<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.ocean-sci.net/inc/os/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/os-3-363-2007</doi>
	<article_url>http://www.ocean-sci.net/3/363/2007/</article_url>
	<abstract_html>http://www.ocean-sci.net/3/363/2007/os-3-363-2007.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/3/363/2007/os-3-363-2007.pdf</fulltext_pdf>
	<start_page>363</start_page>
	<end_page>377</end_page>
	<publication_date>2007-08-03</publication_date>
	<article_title content_type="html">Variability of Antarctic intermediate Water properties in the South Pacific Ocean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Tomczak</name>
			<email>matthias.tomczak@flinders.edu.au</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Chemistry, Physics and Earth Sciences, Flinders University, GPO Box 2100, Adelaide SA 5001, Australia</affiliation>
	</affiliations>
	<abstract content_type="html">Argo float time series data are used to study the salinity
field at the depth of the salinity minimum produced by Antarctic
Intermediate Water (AAIW). It is found that far from showing the smooth
erosion of the minimum that would result from diffusive flow, the salinity
field is characterized by features of geostrophic turbulence such as fronts,
eddies and intrusions. Comparison of the Argo float observations with the
climatology of the World Ocean Atlas (WOA) reveals significant differences
between the two data sets. Some of the differences may have their origin in
problems with the WOA data density in remote regions of the South Pacific,
but most are more likely produced by interannual variations of the AAIW
salinity field.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Armi, L. and Zenk, W.: Large lenses of highly saline Mediterranean water. J. Phys. Oceanogr., 14, 1560&amp;ndash;1576, 1984. </reference>
		<reference numeration="2" content_type="text"> Conkright, M. E., Locarnini, R. A., Garcia, H. E., O&apos;Brien, T. D., Boyer, T. P., Stephens, C., and Antonov, J. I.: World Ocean Atlas 2001: Objective Analyses, Data Statistics, and Figures, CD-ROM Documentation, National Oceanographic Data Center, Silver Spring, MD, 17 pp., 2001. </reference>
		<reference numeration="3" content_type="text"> Conkright, M. E., Antonov, J. I., Baranova, O., Boyer, T. P., Garcia, H. E., Gelfeld, R., Johnson, D., Locarnini, R. A., Murphy, P. P., O&apos;Brien, T. D., Smolyar, I., and Stephens, C.: World Ocean Database 2001, Volume 1: Introduction, edited by: Levitus, S., NOAA AtlasNESDIS 42, U.S. Government Printing Office, Washington, D.C., 167 pp., 2002. </reference>
		<reference numeration="4" content_type="text"> Elliott, B. A. and Sanford, T. B.: The subthermocline lens D1. Part I: Description of water properties and velocity profiles, J. Phys. Oceanogr., 16, 532&amp;ndash;548, 1986a. </reference>
		<reference numeration="5" content_type="text"> Ichikawa, Y., Takatsuki, Y., Mizuno, K., Shikama, N., and Takeuchi, K.: Estimation of drifting velocity and error at parking depth for Argo float, JAMSTECR, 44, 81&amp;ndash;89 (in Japanese), 2001. </reference>
		<reference numeration="6" content_type="text"> McWilliams, J. C.: Submesoscale, coherent vortices in the ocean, Rev. Geophys., 23, 165&amp;ndash;182, 1985. </reference>
		<reference numeration="7" content_type="text"> Oka, E.: Long-term sensor drift found in recovered Argo profiling floats, J. Oceanogr., 61, 775&amp;ndash;781, 2005. </reference>
		<reference numeration="8" content_type="text"> Prater, M. D. and Sanford, T. B.: A meddy off Cape St. Vincent. Part I: Description, J. Phys. Oceanogr., 24, 1572&amp;ndash;1586, 1994. </reference>
		<reference numeration="9" content_type="text"> Roemmich, D., Riser, S., Davis, R., and Desaubies, Y.: Autonomous profiling floats: Workhorse for broadscale ocean observations, Mar. Techn. Soc. J., 38(1), 31&amp;ndash;39, 2004. </reference>
		<reference numeration="10" content_type="text"> Stanton, B. R.: Antarctic Intermediate Water variability in the northern New Zealand region, New Zealand J. Mar. Freshwater Res., 36, 645&amp;ndash;654, 2002. </reference>
		<reference numeration="11" content_type="text"> Tomczak, M. and Andrew, C.: Eddy formation in the Antarctic Intermediate Water of the subtropical South Pacific Ocean, J. Mar. Atmos. Res., 1, 8&amp;ndash;12, 1997. </reference>
		<reference numeration="12" content_type="text"> Tomczak, M. and Godfrey, J. S.: Regional Oceanography: an Introduction 2nd edn., Daya Publishing, Delhi, xi~+~390~pp., 2003. </reference>
		<reference numeration="13" content_type="text"> Wong, A. P. S., Bindoff, N. L., and Church, J. A.: Large-scale freshening of the intermediate waters in the Pacific and Indian Oceans, Nature, 400, 440&amp;ndash;443, 1999. </reference>
		<reference numeration="14" content_type="text"> Wüst, G.: Schichtung und Zirkulation des Atlantischen Ozeans. Das Bodenwasser und die Stratosphäre, Wiss. Ergebn. Dt. Atl. Exp. &quot;METEOR&quot; 1925&amp;ndash;1927, Berlin, 6, 1&amp;ndash;288 (translated as &quot;The stratosphere of the Atlantic Ocean&quot; by Emery, W. J. (1978)), Amerind, 1936. </reference>
	</references>
</article>

