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<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>6</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/os-6-573-2010</doi>
	<article_url>http://www.ocean-sci.net/6/573/2010/</article_url>
	<abstract_html>http://www.ocean-sci.net/6/573/2010/os-6-573-2010.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/6/573/2010/os-6-573-2010.pdf</fulltext_pdf>
	<start_page>573</start_page>
	<end_page>586</end_page>
	<publication_date>2010-06-14</publication_date>
	<article_title content_type="html">Importance of the variability of hydrographic preconditioning for deep convection in the Gulf of Lion, NW Mediterranean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Grignon</name>
			<email>laure.grignon@noc.soton.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. A. Smeed</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. L. Bryden</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>K. Schroeder</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Oceanography Centre, Southampton, UK</affiliation>
		<affiliation numeration="2" content_type="html">CNR-ISMAR, Sede di La Spezia, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">We study the variability of hydrographic preconditioning defined as the heat
and salt contents in the Ligurian Sea before convection. The stratification
is found to reach a maximum in the intermediate layer in December, whose
causes and consequences for the interannual variability of convection are
investigated. Further study of the interannual variability and correlation
tests between the properties of the deep water formed and the winter surface
fluxes support the description of convection as a process that transfers the
heat and salt contents from the top and intermediate layers to the deep
layer. A proxy for the rate of transfer is given by the final convective
mixed layer depth, that is shown to depend equally on the surface fluxes and
on the preconditioning. In particular, it is found that deep convection in
winter 2004–2005 would have happened even with normal winter conditions, due to
low pre-winter stratification.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alverson, K.: Mechanisms for lateral exchange with oceanic convection sites, J. Phys. Oceanogr., 27, 1436–1446, 1997. </reference>
		<reference numeration="2" content_type="text"> Artale, V., Iudicone, D., Santoleri, R., Rupolo, V., Marullo, S., and D&apos;Ortenzio, F.: Role of surface fluxes in ocean general circulation models using satellite sea surface temperature: Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation, J. Geophys. Res.-Oceans, 107, 3120, \doi10.1029/2000JC000452, 2002. </reference>
		<reference numeration="3" content_type="text"> Astraldi, M. and Gasparini, G.: The Seasonal Characteristics of the Circulation in the North Mediterranean Basin and their Relationship with the Atmospheric-Climatic Conditions, J. Geophys. Res.-Oceans, 97, 9531–9540, 1992. </reference>
		<reference numeration="4" content_type="text"> Astraldi, M., Gasparini, G., Manzella, G., and Hopkins, T.: Temporal Variability of Currents in the Eastern Ligurian Sea, J. Geophys. Res.-Oceans, 95, 1515–1522, 1990. </reference>
		<reference numeration="5" content_type="text"> Béthoux, J P., Gentili, B., Raunet, J., and Tailliez, D.: Warming trend in the Western Mediterranean deep water, Nature, 347, 660–662, 1990. </reference>
		<reference numeration="6" content_type="text"> Béthoux, J P., Gentili, B., and Tailliez, D.: Warming and freshwater budget change in the Mediterranean since the 1940s, their possible relation to the greenhouse effect, Geophys. Res. Lett., 25, 1023–1026, 1998. </reference>
		<reference numeration="7" content_type="text"> Béthoux, J P., De~Madron, X., Nyffeler, F., and Tailliez, D.: Deep water in the Western Mediterranean: peculiar 1999 and 2000 characteristics, shelf formation hypothesis, variability since 1970 and geochemical inferences, J. Mar. Syst., 33, 117–131, \doiPII S0924-7963(02)00055-6, 2002. </reference>
		<reference numeration="8" content_type="text"> Bryden, H L. and Stommel, H M.: Limiting processes that determine basic features of the circulation in the Mediterranean Sea, Oceanologica Acta, 7, 289–296, 1984. </reference>
