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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>10</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-1983-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/1983/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/1983/2010/acpd-10-1983-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/1983/2010/acpd-10-1983-2010.pdf</fulltext_pdf>
	<start_page>1983</start_page>
	<end_page>2003</end_page>
	<publication_date>2010-01-29</publication_date>
	<article_title content_type="html">Estimating the maritime component of aerosol optical depth and its dependency on surface wind speed using MODIS and QuikSCAT data</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>Y. Lehahn</name>
			<email>yoav.lehahn@weizmann.ac.il</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>I. Koren</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>E. Boss</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>Y. Ben-Ami</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>O. Altaratz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geophysics and Planetary Sciences, Tel Aviv University, Tel Aviv, Israel</affiliation>
		<affiliation numeration="2" content_type="html">Department of Environmental Sciences, Weizmann Institue, Rehovot, Israel</affiliation>
		<affiliation numeration="3" content_type="html">School of Marine Sciences, University of Maine, Orono, Maine, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Seven years (2002–2008) of satellite measurements from
      SeaWinds aboard Quick Scatterometer (QuikSCAT) and Moderate
      Resolution Imaging Spectroradiometer (MODIS) aboard Terra are
      used for providing a global view on the link between surface
      wind speed and marine aerosol optical depth. This study shows
      that away form the continents the correlation time between the
      surface winds and the marine aerosol exceeds 4 h and
      therefore the two measurements can be linked. A systematic
      comparison between the satellite derived fields at different
      locations over the World Ocean allows to: (i) separate the
      relative contribution of wind-induced marine aerosol to the
      aerosol optical depth (ii) identify a threshold wind speed for
      triggering maritime contribution to aerosol optical depth; and
      (iii) extract an empirical linear equation linking marine
      aerosol optical depth and wind intensity. Wind induced marine
      aerosol contribution to aerosol optical depth is found to be
      dominated by the coarse mode elements. The threshold wind
      speed for triggering emission of coarse maritime aerosol is
      remarkably consistent with an average value of 4.1&amp;plusmn;0.1 m/s.
      When wind intensity exceeds the threshold value,
      coarse mode marine aerosol optical depth is linearly
      correlated to the surface wind speed, with a consistent slope
      of 0.0082&amp;plusmn;0.0004 s/m. The background aerosol optical
      depth, associated with aerosols that are not produced in-situ
      through wind driven processes, shows relatively large seasonal
      and geographical variability, and can be used for estimating
      the contribution of terrestrial aerosols to the aerosol
      optical depth over the ocean.</abstract>
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</article>

