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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>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2001</publication_year>
	</journal>
	<doi>10.5194/acpd-1-167-2001</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/1/167/2001/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/1/167/2001/acpd-1-167-2001.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/1/167/2001/acpd-1-167-2001.pdf</fulltext_pdf>
	<start_page>167</start_page>
	<end_page>192</end_page>
	<publication_date>2001-09-03</publication_date>
	<article_title content_type="html">Nitrous oxide emissions from the Arabian Sea: A synthesis</article_title>
	<authors>
		<author numeration="1" affiliations="1,7">
			<name>H. W. Bange</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. O. Andreae</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>S. Lal</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>C. S. Law</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>S. W. A. Naqvi</name>
		</author>
		<author numeration="6" affiliations="2,8">
			<name>P. K. Patra</name>
		</author>
		<author numeration="7" affiliations="5,9">
			<name>T. Rixen</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>R. C. Upstill-Goddard</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Physical Research Laboratory, Ahmedabad, India</affiliation>
		<affiliation numeration="3" content_type="html">Plymouth Marine Laboratory, Plymouth, United Kingdom</affiliation>
		<affiliation numeration="4" content_type="html">National Institute of Oceanography, Dona Paula, Goa, India</affiliation>
		<affiliation numeration="5" content_type="html">University of Hamburg, Hamburg, Germany</affiliation>
		<affiliation numeration="6" content_type="html">University of Newcastle, Newcastle upon Tyne, United Kingdom</affiliation>
		<affiliation numeration="7" content_type="html">now at Institute for Marine Research, Kiel, Germany</affiliation>
		<affiliation numeration="8" content_type="html">now at Frontier Research System for Global Change, Yokohama, Japan</affiliation>
		<affiliation numeration="9" content_type="html">now at Center for Tropical Marine Ecology, Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">We computed high-resolution (1&lt;sup&gt;o&lt;/sup&gt; latitude &amp;times; 1&lt;sup&gt;o&lt;/sup&gt; longitude) seasonal and annual nitrous
oxide (N&lt;sub&gt;2&lt;/sub&gt;O) concentration fields for the Arabian Sea surface layer using a database
containing more than 2400 values measured between December 1977 and July 1997.
N&lt;sub&gt;2&lt;/sub&gt;O concentrations are highest during the southwest (SW) monsoon along the southern Indian continental shelf. Annual emissions range from 0.33 to 0.70 Tg N&lt;sub&gt;2&lt;/sub&gt;O and
are dominated by fluxes from coastal regions during the SW and northeast monsoons.
However, the tendency to focus on measurements in locally restricted features in combination
with insufficient seasonal data coverage leads to considerable uncertainties of
the concentration fields and thus in the flux estimates, especially in the coastal zones
of the northern and eastern Arabian Sea.</abstract>
	<references>
	</references>
</article>