		<reference numeration="9" content_type="text"> Canals, M., Puig, P., de~Madron, X D., Heussner, S., Palanques, A., and Fabres, J.: Flushing submarine canyons, Nature, 444, 354–357, 2006. </reference>
		<reference numeration="10" content_type="text"> Font, J., Puig, P., Salat, J., Palanques, A., and Emelianov, M.: Sequence of hydrographic changes in NW Mediterranean deep water due to the exceptional winter of 2005, Scientia Marina, 71, 339–346, 2007. </reference>
		<reference numeration="11" content_type="text"> Gascard, J C.: Mediterranean deep water formation, baroclinic instability and oceanic eddies, Oceanologica Acta, 1, 315–330, 1978. </reference>
		<reference numeration="12" content_type="text"> Gasparini, G., Schroeder, K., and Sparnocchia, S.: Straits and Channels as key regions of an integrated marine observatory of the Mediterranean: our experience on their long-term monitoring, in: Towards an Integrated System of Mediterranean Marine Observatories., vol 34 of CIESM Workshop Monographs, pp. 75–79, CIESM, 2008. </reference>
		<reference numeration="13" content_type="text"> Grignon, L.: Causes of the interannual variability of deep convection, PhD thesis, University of Southampton, 2009. </reference>
		<reference numeration="14" content_type="text"> Herrmann, M., Somot, S., Sevault, F., and Estournel, C.: Modeling the deep convection in the northwestern Mediterranean Sea using an eddy-permitting and an eddy-resolving model: Case study of winter 1986–1987, J. Geophys. Res., 113, C04011, \doi10.1029/2006JC003991, 2008. </reference>
		<reference numeration="15" content_type="text"> Hogg, N G.: The preconditioning phase of MEDOC 1969 – II. Topographic effects, Deep-Sea Res., 20, 449–459, 1973. </reference>
		<reference numeration="16" content_type="text"> Hogg, N G. and Stommel, H M.: Hetonic explosions: The breakup and spread of warm pools as explained by baroclinic point vortices, J. Atmos. Sci., 42, 1465–1476, 1985. </reference>
		<reference numeration="17" content_type="text"> Kinder, T. and Bryden, H.: The Physical Oceanography of Sea Straits, chap. The aspiration of deep waters through Straits, pp. 295–319, The Physical Oceanography of Sea Straits, 1990. </reference>
		<reference numeration="18" content_type="text"> Krahmann, G. and Schott, F.: Longterm increases in Western Mediterranean salinities and temperatures: anthropogenic and climatic sources, Geophys. Res. Lett., 25, 4209–4212, 1998. </reference>
		<reference numeration="19" content_type="text"> Legg, S. and Marshall, J.: A heton model of the spreading phase of open-ocean deep convection, J. Phys. Oceanogr., 23, 1040–1056, 1993. </reference>
		<reference numeration="20" content_type="text"> Legg, S., McWilliams, J., and Gao, J B.: Localization of deep ocean convection by a mesoscale eddy, J. Phys. Oceanogr., 28, 944–970, 1998. </reference>
		<reference numeration="21" content_type="text"> Lopez-Jurado, J L., Gonzalez-Pola, C., and Velez-Belchi, P.: Observation of an abrupt disruption of the long-term warming trend at the Balearic Sea, Western Mediterranean Sea, in summer 2005, Geophys. Res. Lett., 32, L24606, \doi10.1029/2005GL024430, 2005. </reference>
		<reference numeration="22" content_type="text"> Madec, G., Lott, F., Delecluse, P., and Crépon, M.: Large-scale preconditioning of deep-water formation in the Northwestern Mediterranean Sea, J. Phys. Oceanogr., 26, 1393–1408, 1996. </reference>
		<reference numeration="23" content_type="text"> Marshall, J. and Schott, F.: Open-ocean convection: Observations, theory, and models, Rev. Geophys., 37, 1–64, 1999. </reference>
		<reference numeration="24" content_type="text"> Marshall, J., Dobson, F., Moore, K., Rhines, P., Visbeck, M., d&apos;Asaro, E., Bumke, K., Chang, S., Davis, R., Fischer, K., Garwood, R., Guest, P., Harcourt, R., Herbaut, C., Holt, T., Lazier, J., Legg, S., McWilliams, J., Pickart, R., Prater, M., Renfrew, I., Schott, F., Send, U., and Smethie, W.: The Labrador Sea deep convection experiment, B. Am. Meteorol. Soc., 79, 2033–2058, 1998. </reference>
		<reference numeration="25" content_type="text"> Marty, J. C. and Chiavérini, J.: Hydrological changes in the Ligurian Sea (NW Mediterranean, DYFAMED site) during 1995–2007 and biogeochemical consequences, Biogeosciences Discuss., 7, 1377–1406, doi:10.5194/bgd-7-1377-2010, 2010. </reference>
