<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.clim-past-discuss.net/inc/cpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>6</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cpd-6-905-2010</doi>
	<article_url>http://www.clim-past-discuss.net/6/905/2010/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/6/905/2010/cpd-6-905-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/6/905/2010/cpd-6-905-2010.pdf</fulltext_pdf>
	<start_page>905</start_page>
	<end_page>961</end_page>
	<publication_date>2010-05-20</publication_date>
	<article_title content_type="html">Do periodic consolidations of Pacific countercurrents trigger global cooling by equatorially symmetric La Niña?</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. H. Duke</name>
			<email>john.duke@curvewater.com</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CurveWater, LLC 138 Congdon St., Providnece, RI 02906, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A sporadic phenomenon of internal tide resonance (ITR) in the western
equatorial Pacific thermocline is shown to precede 11 of 12 major upturns in
the Niño 3.4 index between 1992 and 2008. Observed ITR has up to 9 °C
semidiurnal temperature excursions indicating thermocline heave, but is
invisible in time resolution longer than one day. It is independent of
westerly wind bursts (WWB). A hypothesis is advanced that (1) ITR dissipates
vorticity, leading to Pacific countercurrent consolidation (PCC) by reducing
the vortex stretching term in Sverdrup balance. The consequence of lost
vorticity survives ephemeral ITR events; (2) The specific surface area of
countercurrents is reduced by PCC, which reduces frictional opposition to
zonal gradient pressure, which triggers eastward advection at El Niño onset;
(3) PCC also accelerates transfer of potential energy to the &quot;pycnostad&quot;
below the Equatorial Undercurrent. This shoals the equatorial thermocline,
leading to a distinct mode of equatorially symmetric La Niña (ESLN)
characterized by a winter monsoon cell above a &quot;cold eye&quot; that is
separated from the South American continent, as in 1998; (4) Precessional
southward intertropical convergence zone migration (ITCZ) is an alternate
PCC trigger, but its effect is modulated by obliquity; and (5) ESLN causes
global cooling in all timescales by (a) reduced Hadley cell water vapor
production when its rising branch is above the cold eye, (b) equatorward
shift in southern circumpolar westerlies due to Hadley cell constriction,
(c) possible CO&lt;sub&gt;2&lt;/sub&gt; sequestration by increased EUC iron fertilized export
production on the equator, and (d) possible adjacent cloud seeding by
biogenic dimethyl sulphide. Surprising coincidences of WWB with perigean
eclipses suggest a parallel atmospheric tide influence.

Proposed PCC-ESLN forcing operates in multiple timescales, beginning where the
annual cycle of strong equinoctial tides coincides with the minimum perigee
cycle. This forcing corresponds with El Niño Southern Oscillation (ENSO)
events in 1997, 2002, and 2006. Next, extreme central eclipses that perturb
perigee-sysygy intervals also correspond with extreme ENSO events, notably in
1877, 1888, and 1982, and a 586 year cycle in the frequency of these eclipses
corresponds with known stadial events in the past 4 thousand years. Contrast in the
586 year cycle increases with Earth eccentricity because it is the result of
shorter synodic months at aphelion. Longer timescale forcing is by orbital
control of the east-central Pacific ITCZ position, yielding a 10 thousand
year fast ice sheet melt interval between March and September perihelion.
But default ESLN is only interrupted when perihelion in March coincides with
rising obliquity. A change in the phase relation between obliquity and
precession from 1:2 to 3:5 or 2:5 may therefore explain skipped obliquity
cycles after the mid-Pleistocene transition. A secular improvement in
eclipse commensurability that parallels Cenozoic cooling is noted.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alory, G. and Delcroix, T.: Interannual sea level changes and associated mass transports in the tropical Pacific from TOPEX/Poseidon data and linear model results (1964–1999), J. Geophys. Res., 107(C10), 3153, doi:10.1029/2001JC001067, 2002. </reference>
		<reference numeration="2" content_type="text"> Barker, S., Diz, P., Vautravers, M. J., Pike, J., Knorr, G., Hall, I. R., and Broecker, W. S.: Interhemispheric Atlantic seesaw response during the last deglaciations, Nature, 457, 1097–1103, 2009. </reference>
		<reference numeration="3" content_type="text"> Beaufort, L., de Garidel-Thoron, T., Mix, A. C., and Pisias, N.: ENSO-like forcing on oceanic primary production during the Late Pleistocene, Science, 293, 2440–2444, 2001. </reference>
