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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>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amtd-3-3277-2010</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/3/3277/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/3/3277/2010/amtd-3-3277-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/3/3277/2010/amtd-3-3277-2010.pdf</fulltext_pdf>
	<start_page>3277</start_page>
	<end_page>3291</end_page>
	<publication_date>2010-08-04</publication_date>
	<article_title content_type="html">Possible shift of spectral response function of the MODIS 6.8 μm water vapor channel causing a cold bias up to 3 K</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. J. Sohn</name>
			<email>sohn@snu.ac.kr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>B.-R. Kim</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S.-S. Lee</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Earth and Environmental Sciences, Seoul National University,  Seoul, 151–747, Korea</affiliation>
	</affiliations>
	<abstract content_type="html">The calibration of the Moderate-resolution Imaging Spectroradiometer
      (MODIS) 6.8 μm water vapor (WV) channel was assessed by
      comparing Terra/MODIS measurements with the WV channel brightness
      temperatures equivalent to Infrared Atmospheric Sounding
      Interferometer (IASI) measurements for June 2007 and December
      2007. IASI spectral information was transferred to the Japanese
      Multifunctional Transport Satellite (MTSAT)-1R WV channel and then to
      the MODIS WV channel. Results indicate that the MODIS WV channel is
      biased low up to 3 K, likely caused by the shift of the
      spectral response function by about +11 cm&lt;sup&gt;−1&lt;/sup&gt;. This
      finding is particularly important because the bias of −3 K can
      cause about +30% relative errors in the retrieval of upper
      tropospheric humidity (UTH). In other words, the current MODIS
      measurements may result in higher UTH values, showing relative errors
      up to +30%.</abstract>
	<references>
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</article>

