<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>17</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/npg-17-123-2010</doi>
	<article_url>http://www.nonlin-processes-geophys.net/17/123/2010/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/17/123/2010/npg-17-123-2010.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/17/123/2010/npg-17-123-2010.pdf</fulltext_pdf>
	<start_page>123</start_page>
	<end_page>135</end_page>
	<publication_date>2010-03-22</publication_date>
	<article_title content_type="html">A delay differential model of ENSO variability – Part 2: Phase locking, multiple solutions and dynamics of extrema</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. Zaliapin</name>
			<email>zal@unr.edu</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>M. Ghil</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Mathematics and Statistics, University of  Nevada, Reno, Nevada, USA</affiliation>
		<affiliation numeration="2" content_type="html">Geosciences Department and  Laboratoire de Météorologie Dynamique (CNRS and IPSL), Ecole Normale Supérieure, Paris, France</affiliation>
		<affiliation numeration="3" content_type="html">Department  of Atmospheric &amp; Oceanic Sciences and Institute of Geophysics &amp;  Planetary Physics, University of California, Los Angeles, California, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We consider a highly idealized model for El Niño/Southern
Oscillation (ENSO) variability, as introduced in an earlier paper.
The model is governed by a delay differential equation for
sea-surface temperature &lt;i&gt;T&lt;/i&gt; in the Tropical Pacific, and it combines
two key mechanisms that participate in ENSO dynamics: delayed
negative feedback and seasonal forcing. We perform a theoretical and
numerical study of the model in the three-dimensional space of its
physically relevant parameters: propagation period τ of oceanic
waves across the Tropical Pacific, atmosphere-ocean coupling
κ, and strength of seasonal forcing &lt;i&gt;b&lt;/i&gt;. Phase locking of
model solutions to the periodic forcing is prevalent: the local
maxima and minima of the solutions tend to occur at the same
position within the seasonal cycle. Such phase locking is a key
feature of the observed El Niño (warm) and La Niña (cold)
events. The phasing of the extrema within the seasonal cycle depends
sensitively on model parameters when forcing is weak. We also study
co-existence of multiple solutions for fixed model parameters and
describe the basins of attraction of the stable solutions in a
one-dimensional space of constant initial model histories.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Battisti, D. S.: The dynamics and thermodynamics of a warming event in a coupled tropical atmosphere/ocean model, J. Atmos. Sci., 45, 2889–2919, 1988. </reference>
		<reference numeration="2" content_type="text"> Battisti, D. S. and Hirst, A. C.: Interannual variability in the tropical atmosphere-ocean system: Influence of the basic state and ocean geometry, J. Atmos. Sci., 46, 1687–1712, 1989. </reference>
		<reference numeration="3" content_type="text"> Bjerknes, J.: Atmospheric teleconnections from the equatorial Pacific, Mon. Weather Rev., 97, 163–172, 1969. </reference>
		<reference numeration="4" content_type="text"> Boulanger, J. P., Menkes, C., and Lengaigne, M.: Role of high- and low-frequency winds and wave reflection in the onset, growth and termination of the 1997–1998 El Nino, Clim. Dynam., 22(2–3), 267–280, 2004. </reference>
		<reference numeration="5" content_type="text"> Burgers, G. and Stephenson, D. B.: The &quot;normality&quot; of El Niño, Geophys. Res. Lett., 26, 1027–1030, 1999. </reference>
