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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques</journal_title>
		<journal_url>www.atmos-meas-tech.net</journal_url>
		<issn>1867-1381</issn>
		<eissn>1867-8548</eissn>
		<volume_number>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amt-3-1103-2010</doi>
	<article_url>http://www.atmos-meas-tech.net/3/1103/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech.net/3/1103/2010/amt-3-1103-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech.net/3/1103/2010/amt-3-1103-2010.pdf</fulltext_pdf>
	<start_page>1103</start_page>
	<end_page>1112</end_page>
	<publication_date>2010-08-24</publication_date>
	<article_title content_type="html">Remotely operable compact instruments for measuring atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; column densities at surface monitoring sites</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>N. Kobayashi</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. Inoue</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>M. Kawasaki</name>
			<email>kawasaki@moleng.kyoto-u.ac.jp</email>
		</author>
		<author numeration="4" affiliations="2">
			<name>H. Yoshioka</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. Minomura</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>I. Murata</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>T. Nagahama</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>Y. Matsumi</name>
		</author>
		<author numeration="9" affiliations="5">
			<name>T. Tanaka</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>I. Morino</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>T. Ibuki</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Research Institute for Humanity and Nature, Kyoto 603-8047, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Department of Molecular Engineering, Kyoto University, Kyoto 615-8510, Japan</affiliation>
		<affiliation numeration="3" content_type="html">Department of Geophysics, Tohoku University, Sendai 980-8578, Japan</affiliation>
		<affiliation numeration="4" content_type="html">Solar-Terrestrial Environment Laboratory, Nagoya University, Nagoya 464-8601, Japan</affiliation>
		<affiliation numeration="5" content_type="html">National Institute for Environmental Studies, Tsukuba, 305-8506, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">Remotely operable compact instruments for measuring atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt;
column densities were developed in two independent systems: one utilizing a
grating-based desktop optical spectrum analyzer (OSA) with a resolution enough to
resolve rotational lines of CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; in the regions of 1565–1585 and 1674–1682 nm,
respectively; the other is an application of an optical fiber Fabry-Perot interferometer
(FFPI) to obtain the CO&lt;sub&gt;2&lt;/sub&gt; column density. Direct sunlight was collimated via a small
telescope installed on a portable sun tracker and then transmitted through an optical
fiber into the OSA or the FFPI for optical analysis. The near infrared spectra of the OSA
were retrieved by a least squares spectral fitting algorithm. The CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; column
densities deduced were in excellent agreement with those measured by a Fourier
transform spectrometer with high resolution. The rovibronic lines in the wavelength
region of 1570–1575 nm were analyzed by the FFPI. The &lt;i&gt;I&lt;/i&gt;&lt;sub&gt;0&lt;/sub&gt; and &lt;i&gt;I&lt;/i&gt; values in the
Beer-Lambert law equation to obtain CO&lt;sub&gt;2&lt;/sub&gt; column density were deduced by modulating
temperature of the FFPI, which offered column CO&lt;sub&gt;2&lt;/sub&gt; with the statistical error less than
0.2% for six hours measurement.</abstract>
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</article>

