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<!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>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/os-3-43-2007</doi>
	<article_url>http://www.ocean-sci.net/3/43/2007/</article_url>
	<abstract_html>http://www.ocean-sci.net/3/43/2007/os-3-43-2007.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/3/43/2007/os-3-43-2007.pdf</fulltext_pdf>
	<start_page>43</start_page>
	<end_page>53</end_page>
	<publication_date>2007-02-06</publication_date>
	<article_title content_type="html">How does ocean ventilation change under global warming?</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Gnanadesikan</name>
			<email>anand.gnanadesikan@noaa.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. L. Russell</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>Fanrong Zeng</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Geosciences, University of Arizona, Tucson, AZ, USA</affiliation>
		<affiliation numeration="3" content_type="html">RSIS, Princeton, NJ, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Since the upper ocean takes up much of the heat added to the earth system
by anthropogenic global warming, one would expect that global warming would
lead to an increase in stratification and a decrease in the ventilation of
the ocean interior. However, multiple simulations in global coupled climate
models using an ideal age tracer which is set to zero in the mixed layer and
ages at 1 yr/yr outside this layer show that the intermediate depths in the
low latitudes, Northwest Atlantic, and parts of the Arctic Ocean
become younger under global warming. This paper reconciles these
apparently contradictory trends, showing that the decreases result from
changes in the relative contributions of old deep waters and younger surface
waters. Implications for the tropical oxygen minimum zones, which play
a critical role in global biogeochemical cycling are considered in
detail.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Altabet, M. A., Murray, D. W., and Prell, W. L.: Climatically linked oscillations in Arabian Sea denitrification over the past 1 m.y.: Implications for the marine nitrogen cycle, Paleoceanography, 14, 732&amp;ndash;743, 1999. </reference>
		<reference numeration="2" content_type="text"> Bryan, F. O., Danabasoglu, G., Gent, P. R., and Lindsay, K.: Changes in ocean ventilation during the 21st century in the CCSM3, Ocean Modelling, 15, 141&amp;ndash;156, doi:10.1016/j.ocemod.2006.01.002, 2006. </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. 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 Atlas, NESDIS 42, U.S. Government Printing Office, Washington, D.C., 167 pp, 2002. </reference>
		<reference numeration="4" content_type="text"> Delworth, T. L., Stouffer, R. J., Dixon, K. W., Spelman, M. J., Knutson, T. R., Broccoli, A. J., Kushner, P. J., and Wetherald, R. T.: Review of simulations of climate variability and change with the GFDL R30 coupled climate model, Clim. Dyn., 19(7), 555&amp;ndash;574, 2002. </reference>
		<reference numeration="5" content_type="text"> Delworth, T., Broccoli, A. J., Rosati, A., et al.: GFDL&apos;s global coupled climate models- Part 1: Equilibrium simulations, J. Climate, 18, 643&amp;ndash;674, 2006. </reference>
		<reference numeration="6" content_type="text"> Elkins, J. W., Wofsy, S. C., McElroy, M. C., Kolb, C. E., and Kaplan, W. E.: Aquatic sources and sinks for nitrous oxide, Nature, 275, 602&amp;ndash;606, 1978. </reference>