		<reference numeration="6" content_type="text"> Cane, M.: The evolution of El Niño, past and future, Earth Planet. Sc. Lett., 230(3–4), 227–240, 2005. </reference>
		<reference numeration="7" content_type="text"> Cane, M., Munnich, M., and Zebiak, S. E.: A study of self-excited oscillations of the tropical ocean-atmosphere system. Part I: Linear analysis, J. Atmos. Sci., 47(13), 1562–1577, 1990. </reference>
		<reference numeration="8" content_type="text"> Chang, P., Wang, B., Li, T., and Ji, L.: Interactions between the seasonal cycle and the Southern Oscillation: Frequency entrainment and chaos in intermediate coupled ocean-atmosphere model, Geophys. Res. Lett., 21, 2817–2820, 1994. </reference>
		<reference numeration="9" content_type="text"> Chang, P., Ji, L., Wang, B., and Li, T.: Interactions between the seasonal cycle and El Niño – Southern Oscillation in an intermediate coupled ocean-atmosphere model, J. Atmos. Sci., 52, 2353–2372, 1995. </reference>
		<reference numeration="10" content_type="text"> Diaz, H. F. and Markgraf, V. (Eds.): El Niño: Historical and Paleoclimatic Aspects of the Southern Oscillation, Cambridge Univ. Press, New York, 1993. </reference>
		<reference numeration="11" content_type="text"> Delcroix, T., Eldin, G., McPhaden, M., and Morlière, A.: Effects of westerly wind bursts upon the western equatorial Pacific Ocean, February–April 1991, J. Geophys. Res., 98(C9), 16379–16385, 1993. </reference>
		<reference numeration="12" content_type="text"> Dijkstra, H. A.: Nonlinear Physical Oceanography: A Dynamical Systems Approach to the Large Scale Ocean Circulation and El Niño, 2nd edn., Springer-Verlag, 2005. </reference>
		<reference numeration="13" content_type="text"> Dijkstra, H. A. and Ghil, M.: Low-frequency variability of the ocean circulation: a dynamical systems approach, Rev. Geophys., 43, RG3002, doi:10.1029/2002RG000122, 2005. </reference>
		<reference numeration="14" content_type="text"> Feigenbaum, M. J.: Quantitative universality for a class of non-linear transformations, J. Stat. Phys., 19, 25–52, 1978. </reference>
		<reference numeration="15" content_type="text"> Gebbie, G., Eisenman, I., Wittenberg, A., and Tziperman, E.: Modulation of westerly wind bursts by sea surface temperature: A semistochastic feedback for ENSO, J. Atmos. Sci., 64, 3281–3295, 2007. </reference>
		<reference numeration="16" content_type="text"> Ghil, M. and Jiang, N.: Recent forecast skill for the El Niño/Southern Oscillation, Geophys. Res. Lett., 25, 171–174, 1998. </reference>
		<reference numeration="17" content_type="text">Ghil+02 Ghil, M., Allen, M. R., Dettinger, M. D., Ide, K., Kondrashov, D., Mann, M. E., Robertson, A. W., Saunders, A., Tian, Y., Varadi, F., and Yiou, P: Advanced spectral methods for climatic time series, Rev. Geophys., 40(1), 1003, doi:10.1029/2000RG000092, 2002. </reference>
		<reference numeration="18" content_type="text"> Ghil, M. and Robertson, A. W.: Solving problems with GCMs: General circulation models and their role in the climate modelling hierarchy, in: General Circulation Model Development: Past, Present and Future, edited by: Randall, D., Academic Press, San Diego, 285–325, 2000. </reference>
		<reference numeration="19" content_type="text"> Ghil, M., Zaliapin, I., and Coluzzi, B.: Boolean delay equations: A simple way of looking at complex systems, Physica D, 237, 2967–2986, doi: 10.1016/j.physd.2008.07.006, 2008a. </reference>