		<reference numeration="4" content_type="text"> Beaufort, L., de Garidel-Thoron, T., Linsley, B., Oppo, D., and Buchet, N.: Biomass burning and oceanic primary production estimates in the Sulu Sea area over the last 380 kyr and the East Asian monsoon dynamics, Mar. Geol., 201, 53–65, 2003. </reference>
		<reference numeration="5" content_type="text"> Berger, A.: Long-Term Variations of Daily Insolation and Quaternary Climate Changes, J. Atmos. Sci., 35, 2362–2367, 1978. </reference>
		<reference numeration="6" content_type="text"> Berger, A. and Loutre, M. F.: Insolation values for the climate of the last 10~million of years, Quaternary Sci. Rev., 10(4), 297–317, 1991. </reference>
		<reference numeration="7" content_type="text"> Berger, A. L., Loutre, M. F., and Crucifix, M.: The Earth&apos;s climate in the next hundred thousand years (100 kyr), Surv. Geophys., 24, 117–138, 2003. </reference>
		<reference numeration="8" content_type="text"> Berger, A. L. and Loutre, M. F.: Astonomical theory of climate change, J. Phys IV France, 121, 1–35, doi:10.1051/jp4:2004121001, 2004. </reference>
		<reference numeration="9" content_type="text"> Bond, G. C., Showers, W., Elliot, M., Evans, M., Lotti, R., Hajdas, I., Bonani, G., ans Johnson, S.: The north Atlantic&apos;s 1–2 kyr climate rhythm: Relation to Heinrich Events, Dansgaard/Oeschger cycles and the Little Ice Age, Geophysical Monograph~112, American Geophysical Union, 35–58, 1999. </reference>
		<reference numeration="10" content_type="text"> Broecker, W. S.: Mountain Glaciers: Recorders of Atmospheric Water Vapor Content?, Global Biogeochem. Cy., 11(4), 589–597, 1997. </reference>
		<reference numeration="11" content_type="text"> Broecker, W. S.: Does the Trigger for Abrupt Climate Change Reside in the Ocean or in the Atmosphere?, Science, 300, 1519–1522, 2003. </reference>
		<reference numeration="12" content_type="text"> Broecker, W. S. and Denton, G. H.: The role of ocean-atmosphere reorganizations in glacial cycles, Geochim. Cosmochim. Acta, 53, 2465–2501, 1989. </reference>
		<reference numeration="13" content_type="text"> Broecker, W. S. and van Donk, J.: Insolation changes, ice volumes, and the O18 record in deep sea cores, Rev. Geophys. Space Phys., 8(1), 169–198, 1970. </reference>
		<reference numeration="14" content_type="text"> Brown, J. M. and Fedorov, A. V.: Estimating the diapycnal transport contribution to warm water volume variations in the tropical Pacific, J. Climate, 23, 221–237, 2010. </reference>
		<reference numeration="15" content_type="text"> Cane, M. A.: Climate change: A role for the tropical Pacific, Science, 282, 59–61, 1998. </reference>
		<reference numeration="16" content_type="text"> Cane, M. A. and Clement, A.: A role for the tropical Pacific coupled ocean-atmosphere system on Milankovitch and millennial timescales, Part~II: Global impacts, Geophysical Monograph~112, American Geophysical Union, 373–383, 1999. </reference>
		<reference numeration="17" content_type="text"> Cane, M. A. and Molnar, P.: Closing of the Indonesian seaway as a precursor to east African aridification around 3–4~million years ago, Nature, 411, 157–162, 2001. </reference>
		<reference numeration="18" content_type="text"> Cervany, R. S. and Shaffer, J. A.: The moon and El Niño, Geophys. Res. Lett., 28(1), 25–28, 2001. </reference>
		<reference numeration="19" content_type="text"> Chaves, F. P., Strutton, P. G., Friederich, G. E., Feely, R. A., Feldman, G. C., Foley, D. G., and McPhaden, M. J.: Biological and chemical response of the equatorial Pacific Ocean to the 1997–98 El Niño, Science, 286, 2126–2131,1999. </reference>
		<reference numeration="20" content_type="text"> Chiang, J. C. H.: The tropics in paleoclimate, Annu. Rev. Earth Pl. Sc., 37, 263–297, 2009. </reference>
		<reference numeration="21" content_type="text"> Chiang, J. C. H. and Vimont, D. J.: Analogous Pacific and Atlantic meridional modes of tropical atmosphere-ocean variability, J. Climate, 17, 4141–4158, 2004. </reference>
		<reference numeration="22" content_type="text"> Chiang, J. C. H., Fang, Y., and Chang, P.: Interhemispheric thermal gradient and tropical Pacific climate, Geophys. Res. Lett., 35, L14704, doi:10.1029/2008GL034166, 2008. </reference>
		<reference numeration="23" content_type="text"> Chiang, J. C. H., Fang, Y., and Chang, P.: Pacific Climate Change and ENSO Activity in the Mid-Holocene, J. Climate, 22, 923–939, 2009. </reference>
		<reference numeration="24" content_type="text"> Clark, P. U., Webb, R. S., and Keigwin, L. D.: Mechanisms of global climate change at millennial time scales, Geophysical Monograph~112, American Geophysical Union, 1999. </reference>
