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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>8</volume_number>
		<issue_number>10</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-2643-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/2643/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/2643/2008/acp-8-2643-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/2643/2008/acp-8-2643-2008.pdf</fulltext_pdf>
	<start_page>2643</start_page>
	<end_page>2655</end_page>
	<publication_date>2008-05-20</publication_date>
	<article_title content_type="html">Variability of subtropical upper tropospheric humidity</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-M. Ryoo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. W. Waugh</name>
			<email>waugh@jhu.edu</email>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Gettelman</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, MD, USA</affiliation>
		<affiliation numeration="2" content_type="html">National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Analysis of Atmospheric Infrared Sounder (AIRS) measurements for
  five years shows significant longitudinal variations in the winter
  subtropical upper tropospheric relative humidity (RH), not only in
  the climatological mean values but also in the local distributions
  and temporal variability. The largest climatological mean values
  occur over the central-eastern Pacific and Atlantic oceans, where
  there is also large day-to-day variability. In contrast, there are
  smaller mean values, and smaller variability that occurs at lower
  frequency, over the Indian and western Pacific oceans. These
  differences in the distribution and variability of subtropical RH
  are related to differences in the key transport processes in the
  different sectors. The large variability and intermittent high and
  low RH over the central-eastern Pacific and Atlantic oceans are due
  to intrusions of high potential vorticity air into the
  subtropics. Intrusions seldom occur over the eastern Indian and
  western Pacific oceans, and here the subtropical RH is more closely
  linked to the location and strength of subtropical
  anticyclones. During northern winter there are eastward propagating
  features in the subtropical RH in this region that are out of phase
  with the tropical RH, and are caused by modulation of the
  subtropical anticyclones by the Madden-Julian Oscillation.</abstract>
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