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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-6719-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/6719/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/6719/2007/acpd-7-6719-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/6719/2007/acpd-7-6719-2007.pdf</fulltext_pdf>
	<start_page>6719</start_page>
	<end_page>6735</end_page>
	<publication_date>2007-05-16</publication_date>
	<article_title content_type="html">First direct observation of the atmospheric CO&lt;sub&gt;2&lt;/sub&gt; year-to-year increase from space</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Buchwitz</name>
			<email>michael.buchwitz@iup.physik.uni-bremen.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>O. Schneising</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. P. Burrows</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H. Bovensmann</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. Notholt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics (IUP), University of Bremen FB1, Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The reliable prediction of future atmospheric
CO&lt;sub&gt;2&lt;/sub&gt; concentrations and associated global climate change requires an
adequate understanding of the CO&lt;sub&gt;2&lt;/sub&gt; sources and sinks.
The sparseness of the existing surface measurement network limits current
knowledge about the global distribution of CO&lt;sub&gt;2&lt;/sub&gt; surface fluxes.
The retrieval of the CO&lt;sub&gt;2&lt;/sub&gt; total vertical column from satellite observations
is predicted to improve this situation. Such an application however requires
very high accuracy and precision on the order of 1% (4 ppm) or better.
We report on retrievals of the column-averaged CO&lt;sub&gt;2&lt;/sub&gt; dry air mole fraction,
denoted XCO&lt;sub&gt;2&lt;/sub&gt;, from the measurements of the SCIAMACHY satellite instrument
between 2003 and 2005.
We focus on northern hemispheric large scale CO&lt;sub&gt;2&lt;/sub&gt; features
such as the CO&lt;sub&gt;2&lt;/sub&gt; seasonal cycle and show &amp;ndash; for the first time &amp;ndash; that the
atmospheric annual increase of CO&lt;sub&gt;2&lt;/sub&gt; can be directly observed
using satellite measurements of the CO&lt;sub&gt;2&lt;/sub&gt; total column.
The satellite retrievals are compared with the global assimilation
system CarbonTracker and with local surface CO&lt;sub&gt;2&lt;/sub&gt; measurements based on weekly
flask sampling. We show that the year-to-year CO&lt;sub&gt;2&lt;/sub&gt; increase
as determined from the satellite data agrees
with the reference data within about 1 ppm/year.
We also show that the CO&lt;sub&gt;2&lt;/sub&gt; seasonal cycle over northern hemispheric
low and mid latitudes can be retrieved with a precision of about 2 ppm.
The results presented here demonstrate that it is possible using
satellite measurements to retrieved information on the atmospheric CO&lt;sub&gt;2&lt;/sub&gt;
on the level of a few parts per million.</abstract>
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</article>