		<reference numeration="7" content_type="text"> Galbraith, E. D., Kienast, M., Pedersen, T. F., and Calvert, S. E.: Glacial-interglacial modulation of the marine nitrogen cycle by high-latitude O2 supply to the global thermocline, Paleoceanography, 19, PA4007, doi:10.1029/2003PA001000, 2004. </reference>
		<reference numeration="8" content_type="text"> Gent, P. and McWilliams, J. C.: Isopycnal mixing in ocean circulation models, J. Phys. Oceanogr., 20, 150&amp;ndash;155, 1990. </reference>
		<reference numeration="9" content_type="text"> The GFDL Global Atmospheric Model Development Team: The new GFDL global atmosphere and land model AM2-LM2: Evaluation with prescribed SST simulations, J. Climate, 17(24), 4641&amp;ndash;4673, 2004. </reference>
		<reference numeration="10" content_type="text"> Gnanadesikan, A., Dunne, J. P., Key, R. M., Matsumoto, K., Sarmiento, J. L., Slater, R. D., and Swathi, P. S.: Oceanic ventilation and biogeochemical cycling: Understanding the physical mechanisms that produce realistic distributions of tracers and productivity, Global Biogeochem. Cycles, 18, GB4010, doi:10.1029/2003GB002097, 2004. </reference>
		<reference numeration="11" content_type="text"> Gnanadesikan, A., Dixon, K. W., Griffies, S. M., et al.: GFDL&apos;s global coupled climate models- Part 2: The baseline ocean simulation, J. Climate, 18, 675&amp;ndash;697, 2006. </reference>
		<reference numeration="12" content_type="text"> Griffies, S. M., Gnanadesikan, A., Dixon, K. W., Dunne, J. P., Gerdes, R., Harrison, M. J., Rosati, A., Russell, J. L., Samuels, B. L., Spelman, M. J., Winton, M., and Zhang, R.: Formulation of an ocean model for global climate simulations, Ocean Sci., 1, 45&amp;ndash;79, 2005. </reference>
		<reference numeration="13" content_type="text"> Griffies, S. M., Harrison, M. J., Pacanowski, R. C., and Rosati, A.: A Technical Guide to MOM4. GFDL Ocean Group Technical Report No. 5, Princeton, NJ: NOAA/Geophysical Fluid Dynamics Laboratory, 2003. </reference>
		<reference numeration="14" content_type="text"> Gruber, N. and Sarmiento, J. L.: Global patterns of marine nitrogen fixation and denitrification, Global Biogeochem. Cycles, 11, 235&amp;ndash;266, 1997. </reference>
		<reference numeration="15" content_type="text"> Hirst, A. C., Gordon, H. D., and O&apos;Farrell, S. P.: Global warming in a coupled climate model including oceanic eddy-induced advection, Geophys. Res. Lett., 21, 3361&amp;ndash;3364, 1996. </reference>
		<reference numeration="16" content_type="text"> Lin, S.-J.: A &quot;vertically Lagrangian&quot; finite-volume dynamical core for global models, Mon. Wea. Rev., 132(10), 2293&amp;ndash;2307, 2004. </reference>
		<reference numeration="17" content_type="text"> Lionello, P. and Pedlosky, J.: The role of a finite density jump at the bottom of the quasi-continuous ventilated thermocline, J. Phys. Oceanogr., 30, 338&amp;ndash;351, 2000. </reference>
		<reference numeration="18" content_type="text"> Luyten, J. L., Pedlosky, J., and Stommel, H. M.: The ventilated thermocline, J. Phys. Oceanogr., 13, 292&amp;ndash;309, 1983. </reference>
		<reference numeration="19" content_type="text"> Manabe, S. and Stouffer, R. J.: Multiple-century response of a coupled ocean- atmosphere model to an increase of atmospheric carbon dioxide, J. Climate, 7, 5&amp;ndash;23, 1994. </reference>
		<reference numeration="20" content_type="text"> Pacanowski, R., Dixon, K., and Rosati, A.: The GFDL Modular Ocean Model users guide version 1, GFDL Ocean Group Tech Rep 2, pp. 44, 1991. </reference>
		<reference numeration="21" content_type="text"> Reid, J. L.: On the total geostrophic circulation of the South Pacific: Flow patterns, tracers and transports, Progress in Oceanography, 16, 1&amp;ndash;61, 1985. </reference>