		<reference numeration="25" content_type="text"> Charlson, R. J., Lovelock, J. E., Andreae, M. O. and Warren, S. G.: Ocean phytoplankton, atmospheric sulphur, cloud albedo and climate, Nature, 326, 655–661, 1987. </reference>
		<reference numeration="26" content_type="text"> Clemens, S. C. and Prell, W. L.: A 350,000~year summer-monsoon multi-proxy stack from the Owen Ridge, northern Arabian Sea, Mar. Geol., 201, 35–51, 2003. </reference>
		<reference numeration="27" content_type="text"> Clemens, S. C.: Millennial-band climate spectrum resolved and linked to centennial-scale solar cycles, Quaternary Sci. Rev., 24, 521–531, 2005. </reference>
		<reference numeration="28" content_type="text"> Clement, A. C. and Peterson, L. C.: Mechanisms of abrupt climate change of the last glacial period, Rev. Geophys., 46, RG4002, doi:10.1029/2006RG000204, 2008. </reference>
		<reference numeration="29" content_type="text"> Clement, A., Seager, R., and Cane, M. A.: Orbital control on the El Niño/Southern Oscillation and the tropical climate, Paleoceanography, 14, 441–456, 1999. </reference>
		<reference numeration="30" content_type="text"> Clement, A., Cane, M. A., and Seager, R.: Suppression of El Niño during the mid-Holocene by changes in the Earth&apos;s orbit, Paleoceanography, 15(6), 731–737, 2000. </reference>
		<reference numeration="31" content_type="text"> Clement, A., Cane, M. A. and Seager, R.: An Orbitally Driven Tropical Source for Abrupt Climate Change, J. Climate, 14(11), 2369–2375, 2001. </reference>
		<reference numeration="32" content_type="text"> Coale, K. H., Johnson, K. S., Fitzwater, S. E., Gordon, R. M., Tanner, S., Chavez, F. P., Ferioli, L., Sakamoto, C., Rogers, P., Millero, F., Steinberg, P., Nightingale, P., Cooper, D., Cocklan, W. P., Landry, M. R., Constantinou, J., Rollwagen, G., Trasvina, A., and Kudela, R.: A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean, Nature, 383, 495–501, 1996. </reference>
		<reference numeration="33" content_type="text"> Cook, E. R., Woodhouse, C. A., Eakin, C. M., Meko, D. M., and Stahle, D. W.: Long term aridity changes in the western united states, Science, 306, 1015–1018, 2004. </reference>
		<reference numeration="34" content_type="text"> Duke, J. H.: A Common Mechanism of Multi-timescale Abrupt Global Change, Eos Trans AGU, 83(47), Fall Meet. Suppl., Abstract PP23C-1485, 2008. </reference>
		<reference numeration="35" content_type="text"> Fang, Y., Chiang, J. C. H., and Chang, P.: Variation of mean sea surface temperature and modulation of El Niño – Southern Oscillation variance during the past 150 years, Geophys. Res. Lett., 35, L08703, doi:10.1029/2007GL033097, 2008. </reference>
		<reference numeration="36" content_type="text"> Fedorov, A. V.: The response of the coupled tropical ocean–atmosphere to westerly wind bursts, Q. J. Roy. Meteorol. Soc., 128, 1–23, 2002. </reference>
		<reference numeration="37" content_type="text"> Fedorov, A. and Melville, W. K.: Kelvin Fronts on the Equatorial Thermocline, J. Phys. Oceanogr., 30, 1692–1705, 2000. </reference>
		<reference numeration="38" content_type="text"> Fedorov, A. V., Dekens, P. S., McCarthy, M., Ravelo, A. C., deMenocal, P. B., Barreiro, M., Pacanowski, R. C., and Philander, S. G.: The Pliocene paradox (mechanisms for a permanent El Niño), Science, 312, 1485–1489, 2006. </reference>
		<reference numeration="39" content_type="text"> Ferrari, R. and Wunsch, C.: Ocean circulation kinetic energy: reservoirs, sources, and sinks, Annu. Rev. Fluid Mech., 41, 253–282, 2009. </reference>
		<reference numeration="40" content_type="text"> Ffield, A. and Gordon, A. L.: Tidal mixing signatures in the Indonesian Seas, J. Phys. Oceanogr., 26, 1924–1937, 1996. </reference>
		<reference numeration="41" content_type="text"> Garrett, C. and Kunze, E.: Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech., 39, 57–87, 2007. </reference>
		<reference numeration="42" content_type="text"> Gergis, J. L. and Fowler, A. M.: A history of ENSO events since A D 1525: implications for future climate change, Climatic Change, 92, 343–387, 2009. </reference>
		<reference numeration="43" content_type="text"> Gregg, M. C., Peters, H., Wesson, J. C., Oakey, N. S., and Shay, T. J.: Intensive measurements of turbulence and shear in the equatorial undercurrent, Nature, 318, 140–144, 1985. </reference>
		<reference numeration="44" content_type="text"> Gregg, M. C., Sanford, T. B., and Winkel, D. P.: Reduced mixing from the breaking of internal waves in equatorial waters, Nature, 422, 513–515, 2003. </reference>
		<reference numeration="45" content_type="text"> Grodsky, S. A. and Carton, J. A.: Intense surface currents in the tropical Pacific during 1996–1998, J. Geophys. Res., 206(C8), 16673–16684, 2001. </reference>
