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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>2</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amtd-2-1247-2009</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/2/1247/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/2/1247/2009/amtd-2-1247-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/2/1247/2009/amtd-2-1247-2009.pdf</fulltext_pdf>
	<start_page>1247</start_page>
	<end_page>1291</end_page>
	<publication_date>2009-05-05</publication_date>
	<article_title content_type="html">In-situ measurements of oxygen, carbon monoxide and greenhouse gases from Ochsenkopf tall tower in Germany</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. L. Thompson</name>
			<email>rthompson@bgc-jena.mpg.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. C. Manning</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>E. Gloor</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>U. Schultz</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>T. Seifert</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>F. Hänsel</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>A. Jordan</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>M. Heimann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Biogeochemistry, Jena, Germany</affiliation>
		<affiliation numeration="2" content_type="html">University of East Anglia, Norwich, UK</affiliation>
		<affiliation numeration="3" content_type="html">University of Leeds, Leeds, UK</affiliation>
	</affiliations>
	<abstract content_type="html">We present 2.5 years of in-situ measurements of CO&lt;sub&gt;2&lt;/sub&gt;, O&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;,
CO, N&lt;sub&gt;2&lt;/sub&gt;O and SF&lt;sub&gt;6&lt;/sub&gt; mixing ratios sampled from 23, 90 and 163 m above
ground on the Ochsenkopf tower in the Fichtelgebirge range, Germany
(50&amp;deg;01´49´´ N, 11&amp;deg;48´30´´ E, 1022 m a.s.l.). In addition to the in-situ
measurements, flask samples are taken at Ochsenkopf at approximately weekly
intervals and are subsequently analysed for the same species, as well as
H&lt;sub&gt;2&lt;/sub&gt;, and the stable isotopes, &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C, &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O in
CO&lt;sub&gt;2&lt;/sub&gt;. The in-situ measurements of CO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;2&lt;/sub&gt; from 23 m show
substantial diurnal variations that are modulated by biospheric fluxes,
combustion of fossil fuels, and by diurnal changes in the planetary boundary
layer height. Measurements from 163 m exhibit only very weak diurnal
variability, as this height (1185 m a.s.l.) is generally above the nocturnal
boundary layer. CH&lt;sub&gt;4&lt;/sub&gt;, CO, N&lt;sub&gt;2&lt;/sub&gt;O and SF&lt;sub&gt;6&lt;/sub&gt; show little diurnal
variation even at 23 m owing to the absence of any significant diurnal
change in the fluxes and the absence of any strong local sources or sinks.
From the in-situ record, the seasonal cycles of the gas species have been
characterized and the multi-annual trends determined. Because the record is
short, the calculation of the trend is sensitive to inter-annual variations
in the amplitudes of the seasonal cycles. However, for CH&lt;sub&gt;4&lt;/sub&gt; a
significant change in the growth-rate was detected for 2006.5–2008.5 as
compared with the global mean from 1999 to 2006 and is consistent with other
recent observations of a renewed increasing global growth rate in CH&lt;sub&gt;4&lt;/sub&gt;
since the beginning of 2007.</abstract>
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