		<reference numeration="20" content_type="text"> Ghil, M., Zaliapin, I., and Thompson, S.: A delay differential model of ENSO variability: parametric instability and the distribution of extremes, Nonlin. Processes Geophys., 15, 417–433, 2008b. </reference>
		<reference numeration="21" content_type="text"> Ghil, M., Chekroun, M. D., and Simonnet, E.: Climate dynamics and fluid mechanics: Natural variability and related uncertainties, Physica D, 237, 2111–2126, 2008c. </reference>
		<reference numeration="22" content_type="text"> Glantz, M. H., Katz, R. W., and Nicholls, N. (Eds.): Teleconnections Linking Worldwide Climate Anomalies, Cambridge Univ. Press, New York, 545~pp., 1991. </reference>
		<reference numeration="23" content_type="text"> Grebogi, C., Ott, E., and Yorke, J A.: Chaos, strange attractors, and fractal basin boundaries in nonlinear dynamics, Science, 238(4827), 632–638, 1987. </reference>
		<reference numeration="24" content_type="text"> Hale, J K.: Theory of Functional Differential Equations, Springer-Verlag, New-York, 1977. </reference>
		<reference numeration="25" content_type="text"> Hale, J K. and Verduyn Lunel, S.: Introduction to Functional Differential Equations, Springer-Verlag, New York, 1993. </reference>
		<reference numeration="26" content_type="text"> Harrison, D. E. and Giese, B.: Remote westerly wind forcing of the eastern equatorial Pacific; some model results, Geophys. Res. Lett., 15, 804–807, 1988. </reference>
		<reference numeration="27" content_type="text"> Hoerling, M. P., Kumar, A., and Zhong, M.: El Niño, La Niña, and the nonlinearity of their teleconnections, J. Climate, 10, 1769–1786, 1997. </reference>
		<reference numeration="28" content_type="text"> Hurrell, J. W. and K. E. Trenberth: Global sea surface temperature analyses: Multiple problems and their implications for climate analysis, modelling, and reanalysis, B. Am. Meteorol. Soc., 80, 2661–2678, 1999. </reference>
		<reference numeration="29" content_type="text"> Jiang, N., Neelin, J. D., and Ghil, M.: Quasi-quadrennial and quasi-biennial variability in the equatorial Pacific, Clim. Dynam., 12, 101–112, 1995. </reference>
		<reference numeration="30" content_type="text"> Jin, F.-F., Neelin, J. D., and Ghil, M.: El Niño on the Devil&apos;s Staircase: Annual subharmonic steps to chaos, Science, 264, 70–72, 1994. </reference>
		<reference numeration="31" content_type="text"> Jin, F.-F., Neelin, J. D., and Ghil, M.: El Niño/Southern Oscillation and the annual cycle: Subharmonic frequency locking and aperiodicity, Physica D, 98, 442–465, 1996. </reference>
		<reference numeration="32" content_type="text"> Kadanoff, L P.: Roads to chaos, Phys. Today, 12, 46–53, 1983. \bibitem[Kondrashov et al.(2005)] KKGR05 Kondrashov, D., Kravtsov, S., Robertson, A W., and Ghil, M.: A hierarchy of data-based ENSO models, J. Climate, 18, 4425–4444, 2005. </reference>
		<reference numeration="33" content_type="text"> Latif, M., Barnett, T. P., Flügel, M., Graham, N. E., Xu, J.-S., and Zebiak, S. E.: A review of ENSO prediction studies, Clim. Dynam., 9, 167–179, 1994. </reference>
		<reference numeration="34" content_type="text"> Lengaigne, M., Guilyardi, E., Boulanger, J. P., et al.: Triggering of El Nino by westerly wind events in a coupled general circulation model, Clim. Dynam., 23(6), 601–620, 2004. </reference>
		<reference numeration="35" content_type="text"> Madden, R. A. and Julian, P. R.: Description of a 40–50 day oscillation in the zonal wind in the tropical Pacific, J. Atmos. Sci., 28, 702–708, 1971. </reference>
		<reference numeration="36" content_type="text"> Madden, R. A. and Julian, P. R.: Description of global-scale circulation cells in the tropics with a 40–50 day period, J. Atmos. Sci., 29, 1109-,1123, 1972. </reference>
