. The data for most of
the measured parameters in the CARINA database were objectively examined in
order to quantify systematic differences in the reported values, i.e.
secondary quality control. Systematic biases found in the data have been
corrected in the data products, i.e. three merged data files with measured,
calculated and interpolated data for each of the three CARINA regions; AMS,
Atlantic and Southern Ocean. Out of a total of 188 cruise entries in the
CARINA database, 59 reported pH measured values.

&lt;br&gt;&lt;br&gt;
Here we present details of the secondary QC on pH for the CARINA database.
Procedures of quality control, including crossover analysis between cruises
and inversion analysis of all crossover data are briefly described.
Adjustments were applied to the pH values for 21 of the cruises in the
CARINA dataset. With these adjustments the CARINA database is consistent
both internally as well as with GLODAP data, an oceanographic data set based
on the World Hydrographic Program in the 1990s. Based on our analysis we
estimate the internal accuracy of the CARINA pH data to be 0.005 pH units.
The CARINA data are now suitable for accurate assessments of, for example,
oceanic carbon inventories and uptake rates and for model validation.</description><dc:date>2009-10-13T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/367/2009/"><title>Assessing the internal consistency of the CARINA database in the Indian sector of the Southern Ocean</title><link>http://www.earth-syst-sci-data-discuss.net/2/367/2009/</link><description>&lt;b&gt;Assessing the internal consistency of the CARINA database in the Indian sector of the Southern Ocean&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 367-419, 2009&lt;br /&gt;&lt;br /&gt;Author(s): C. Lo Monaco, M. Álvarez, R. M. Key, X. Lin, T. Tanhua, B. Tilbrook, D. C. E. Bakker, S. van Heuven, M. Hoppema, N. Metzl, A. F. Ríos, C. L. Sabine, and A. Velo&lt;br /&gt;&lt;br /&gt;Carbon and carbon-relevant hydrographic and hydrochemical ancillary data
from previously not publicly available cruises were retrieved and recently
merged to a new data base, CARINA. The initial North Atlantic project, an
international effort for ocean carbon synthesis, was extended to include the
Arctic Mediterranean Seas (Arctic Ocean and Nordic Seas) and all three
sectors of the Southern Ocean. From a total of 188 cruises, 37 cruises are
part of the Southern Ocean. The present work focuses on data collected in
the Indian sector (20&amp;deg; S–70&amp;deg; S; 30&amp;deg; E–150&amp;deg; E). The Southern
Indian Ocean dataset covers the period 1992–2004 and includes seasonal
repeated observations. Parameters including dissolved inorganic carbon
(TCO&lt;sub&gt;2&lt;/sub&gt;), total alkalinity (TA), oxygen, nitrate, phosphate and silicate
were examined for cruise-to-cruise and overall consistency. In addition,
data from an existing, quality controlled data base (GLODAP) were introduced
in the CARINA analysis to improve data coverage in the Southern Ocean. A
global inversion was performed to synthesize the information deduced from
objective comparisons of deep measurements (&amp;gt;1500 m) at nearby stations
(generally &amp;lt;220 m). The corrections suggested by the inversion were
allowed to vary within a fixed envelope, thus accounting for ocean interior
variability. The adjustments applied to CARINA data and those recommended
for GLODAP data, in order to obtain a consistent merged dataset, are
presented and discussed. The final outcome of this effort is a new quality
controlled data base for TCO&lt;sub&gt;2&lt;/sub&gt; and other properties of the carbon system
that can now be used to investigate the natural variability or stability of
ocean chemistry and the accumulation of anthropogenic carbon. This data
product also offers an important new synthesis of seasonal to decadal
observations to validate ocean biogeochemical models in a region where
historical data were very sparse.</description><dc:date>2009-10-09T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/331/2009/"><title>Consistency of cruise data of the CARINA database in the Atlantic sector of the Southern Ocean</title><link>http://www.earth-syst-sci-data-discuss.net/2/331/2009/</link><description>&lt;b&gt;Consistency of cruise data of the CARINA database in the Atlantic sector of the Southern Ocean&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 331-365, 2009&lt;br /&gt;&lt;br /&gt;Author(s): M. Hoppema, A. Velo, S. van Heuven, T. Tanhu, R. M. Key, X. Lin, D. C. E. Bakker, F. F. Perez, A. F. Ríos, C. Lo Monaco, C. L. Sabine, M. Álvarez, and R. G. J. Bellerby&lt;br /&gt;&lt;br /&gt;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.</description><dc:date>2009-08-27T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/309/2009/"><title>Nordic Seas total alkalinity data in CARINA</title><link>http://www.earth-syst-sci-data-discuss.net/2/309/2009/</link><description>&lt;b&gt;Nordic Seas total alkalinity data in CARINA&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 309-330, 2009&lt;br /&gt;&lt;br /&gt;Author(s): A. Olsen&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon relevant hydrographic and
hydrochemical parameters from 188 previously non-publicly available cruises
in the Arctic, Atlantic, and Southern Ocean have been retrieved and merged
into a new database: CARINA (CARbon IN the Atlantic). The data have been
subject to rigorous quality control (QC) in order to ensure highest possible
quality and consistency. The data for most of the parameters included were
examined in order to quantify systematic biases in the reported values, i.e.
secondary quality control. Significant biases have been corrected for in the
data products, i.e. the three merged files with measured, calculated and
interpolated values for each of the three CARINA regions; the Arctic
Mediterranean Seas (AMS), the Atlantic (ATL) and the Southern Ocean (SO).
