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<article language="en">
	<journal>
		<journal_title>The Cryosphere</journal_title>
		<journal_url>www.the-cryosphere.net</journal_url>
		<issn>1994-0416</issn>
		<eissn>1994-0424</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tc-4-325-2010</doi>
	<article_url>http://www.the-cryosphere.net/4/325/2010/</article_url>
	<abstract_html>http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf</fulltext_pdf>
	<start_page>325</start_page>
	<end_page>331</end_page>
	<publication_date>2010-09-02</publication_date>
	<article_title content_type="html">Local scaling characteristics of Antarctic surface layer turbulence</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>S. Basu</name>
			<email>sukanta_basu@ncsu.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Ruiz-Columbié</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>J. A. Phillipson</name>
		</author>
		<author numeration="4" affiliations="1,4">
			<name>S. Harshan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Science Group, Department of Geosciences, Texas Tech University, Lubbock, Texas, USA</affiliation>
		<affiliation numeration="2" content_type="html">now at: Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, North Carolina, USA</affiliation>
		<affiliation numeration="3" content_type="html">now at: National Weather Service, St. Louis, Missouri, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: Centre for Atmospheric and Oceanic Sciences, Indian Institute of Science, Bengaluru, Karnataka, India</affiliation>
	</affiliations>
	<abstract content_type="html">Over the past years, several studies have validated Nieuwstadt&apos;s local
scaling hypothesis by utilizing turbulence observations from the
mid-latitude, nocturnal stable boundary layers. In this work, we probe into
the local scaling characteristics of polar, long-lived stable boundary layers
by analyzing turbulence data from the South Pole region of the antarctic
plateau.</abstract>
	<references>
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</article>