		<reference numeration="46" content_type="text"> Grootes, P. and Stuiver, M.: Oxygen 18/16 variability in Greenland snow and ice with 10&lt;sup&gt;3&lt;/sup&gt;–10$^5$ year time resolution, J. Geophys. Res., 102(C12), 26455–26470, 1997. </reference>
		<reference numeration="47" content_type="text"> Hanna, E.: Anomalous peak in Antarctic sea-ice area, winter 1998, coincident with ENSO, Geophys. Res. Lett., 28(8), 1595–1598, 2001. </reference>
		<reference numeration="48" content_type="text"> Harrison, M. J. and Hallberg, R. W.: Pacific subtropical cell response to reduced equatorial dissipation, J. Phys. Oceanogr., 38, 1894–1912, 2008. </reference>
		<reference numeration="49" content_type="text"> Haug, G. H., Konrad, A., Hughen, K. A., Sigman, D. M., Peterson, L. C., and Röhl, U.: Southward migration of the intertropical convergence zone through the holocene, Science, 293, 1304–1308, 2001. </reference>
		<reference numeration="50" content_type="text"> Hays, J. D., Imbrie, J., and Shackleton, N. J.: Variations in the earth&apos;s orbit: Pacemanker of the ice ages, Science, 194, 1121–1132, 1976. </reference>
		<reference numeration="51" content_type="text"> Heming, S. R., Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint, Rev. Geophys., 42, RG1005, doi:10.1029/2003RG000128, 2004. </reference>
		<reference numeration="52" content_type="text"> Hendon, H. H., Wheeler, M. C., and Zhang, C.: Seasonal Dependence of the MJO-ENSO Relationship, J. Climate, 20, 531–543, 2007. </reference>
		<reference numeration="53" content_type="text"> Hinnov, L. A., Schulz, M., and Yiou, P.: Interhemispheric space-time attributes of the Dansgaard-Oeschger oscillations between 100~and 0 ka, Quaternary Sci. Rev., 21(10), 1213–1228, 2002. </reference>
		<reference numeration="54" content_type="text"> Huybers, P.: Early Pleistocene Glacial Cycles and the Integrated Summer Insolation Forcing, Science, 313, 508–511, 2006. </reference>
		<reference numeration="55" content_type="text"> Huybers, P.: Glacial variability over the last two million years: an extended depth-derived age model, continuous obliquity pacing, and the Pleistocene progression, Quaternary Sci. Rev., 26, 37–55, 2007. </reference>
		<reference numeration="56" content_type="text"> Huybers, P. and Wunsch, C.: Obliquity pacing of the late Pleistocene glacial terminations, Nature, 434, 491–494, 2005. </reference>
		<reference numeration="57" content_type="text"> Huybers, P.: Pleistocene glacial variability as a chaotic response to obliquity forcing, Clim. Past, 5, 481–488, doi:10.5194/cp-5-481-2009, 2009. </reference>
		<reference numeration="58" content_type="text"> Jin, F.-F.: An Equatorial Ocean Recharge Paradigm for ENSO, Part~I: Conceptual Model, J. Atmos. Sci., 54, 811–829, 1997a. </reference>
		<reference numeration="59" content_type="text"> Jin, F.-F.: An Equatorial Ocean Recharge Paradigm for ENSO, Part~II: A Stripped-Down Coupled Model, J. Atmos. Sci., 54, 830–847, 1997b. </reference>
		<reference numeration="60" content_type="text"> Johnson, G. C. and McPhaden, M. J.: Interior pycnocline flow from the subtropical to the equatorial Pacific Ocean, J. Phys. Oceanogr., 29, 3073–3089, 1999. </reference>
		<reference numeration="61" content_type="text"> Johnson, G. C., Sloyan, B. M., Kessler, W. S., and McTaggart, K. E.: Direct measurements of the upper ocean currents and water properties across the tropical Pacific during the 1990s, Prog. Oceanogr., 52, 31–61, 2002. </reference>
		<reference numeration="62" content_type="text"> Johnston, T. M. S., Merrifield, M. A., and Holloway, P. E.: Internal tide scattering at the Line Islands Ridge, J. Geophys. Res., 108(C11), 3365, doi:10.1029/2003JC001844, 2003. </reference>
		<reference numeration="63" content_type="text"> Jones, J. H.: Vertical mixing in the equatorial undercurrent, J. Phys. Oceanogr., 3, 286–196, 286–296, 1973. </reference>
		<reference numeration="64" content_type="text"> Keeling, C. W. and Whorf, T. P.: Possible forcing of global temperature by oceanic tides, P. Natl. Acad. Sci. USA, 94, 8321–8328, 1997. </reference>
		<reference numeration="65" content_type="text"> Keeling, C. W. and Whorf, T. P.: The 1,800-year oceanic tidal cycle: A Possible cause of rapid climate change, P. Natl. Acad. Sci. USA, 97(8), 3814–3819, 2000. </reference>
		<reference numeration="66" content_type="text"> Kessler, W. S., Johnson, G. C., and Moore, D. W.: Sverdrup and Nonlinear Dynamics of the Pacific Equatorial Currents, J. Phys. Oceanogr., 33, 994–1008, 2003. </reference>