With the adjustments the CARINA database is consistent both internally as
well as with GLODAP (Key et al., 2004) and is suitable for accurate
assessments of, for example, oceanic carbon inventories and uptake rates and
for model validation. The Arctic Mediterranean Seas includes the Arctic
Ocean and the Nordic Seas, and the quality control was carried out
separately in these two areas. This contribution presents an account of the
quality control of the total alkalinity (ALK) data from the Nordic Seas in
CARINA. Out of the 35 cruises from the Nordic Seas included in CARINA, 21
had ALK data. The data from 6 of these were found to be of low quality and
should not be used. Of the others, 3 were found to be biased low and were
subject to adjustment. Thus the final CARINA data product contains ALK data
from 15 cruises from the Nordic Seas, and these data appear consistent to
&amp;plusmn;3 μmol kg&lt;sup&gt;&amp;minus;1&lt;/sup&gt;.</description><dc:date>2009-08-27T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/281/2009/"><title>Arctic Ocean data in CARINA</title><link>http://www.earth-syst-sci-data-discuss.net/2/281/2009/</link><description>&lt;b&gt;Arctic Ocean data in CARINA&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 281-308, 2009&lt;br /&gt;&lt;br /&gt;Author(s): S. Jutterström, L. G. Anderson, N. R. Bates, R. Bellerby, T. Johannessen, E. P. Jones, R. M. Key, X. Lin, A. Olsen, and A. M. Omar&lt;br /&gt;&lt;br /&gt;The paper describes the steps taken for quality controlling chosen
parameters within the Arctic Ocean data included in the CARINA data set and
checking for offsets between the individual cruises. The evaluated
parameters are the inorganic carbon parameters (total dissolved inorganic
carbon, total alkalinity and pH), oxygen and nutrients: nitrate, phosphate
and silicate. More parameters can be found in the CARINA data product, but
were not subject to a secondary quality control. The main method in
determining offsets between cruises was regional multi-linear regression,
after a first rough basin-wide deep-water estimate of each parameter.
Lastly, the results of the secondary quality control are discussed as well
as suggested adjustments.</description><dc:date>2009-08-21T00:00:00+02:00</dc:date></item><item rdf:about="http://www.earth-syst-sci-data-discuss.net/2/241/2009/"><title>Atlantic Ocean CARINA data: overview and salinity adjustments</title><link>http://www.earth-syst-sci-data-discuss.net/2/241/2009/</link><description>&lt;b&gt;Atlantic Ocean CARINA data: overview and salinity adjustments&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Earth System Science Data Discussions, 2, 241-280, 2009&lt;br /&gt;&lt;br /&gt;Author(s): T. Tanhua, R. Steinfeldt, R. M. Key, P. Brown, N. Gruber, R. Wanninkhof, F. Perez, A. Körtzinger, A. Velo, U. Schuster, S. van Heuven, J. L. Bullister, I. Stendardo, M. Hoppema, A. Olsen, A. Kozyr, D. Pierrot, C. Schirnick, and D. W. R. Wallace&lt;br /&gt;&lt;br /&gt;Water column data of carbon and carbon-relevant hydrographic and
hydrochemical parameters from 188 previously non-publicly available cruise
data sets in the Arctic, Atlantic and Southern Ocean have been retrieved and
merged into a new database: CARINA (CARbon IN the Atlantic). The data have
gone through rigorous quality control procedures to assure the highest
possible quality and consistency. The data for the pertinent parameters in
the CARINA database were objectively examined in order to quantify
systematic differences in the reported values, i.e. secondary quality
control. Systematic biases found in the data have been corrected in the data
products, i.e. three merged data files with measured, calculated and
interpolated data for each of the three CARINA regions, i.e. Arctic,
Atlantic and Southern Ocean. Ninety-eight of the cruises in the CARINA
database were conducted in the Atlantic Ocean, defined here as the region
south of the Greenland-Iceland-Scotland Ridge and north of about 30&amp;deg; S.
Here we present an overview of the Atlantic Ocean synthesis of the CARINA
data and the adjustments that were applied to the data product. We also
report details of the secondary QC for salinity for this data set.
Procedures of quality control – including crossover analysis between
stations and inversion analysis of all crossover data – are briefly
described. Adjustments to salinity measurements were applied to the data
from 10 cruises in the Atlantic Ocean region. Based on our analysis we
estimate the internal accuracy of the CARINA-ATL salinity data to be 4.1 ppm.
With these adjustments the CARINA database is consistent both
internally as well as with GLODAP data, an oceanographic data set based on
the World Hydrographic Program in the 1990s (Key et al., 2004), and is now
suitable for accurate assessments of, for example, oceanic carbon
inventories and uptake rates and for model validation.</description><dc:date>2009-08-20T00:00:00+02:00</dc:date></item></rdf:RDF>