		<reference numeration="22" content_type="text"> Russell, J. L. and Dickson, A. G.: Variability in oxygen and nutrients in South Pacific Antarctic Intermediate Water, Global Biogeochem. Cycles, 17(2), 1033, doi:10.1029/2000GB001317, 2003. </reference>
		<reference numeration="23" content_type="text"> Russell, J. L., Dixon, K. W., Gnanadesikan, A., Stouffer, R. J., and Toggweiler, J. R.: Southern Ocean Westerlies in a warming world: Propping open the door to the deep ocean, J. Climate, 19, 6382&amp;ndash;6390, 2006. </reference>
		<reference numeration="24" content_type="text"> Sarmiento, J. L., Hughes, T. M. C., Stouffer, R. J., and Manabe, S.: Simulated response of the ocean carbon cycle to anthropogenic climate warming, Nature, 393, 245&amp;ndash;249, 1998. </reference>
		<reference numeration="25" content_type="text"> Sarmiento, J. L., Slater, R., Barber, R., Bopp, L., Doney, S. C., Hirst, A. C., Kleypas, J., Matear, R., Mikolajewicz, U., Monfray, P., Soldatov, V., Spall, S. A., and Stouffer, R. J.: Response of ocean ecosystems to global warming, Global Biogeochem. Cycles, 18, GB3003, doi:10.1029/2003GB002134, 2004. </reference>
		<reference numeration="26" content_type="text"> Stouffer, R. J., Weaver, A. J., and Eby, M.: A method for obtaining pre-twentieth century initial conditions for use in climate change studies, Clim. Dyn., 23, 327&amp;ndash;339, 2004. </reference>
		<reference numeration="27" content_type="text"> Stouffer, R. J., Broccoli, A. J., Delworth, T. L., Dixon, K. W., Gudgel, R., Held, I., Hemler, R., Knutson, T., Lee, H.-C., Schwartzkopf, M. D., Soden, B., Spelman, M. J., Winton, M., and Zeng, F.: GFDL&apos;s CM2 Global Coupled Climate Models &amp;ndash; Part 4: Idealized Climate Response, J. Climate, 19, 723&amp;ndash;740, 2006. </reference>
		<reference numeration="28" content_type="text"> Vecchi, G. A. and Soden, B. J.: Global warming and the weakening of the tropical circulation, J. Climate, in press, 2007. </reference>
		<reference numeration="29" content_type="text"> Vecchi, G. A., Soden, B. J., Wittenberg, A. T., Held, I. M., Leetmaa, A., and Harrison, M. J.: Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing, Nature, 441(7089), 73&amp;ndash;76, 2006. </reference>
		<reference numeration="30" content_type="text"> Volk, T. and Hoffert, M. J.: Ocean carbon pumps: analysis of relative strengths and efficiencies in ocean-driven atsmopheric pCO&lt;sub&gt;2&lt;/sub&gt; change, in: The Carbon Cycle and Atmospheric CO&lt;sub&gt;2&lt;/sub&gt;: Natural variations Archean to Present, edited by: Sundquist, E. and Broecker, W. S., Geophys. Monogr. Ser., 32, 163&amp;ndash;184, 1985. </reference>
		<reference numeration="31" content_type="text"> Wallmann, K.: Feedbacks between oceanic redox states and marine productivity:A model perspective focused on benthic phosphorus cycling, Global Biogeochem. Cycles, 17, 1084, doi:10.1029GB001968, 2003. </reference>
		<reference numeration="32" content_type="text"> Washington, W. M. and Meehl, G. A.: Climate sensitivity due to increased CO&lt;sub&gt;2&lt;/sub&gt;: experiments with a coupled atmosphere and ocean general circulation model, Clim. Dyn., 4, 1&amp;ndash;38, 1989. </reference>
		<reference numeration="33" content_type="text"> Willey, D. A., Fine, R. A., Sonnerup, R. E., Bullister, J. L., Smethie, W. M., and Warner, M. J.: Global oceanic chloroflourocarbon inventory, Geophys. Res. Lett., 31, L011303, doi:10.1029/2003GL018816, 2004. </reference>
	</references>
</article>