		<reference numeration="67" content_type="text"> Kienast, M., Kienast, S. S., Calvert, S. E., Eglinton, T. I., Mollenhauer, G., François, R., and Mix, A. C.: Eastern Pacific cooling and Atlantic overturning circulation during the last deglaciations, Nature, 443, 846–849, 2006. </reference>
		<reference numeration="68" content_type="text"> Koutavas, A. and Lynch-Stieglitz, J.: Glacial-interglacial dynamics of the eastern equatorial Pacific cold tongue-Intertropical Convergence system reconstructed from oxygen isotope records, Paleoceanography, 18(4), 1089, doi:10.1029/2003PA000894, 2003. </reference>
		<reference numeration="69" content_type="text"> Koutavas, A. and Lynch-Stieglitz, J.: Variability of the marine ITCZ over the eastern Pacific during the past 30,000 years, in: The Hadley Circulation: Present, Past and Future, edited by: Diaz, H. F. and Bradley, R. S., Kluwer Academic Publishers, The Netherlands, 347–369, 2005. </reference>
		<reference numeration="70" content_type="text"> Koutavas, A., Lynch-Stieglitz, J., Marchitto Jr., T. M., and Sachs, J. P.: El Niño-like pattern in ice age tropical Pacific sea surface temperature, Science, 297, 226–230, 2002. </reference>
		<reference numeration="71" content_type="text"> Kukla, G. J., Clement, A. C., Cane, M. A., Gavin, J. E., and Zebiac, Z. E.: Last Interglacial and early glacial ENSO, Quaternary Res., 58, 27–32, 2002. </reference>
		<reference numeration="72" content_type="text"> Kukla, G. J. and Gavin, J. E.: Milankovitch climate reinforcements, Global Planet. Change, 40, 27–48, 2004. </reference>
		<reference numeration="73" content_type="text"> Kukla, J. G. and Gavin, J. E.: Did glacials start with global warming?, Quaternary Sci. Rev., 24, 1547–1557, 2005. </reference>
		<reference numeration="74" content_type="text"> Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., and Levrard, B.: A long term numerical solution for the insolation quantities of the Earth, Astron. Astrophys., 428, 261–285, 2004. </reference>
		<reference numeration="75" content_type="text"> Lindzen, R. S.: Atmospheric Tides, Ann. Rev. Earth Pl. Sc., 7, 199–225, 1979. </reference>
		<reference numeration="76" content_type="text"> Lisiecki, L. E. and Raymo, M. E.: A Pliocene-Pleistocene stack of 57~globally distributed benthic $\delta^18$O records, Paleoceanography, 20, PA1003, doi:10.10289/2004pa001071, 2005. </reference>
		<reference numeration="77" content_type="text"> Lisiecki, L. E. and Raymo, M. E.: Plio-Pleistocene climate evolution: trends and transitions in glacial cycle dynamics, Quaternary Sci. Rev., 26, 56–69, 2007. </reference>
		<reference numeration="78" content_type="text"> Liu, Z., Cleaveland, L. C., and Herbert, T. D.: Early onset and origin of 100-kry cycles in Pleistocene tropical SST records, Earth Planet Sc. Lett., 265, 703–715, 2008. </reference>
		<reference numeration="79" content_type="text"> Lyard, F., Lefevre, F., Letellier, T., and Francis, O.: Modelling the global ocean tides: modern insights from FES2004, Ocean Dynam., 56, 394–415, 2006. </reference>
		<reference numeration="80" content_type="text"> Lyle, M. W., Prahl, F. G., and Sparrow, M. A.: Upwelling and productivity changes inferred from a temperature record in the central equatorial Pacific, Nature, 355, 812–815, 1992. </reference>
		<reference numeration="81" content_type="text"> Marshall, S. J. and Clark, P. U.: Basal temperature evolution of North American ice sheets and implications for the 100-kyr cycle, Geophys. Res. Lett., 29(24), 2214, doi:10.1029/2002GL015192, 2002. </reference>
		<reference numeration="82" content_type="text"> McPhaden, M. J.: The Equatorial Undercurrent: 100~years of discovery, Eos, 67(40), 7~October, 1986. </reference>
		<reference numeration="83" content_type="text"> McPhaden, M. J.: Genesis and evolution of the 1997–98 El Niño, Science, 283, 950–954, 1999. </reference>
		<reference numeration="84" content_type="text"> McPhaden, M. J.: Evolution of the 2002/03 El Niño, B. Am. Meteor. Soc., May, 677–695, 2004. </reference>
		<reference numeration="85" content_type="text"> McPhaden, M. J.: ENSO as an integrating concept in earth science, Science, 314, 1740–1745, 2006. </reference>
		<reference numeration="86" content_type="text"> Meeus, J: Mathematical astronomy morsels~III, William-Bell, Inc. Richmond, VA, USA, 2004. </reference>
		<reference numeration="87" content_type="text"> Meyers, G. and Donguy, J.-R.: The north equatorial countercurrent and heat storage in the western Pacific Ocean durinh 1982–83, Science, 312, 258–260, 1984. </reference>
		<reference numeration="88" content_type="text"> MICA~2.0: US~Naval Observatory multiyear Interactive computer almanac 1800–2050, Willmann-Bell, Inc. Richmond, VA, 1998–2005. </reference>
		<reference numeration="89" content_type="text"> Munk, W. and Wunsch, C.: Abyssal recipes~II: energetic of tidal and wind mixing, Deep-Sea Res. Pt I, 45, 1977–2010, 1998. </reference>