		<reference numeration="37" content_type="text"> Madden, R. A. and Julian, P. R.: Observations of the 40–50-day tropical oscillation – A review, Mon. Weather Rev., 122(5), 814–37, 1994. </reference>
		<reference numeration="38" content_type="text"> McPhaden, M J., Busalacchi, A J ., Cheney, R., Donguy, J R., Gage, K S., Halpern, D., Ji, M., Julian, P., Meyers, G., Mitchum, G T., Niiler, P P., Picaut, J., Reynolds, R W., Smith, N., and Takeuchi, K.: The Tropical Ocean-Global Atmosphere observing system: A decade of progress, J. Geophys. Res., 103(C7), 14169–14240, 1998. </reference>
		<reference numeration="39" content_type="text"> Munnich, M., Cane, M., and Zebiak, S. E.: A study of self-excited oscillations of the tropical ocean-atmosphere system. Part II: Nonlinear cases, J. Atmos. Sci., 48(10), 1238–1248, 1991. </reference>
		<reference numeration="40" content_type="text"> Neelin, J. D., Latif, M., and Jin, F.-F.: Dynamics of coupled ocean-atmosphere models: the tropical problem, Annu. Rev. Fluid Mech., 26, 617–659, 1994. </reference>
		<reference numeration="41" content_type="text"> Neelin, J. D., Battisti, D. S., Hirst, A. C., Jin, F.-F., Wakata, Y., Yamagata, T., and Zebiak, S.: ENSO Theory, J. Geophys. Res., 103(C7), 14261–14290, 1998. </reference>
		<reference numeration="42" content_type="text"> Nussbaum, R. D.: Functional Differential Equations, available at: http://citeseer.ist.psu.edu/437755.html, 1998. </reference>
		<reference numeration="43" content_type="text"> Philander, S. G. H.: El Niño, La Niña, and the Southern Oscillation, Academic Press, San Diego, 1990. </reference>
		<reference numeration="44" content_type="text"> Reynolds, R. W. and Smith, T. M.: Improved global sea surface temperature analyses using optimum interpolation, J. Climate, 7, 929–948, 1994. </reference>
		<reference numeration="45" content_type="text"> Sardeshmukh, P. D., Compo, G. P., and Penland, C.: Changes of probability associated with El Niño, J. Climate, 13, 4268–4286, 2000. </reference>
		<reference numeration="46" content_type="text"> Saunders, A. and Ghil, M.: A Boolean delay equation model of ENSO variability, Physica D, 160, 54–78, 2001. </reference>
		<reference numeration="47" content_type="text"> Saynisch, J., Kurths, J., and Maraun, D.: A conceptual ENSO model under realistic noise forcing, Nonlin. Processes Geophys., 13, 275–285, 2006. </reference>
		<reference numeration="48" content_type="text"> Shampine, L. F. and Thompson, S.: A friendly Fortran 90 DDE solver, Appl. Numer. Math., 56(2–3), 503–516, 2006. </reference>
		<reference numeration="49" content_type="text"> Suarez, M. J. and Schopf, P. S.: A delayed action oscillator for ENSO, J. Atmos. Sci, 45, 3283–3287, 1988. </reference>
		<reference numeration="50" content_type="text"> Trenberth, K. E.: The definition of El Niño, B. Am. Meteorol. Soc., 78, 2771–2777, 1997. </reference>
		<reference numeration="51" content_type="text"> Tziperman, E., Stone, L., Cane, M., and Jarosh, H.: El Niño chaos: Overlapping of resonances between the seasonal cycle and the Pacific ocean-atmosphere oscillator, Science, 264, 72–74, 1994. </reference>
		<reference numeration="52" content_type="text"> Tziperman, E., Cane, M. A., and Zebiak, S. E.: Irregularity and locking to the seasonal cycle in an ENSO prediction model as explained by the quasi-periodicity route to chaos, J. Atmos. Sci., 50, 293–306, 1995. </reference>
		<reference numeration="53" content_type="text"> Verbickas, S.: Westerly wind bursts in the tropical Pacific, Weather, 53, 282–284, 1998.  </reference>
	</references>
</article>