		<reference numeration="26" content_type="text"> Marty, J., Chiaverini, J., Pizay, M., and Avril, B.: Seasonal and interrannual dynamics of nutrients and phytoplankton pigments in the wester Mediterranean Sea at the DYFAMED time-series station (1991–1999), Deep-Sea Res. II, 49, 1965–1985, 2002. </reference>
		<reference numeration="27" content_type="text"> MEDOC-Group: Observation of formation of deep water in the Mediterranean Sea, 1969, Nature, 227, 1037–1040, 1970. </reference>
		<reference numeration="28" content_type="text"> Merckelbach, L., Smeed, D., and Griffiths, G.: Vertical Water Velocities from Underwater Gliders, J. Atmos. Oceanic Technol., 27, 547–563, \doi10.1175/2009JTECHO710.1, 2010. </reference>
		<reference numeration="29" content_type="text"> Mertens, C. and Schott, F.: Interannual variability of deep-water formation in the Northwestern Mediterranean, J. Phys. Oceanogr., 28, 1410–1424, 1998. </reference>
		<reference numeration="30" content_type="text"> Millot, C.: Interannual salinification of the Mediterranean inflow, Geophys. Res. Lett., 34, L21609, \doi10.1029/2007GL031179, 2007. </reference>
		<reference numeration="31" content_type="text"> Painter, S. and Tsimplis, M.: Temperature and salinity trends in the upper waters of the Mediterranean Sea as determined from the MEDATLAS dataset, Cont. Shelf Res., 23, 1507–1522, \doi10.1016/j.csr.2003.08.008, 2003. </reference>
		<reference numeration="32" content_type="text"> Rohling, E. and Bryden, H.: Man-induced salinity and temperature increases in Western Mediterranean Deep-Water, J. Geophys. Res.-Oceans, 97, 11191–11198, 1992. </reference>
		<reference numeration="33" content_type="text"> Schott, F. and Leaman, K D.: Observations with moored Acoustic Doppler Current Profilers in the convection regime in the Golfe Du Lion, J. Phys. Oceanogr., 21, 558–574, 1991. </reference>
		<reference numeration="34" content_type="text"> Schott, F, F., Visbeck, M, M., and Fischer, J.: Observations of vertical currents and convection in the central Greenland Sea during the winter of 1988–1989, J. Geophys. Res.-Oceans, 98, 14401–14421, 1993. </reference>
		<reference numeration="35" content_type="text"> Schroeder, K., Gasparini, G., Tangherlini, M., and Astraldi, M.: Deep and intermediate water in the Western Mediterranean under the influence of the Eastern Mediterranean Transient, Geophys. Res. Lett., 33, L21607, \doi10.1029/2006GL027121, 2006. </reference>
		<reference numeration="36" content_type="text"> Schroeder, K., Ribotti, A., Borghini, M., Sorgente, R., Perilli, A., and Gasparini, G.: An extensive Western Mediterranean Deep Water Renewal between 2004 and 2006, Geophys. Res. Lett., 35, L18605, \doi10.1029/2008GL03514, 2008. </reference>
		<reference numeration="37" content_type="text"> Schroeder, K., Josey, S., Herrmann, M., Grignon, L., Gasparini, G., and Bryden, H.: Abrupt warming and salting of the Western Mediterranean Deep Waterafter 2005: atmospheric forcing and lateral advection., J. Geophys. Res., \doi10.1029/2009JC005850, in press, 2010. </reference>
		<reference numeration="38" content_type="text"> Send, U. and Marshall, J.: Integral effects of deep convection, J. Phys. Oceanogr., 25, 855–872, 1995. </reference>
		<reference numeration="39" content_type="text"> Smith, R. O., Bryden, H. L., and Stansfield, K.: Observations of new western Mediterranean deep water formation using Argo floats 2004–2006, Ocean Sci., 4, 133–149, doi:10.5194/os-4-133-2008, 2008.  </reference>
		<reference numeration="40" content_type="text"> Stommel, H., Bryden, H., and Mangelsdorf, P.: Does some of Mediterranean outflow come from great depth?, Pure Appl. Geophys., 105, 879–889, 1973. </reference>
		<reference numeration="41" content_type="text"> Testor, P. and Gascard, J C.: Post-convection spreading phase in the Northwestern Mediterranean Sea, Deep-Sea Res. Part I-Oceanographic Research Papers, 53, 869–893, \doi10.1016/j.dsr.2006.02.004, 2006. </reference>
		<reference numeration="42" content_type="text"> Vignudelli, S., Gasparini, G., Astraldi, M., and Schiano, M.: A possible influence of the North Atlantic Oscillation on the circulation of the Western Mediterranean Sea, Geophys. Res. Lett., 26, 623–626, 1999. </reference>
		<reference numeration="43" content_type="text"> Voorhis, A D. and Webb, D C.: Vertical currents in a winter sinking region, Transactions-American Geophysical Union, 51, 315, 1970. </reference>
	</references>
</article>