		<reference numeration="90" content_type="text"> Munk, W., Dzieciuch, M., and Jayne, S.: Millennial Climate Variability: Is There a Tidal Connection?, J. Climate, 15, 370–385, 2002. </reference>
		<reference numeration="91" content_type="text"> Murray, R. W., Knowlton, C., Leinen, M., Mix, A. C., and Polsky, C. H.: Export production and carbonate dissolution in the central equatorial Pacific Ocean over the last 1 Myr, Paleoceanography, 15(6), 570–592, 2000a. </reference>
		<reference numeration="92" content_type="text"> Murray, R. W., Knowlton, C., Leinen, M., Mix, A. C., and Polsky, C. H.: Export production and terrigenous matter in the Central Equatorial Pacific Ocean during interglacial oxygen isotope Stage~11, Global Planet. Change, 24, 59–78, 2000b. </reference>
		<reference numeration="93" content_type="text"> Oort, A. H. and Yienger, J. J.: Observed interannual variability in the Hadley Circulation and its connection to ENSO, J. Climate, 9, 2751–2767, 1996. </reference>
		<reference numeration="94" content_type="text"> Ortiz, J. D., O&apos;Connell, S. B., Delvisco, J., Dean, W., Carriquiry, J. D., Marchitto, T., Zheng, Y., and van Geen, A.: Enhanced marine productivity off western North America during warm climate intervals of the past 52 k.y., Geology, 32(6), 521–524, 2004. </reference>
		<reference numeration="95" content_type="text"> Paytan, A., Kastner, M., and Chavez, F. P.: Glacial to Interglacial Fluctuations in Productivity in the Equatorial Pacific as Indicated by Marine Barite, Science, 274, 1355–1357, 1996. </reference>
		<reference numeration="96" content_type="text"> Pedersen, T. F.: Increased productivity in the eastern equatorial Pacific during the lat glacial maximum (19,000~to 14,000 B.P.), Geology, 11, 16–19, 1983. </reference>
		<reference numeration="97" content_type="text"> Peeters, F. J. C., Acheson, R., Brummer, G.-J. A., deRuijter, W. P. M., Schneider, R. R., Ganssen, G. M., Ufkes, E., and Kroon, D.: Vigorous exchange between the Indian and Atlantic oceans at the end of the past five glacial periods, Nature, 430, 661–665, 2004. </reference>
		<reference numeration="98" content_type="text"> Philander, S. G. H., Gu, D., Halpern, D., Lambert, G., Lau, N.-C., Li, T., and Pacanowski, R. C.: Why the ITCZ is mostly north of the equator, J. Climate, 9(12), 2958–2972, 1996. </reference>
		<reference numeration="99" content_type="text"> Picaut, J., Ioualalen, M., Menkes, C., Delcroix, T., and McPhaden, M. J.: Mechanism of the Zonal Displacements of the Pacific Warm Pool: Implications for ENSO, Science, 274, 1486–1489, 1996. </reference>
		<reference numeration="100" content_type="text"> Pierrehumbert, R. T.: Climate change and the tropical Pacific: the sleeping dragon wakes, P. Natl. Acad. Sci., 97(4), 1355–1358, 2000. </reference>
		<reference numeration="101" content_type="text"> Platzman, G. W.: The atmospheric tide as a continuous spectrum: lunar semidiurnal tide in surface pressure, Meteorol. Atmos. Phys., 38, 70–88, 1988. </reference>
		<reference numeration="102" content_type="text"> Ray, R. D.: Decadal climate variability: Is there a tidal connection?, J. Climate, 20, 3542–3560, 2007. </reference>
		<reference numeration="103" content_type="text"> Ray, R. D. and Cartwright, D. E.: Estimates of internal energy fluxes from Topex/Poseidon altimetry: central North Pacific, Geophys. Res. Lett., 28(7), 1259–1263, 2001. </reference>
		<reference numeration="104" content_type="text"> Raymo, M.: The timing of major climate terminations, Paleoceanography, 12(4), 577–585, 1997. </reference>
		<reference numeration="105" content_type="text"> Raymo, M. E. and Nisancioglu, K.: The 41 kyr world: Milankovitch&apos;s other unsolved mystery, Paleoceanography, 18(1), 1011, doi:10.1029/2002PA00079, 2003. </reference>
		<reference numeration="106" content_type="text"> Robertson, R. and Field, A.: M2~baroclinic tides in the Indonesian Seas, Oceanography, 18(4), December, 2005. </reference>
		<reference numeration="107" content_type="text"> Rockström, J., Steffen, W., Noone, K., Persson, Å., Chapin~III, F. S., Lambin, E., Lenton, T. M., Scheffer, M., Folke, C., Schellnhuber, H., Nykvist, B., De Wit, C. A., Hughes, T., van der Leeuw, S., Rodhe, H., Sörlin, S., Snyder, P. K., Costanza, R., Svedin, U., Falkenmark, M., Karlberg, L., Corell, R. W., Fabry, V. J., Hansen, J., Walker, B., Liverman, D., Richardson, K., Crutzen, P., and Foley, J.: Planetary boundaries: exploring the safe operating space for humanity, Ecol. Soc., 14(2), 32, 2009. </reference>
