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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>10</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acp-10-2227-2010</doi>
	<article_url>http://www.atmos-chem-phys.net/10/2227/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/10/2227/2010/acp-10-2227-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/10/2227/2010/acp-10-2227-2010.pdf</fulltext_pdf>
	<start_page>2227</start_page>
	<end_page>2236</end_page>
	<publication_date>2010-03-03</publication_date>
	<article_title content_type="html">A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Buligon</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. A. Degrazia</name>
			<email>degrazia@ccne.ufsm.br</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>O. C. Acevedo</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>C. R. P. Szinvelski</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. G. O. Goulart</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Universidade Federal de Santa Maria, Departamento de FÃ­sica, Santa Maria, RS, Brazil</affiliation>
		<affiliation numeration="2" content_type="html">Universidade Federal do Pampa/UFSM, Centro de CiÃªncias Exatas e TecnolÃ³gicas, BagÃ©, RS, Brazil</affiliation>
		<affiliation numeration="3" content_type="html">Centro de EducaÃ§Ã£o Superior do Alto Vale do ItajaÃ­, UDESC/CEAVI, Ibirama, SC, Brazil</affiliation>
	</affiliations>
	<abstract content_type="html">A novel methodology to derive the average wind profile from the Navier-Stokes
equations is presented. The development employs the Generalized Integral
Transform Technique (GITT), which combines series expansions with Integral
Transforms. The new approach provides a solution described in terms of the
quantities that control the wind vector with height. Parameters, such as
divergence and vorticity, whose magnitudes represent sinoptic patterns are
contained in the semi-analytical solution. The results of this new method
applied to the convective boundary layer are shown to agree with wind data
measured in Wangara experiment.</abstract>
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</article>