		<reference numeration="108" content_type="text"> Rodbell, D. T., Seltzer, G. O., Anderson, D. M., Abott, M. B., Enfield, D. B., and Newman, J. H.: An $\sim$15,00~year record of El Niñ0-driven alleviation in southwestern Equador, Science, 283, 516–520, 1999. </reference>
		<reference numeration="109" content_type="text"> Ruddiman, W. F.: Orbital changes and climate, Quaternary Sci. Rev., 25, 3092–3112, 2006. </reference>
		<reference numeration="110" content_type="text"> Ryan, J. P., Polito, P. S., Strutton, P. G., and Chavez, F. P.: Unusual large-scale phytoplankton blooms in the equatorial Pacific, Prog. Oceangr., 55, 263–285, 2002. </reference>
		<reference numeration="111" content_type="text"> Sandweiss, D. H., Richardson~III, J. B., Reitz, E. J., Rollins, H. B., and Maasch, K. A.: Geoarchaeological evidence from Peru for a 5000~years~B.P onset of El Niño, Science, 273, 1531–1533, 1996. </reference>
		<reference numeration="112" content_type="text"> Seager, R., Clement, A. C., and Cane, M. A.: Glacial Cooling in the Tropics: Exploring the roles of Tropspheric Water Vapor, Surface Wind Speed, and Boundary Layer Proceses, J. Atmos. Sci., 57, 2144–2157, 2000. </reference>
		<reference numeration="113" content_type="text"> Seager, R., Battisti, D. S., Yin, J., Gordon, N., Naiki, N., Clement, A. C., and Cane, M. A.: Is the Gulf Stream responsible for Europe&apos;s mild winters?, Q. J. Roy. Meteorol. Soc., 128(586), 2563–2586, 2002. </reference>
		<reference numeration="114" content_type="text"> Seager, R., Naik, N., Ting, M., Cane, M. A., Harnik, N., and Kushnir, Y.: Adjustment of the atmospheric circulation to tropical Pacific SST anomalies: Variability of transient eddy propagation in the Pacific-North America sector, Q. J. Roy. Meteorol. Soc., 136(647), 277–296, 2010. </reference>
		<reference numeration="115" content_type="text"> Seidel, D. J., Fu, Q., Randel, W. J., and Reichler, T. J.: Widening the tropical belt in a changing climate, Nat. Geosci., 1, 21–24, 2008. </reference>
		<reference numeration="116" content_type="text"> Shaffer, J. A. and Cerveny, R. S.: Long-term equilibrium tides, J. Geophys. Res., 103(C9), 18801–18807, 1998. </reference>
		<reference numeration="117" content_type="text"> Steffensen, J. P., Anderson, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen, D., Fischer, H., Goto-Azuma, K., Hansson, M., Johnsen, S. J., Jouzel, J., Masson-Delmotte, V., Popp, T., Rasmussen, S. O., Röthlisberger, R., Ruthe, U., Stauffer, B., Siggaard-Andersen, M.-L., Sveinbjorndottir, A. E., Svensson, A., and White, J. W. C.: High resolution Greenland ice coredata show abrupt climate change happens in few years, Science, 321, 680–684, 2008. </reference>
		<reference numeration="118" content_type="text"> Steves, B. A.: The cycles of selene, Vista. Ast. S., 41(4), 543–571, 1998. </reference>
		<reference numeration="119" content_type="text"> Stott, L., Poulsen, C., Lund, S., and Thunell, R.: Super ENSO and global climate oscillations at millennial time scales, Science, 297, 222–226, 2002. </reference>
		<reference numeration="120" content_type="text"> Sverdrup, H. U.: Wind-driven currents in a baroclinic ocean; with application to the equatorial currents of the eastern Pacific, P. Natl. Acad. Sci., 33, 318–326, 1947. </reference>
		<reference numeration="121" content_type="text"> Takahashi, T., Sutherland, S. C., Sweeney, C., Poisson, A., Metzl, N., Tilbrook, B., Bates, N., Wanninkhof, R., Feely, R. A., Sabine, C., Olafsson, J., and Nojiri, Y.: Global sea-air CO&lt;sub&gt;2&lt;/sub&gt; flux based on climatological surface ocean $p$CO&lt;sub&gt;2&lt;/sub&gt;, and seasonal biological and temperature effects, Deep-Sea Res. Pt II, 49, 1601–1622, 2002. </reference>
		<reference numeration="122" content_type="text"> Takahashi, K. and Battisti, D. S.: Processes Controlling the Mean Tropical Pacific Precipitation Pattern, Part~I: The Andes and the Eastern Pacific ITCZ, J. Climate, 20, 3434–3451, 2007. </reference>
		<reference numeration="123" content_type="text"> Tang, Y. and Yu, B.: MJO and its relationship to ENSO, J. Geophys. Res., 113, D14106, doi:10.1029/2007JD009230, 2008. </reference>
		<reference numeration="124" content_type="text"> Taylor, K. C., Lamorey, G. W., Doyle, G. A., Alley, R. B., Grootes, P. M., Mayewski, P. A., White, J. W. C., and Barlow, L. K.: The &quot;flickering switch&quot; of late Pleistocene climate change, Nature, 361, 432–436, 1993. </reference>
		<reference numeration="125" content_type="text"> Thompson, L. G., Moseley-Thompson, E., Brecher, H., Davis, M., Leon, B., Les, D., Lin, P. N., Mashoitta, T., and Moutain, K.: Abrupt tropical climate change: Past and present, P. Natl. Acad. Sci., 103(28), 10536–10543, 2006. </reference>
		<reference numeration="126" content_type="text"> Timmermann, A., Lorenz, S. J., An, S.-I., Clement, A., and Xie, S.-P.: The Effect of Orbital Forcing on the Mean Climate and Variability of the Tropical Pacific, J. Climate, 20(16), 4147–4159, 2007a. </reference>
		<reference numeration="127" content_type="text"> Timmermann, A., Okumura, Y., An, S.-I., Clement, A., Dong, B., Guilyardi, E., Hu, A., Jungclaus, J. H., Renold, M., Stocker, T. F., Stouffer, R. J., Sutton, R., Xie, S.-P., and Yin, J.: The influence of a weakening of the Atlantic meridional overturning circulation on ENSO, J. Climate, 20, 4899–4919, 2007b. </reference>
		<reference numeration="128" content_type="text"> Toggweiler, J. R., Russel, J. L., and Carson, S. R.: Midlatitude westerlies, atmospheric CO&lt;sub&gt;2&lt;/sub&gt;, and climate change during the ice ages, Paleoceanography, 21, PA2005, doi:10.1029/2005PA001154, 2006. </reference>
		<reference numeration="129" content_type="text"> Trenberth, K. E. and Stepaniak, D. P.: Indices of El Niño evolution, J. Climate, 14, 1697–1701, 2001. </reference>
		<reference numeration="130" content_type="text"> Trend-Staid, M. and Prell, W. L.: Sea surface temperature at the Last Glacial Maximum: A reconstruction using the modern analog technique, Paleoceanography, 17(4), 1065, doi:10.1029/2000PA000506, 2002. </reference>
		<reference numeration="131" content_type="text"> Treolar, N. C.: Luni-solar tidal influences on climate variability, Int. J. Climatol., 22, 1527–1542, 2002. </reference>
		<reference numeration="132" content_type="text"> Turner, S. M., Nightingale, P. D., Spokes, L. J., Liddicoat, M. I., and Liss, P. S.: Increased dimethyl sulphide concntrations in sea water from in situ iron enrichment, Nature, 383, 513–517, 1996. </reference>
		<reference numeration="133" content_type="text"> Van den Bergh, G.: Periodicity and variability of solar (and lunar) eclipses, H D Tjeenk Willink &amp; Zoon N V., Haarlem, 1955. </reference>
		<reference numeration="134" content_type="text"> Vecchi, G. A.: The Termination of the 1997–1998 El Niño, Part~II: Mechanism of Atmospheric Change, J. Climate, 19, 2647–2664, 2006. </reference>
		<reference numeration="135" content_type="text"> Wang, B. and Wang, Y.: Dynamics of the ITCZ-equatorial cold tongue complex and causes of the latitudinal climate asymmetry, J. Climate, 12, 1830–1847, 1999. </reference>
		<reference numeration="136" content_type="text"> Wang, C. and Picaut, J.: Understanding ENSO physics – A review, in Earth&apos;s Climate: The Ocean-Atmosphere Interaction, AGU Geophys. Monogr. Ser., 147, 21–48, 2004. </reference>
		<reference numeration="137" content_type="text"> Wang, X., Auler, A. S., Edwards, R. L., Cheng, H., Cristalli, P. S., Smart, P. L., David, A., Richards, D. A., and Shen, C.-C.: Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies, Nature, 432, 740–743, 2004. </reference>
		<reference numeration="138" content_type="text"> Wells, M. L., Vallis, G. K., and Silver, E. A.: Tectonic Processes in Papua New Guinea and past productivity in the eastern equatorial Pacific Ocean, Nature, 398, 601–604, 1999. </reference>
		<reference numeration="139" content_type="text"> Wood, F.: Tidal dynamics, Reidel, Dordrecht, The Netherlands, 1986. </reference>
		<reference numeration="140" content_type="text"> Wyrtki, K. and Kilonsky, B.: Mean Water and Current Structure during the Hawaii-to-Tahiti Shuttle Experiment, J. Phys. Oceanogr., 14, 242–254, 1984. </reference>
		<reference numeration="141" content_type="text"> Wyrtki, K.: Water Displacements in the Pacific and the genesis of El Niño cycles, J. Geophys. Res., 90(C4), 7129–7130, 1985. </reference>
		<reference numeration="142" content_type="text"> Xie, S.-P. and Philander, S. G. H.: A coupled ocean-atmosphere model of relevance to the ITCZ in the eastern Pacific, Tellus~A, 46, 340–350, 1994. </reference>
		<reference numeration="143" content_type="text"> Xie, S.-P.: The shape of continents, air-sea interaction, and the rising branch of the Hadley Circulation, in: The Hadley Circulation: Present, Past and Future, edited by: Diaz, H. F. and Bradley, R. S., Kluwer Academic Publishers, The Netherlands, 121–152, 2005. </reference>
		<reference numeration="144" content_type="text"> Yu, X. and McPhaden, M. J.: Seasonal Variability in the Equatorial Pacific, J. Phys. Oceanogr., 29, 925–947, 1999. </reference>
		<reference numeration="145" content_type="text"> Yu, X. and McPhaden, M. J.: Dynamical Analysis of Seasonal and Interannual Variability in the Equatorial Pacific, J. Phys.l Oceanogr., 29, 2350–2369, 1999. </reference>
		<reference numeration="146" content_type="text"> Zachos, J., Pagani, M., Sloan, L., Thomas, E., and Billups, K.: Trends, rhythms, and aberrations in global climate 65 Ma to present, Science, 292, 686–693, 2001. </reference>
	</references>
</article>

