var stein_okal05 = "S. Stein, E. A. Okal, Nature 434, 581 (2005).";
var bilham05 = "R. Bilham, Science 308, 1126 (2005).";
var subarya_etal05 = "C. Subarya et al., Eos Trans. AGU 86, U51A (2005).";
var note4 = "The Cocos Islands gauge is maintained by the National Tidal Centre of the Australian Bureau of Meteorology.";
var liu_etal05 = "P. Liu et al., Science 308, 1595 (2005).";
var titov_synolakis97 = "V. V. Titov, C. E. Synolakis, Geophys. Res. Lett. 24, 1315 (1997).";
var note7 = "Here, we use "amplitude-sensitive" tsunami arrival time estimation because it is more accurate than travel-time algorithms that do not take into account wave amplitude. The tsunami travel times contoured in Fig. 1 are inferred from arrival times for the smallest waves simulated by the MOST tsunami propagation model. The areas without contours delineate regions where arrival times are difficult to estimate because waves of similar small amplitudes arrive at different times from different "packets" and from prolonged wave trains. This creates multivalue arrival times for some locations, reflecting the difficulties in determining tsunami arrival at tide-gauge records with small initial wave amplitudes.";
var gower05 = "J. Gower, Eos 86, 37 (2005).";
var smith_etal05 = "W. Smith, R. Scharroo, V. Titov, D. Arcas, B. Arbic, Oceanography 18, 10 (2005).";
var titov_synolakis98 = "V. V. Titov, C. E. Synolakis, J. Waterways Ports Coastal Ocean Eng. 124, 57 (1998).";
var ammon_etal05 = "C. J. Ammon et al., Science 308, 1133 (2005).";
var hirata_inprep = "K. Hirata, in preparation.";
var titov_etal01 = "V. V. Titov, H. O. Mofjeld, F. I. González, J. C. Newman, in Tsunami Research at the End of a Critical Decade, G. T. Hebenstreit, Ed. (Kluwer Academic Publishers, Amsterdam, 2001), pp. 75–90.";
var note14 = "At the time of the initial simulation, the preliminary estimate of the earthquake magnitude was M![\"\"](\"/pubs/greek/subW.gif\")
= 8.5, representing a release of energy lower by a factor of 16 than the final estimate of M = 9.3. The only direct tsunami measurement available was for the Cocos Islands. This record provided the initial scaling for the initial specification of the tsunami source, modeled as the instantaneous seafloor deformation of the aftershock area, corresponding to a 1200-km-long rupture along the Sunda Trench. This initial tsunami source length and the resulting magnitude differed substantially from the much shorter rupture length and lower magnitude indicated by the preliminary seismic analysis. However, the resulting model simulations agreed qualitatively with the early tsunami observations. Later seismic analyses [Ammon et al., 2005] have confirmed the larger earthquake magnitude and source region.";
var marchuk_titov89 = "An. G. Marchuk, V. V. Titov, in Proc. IUGG/IOC International Tsunami Symposium, Novosibirsk, USSR (1989), pp. 11–17.";
var koshimura_etal99 = "S. Koshimura, F. Imamura, N. Shuto, Coastal Eng. J. 41, 167 (1999).";
var gonzalez_etal95 = "F. I. Gonza´lez, K. Satake, E. F. Boss, H. O. Mofjeld, Pure Appl. Geophys. 144, 409 (1995).";
var note18 = "Sea-level records for Dumont d'Urville are available as part of the French ROSAME (Réseau d'Observation Sub-antartique et Antartique du niveau de la Mer) Antarctica and South Indian Ocean Tide Gauge Network. Plots for the tsunami arrival on 26 December 2004, were provided by Laurent Testut (Laurent.Testut@notos.cst.cnes.fr).";
var note19 = "Here, "near field" for this major tsunami encompasses almost all of the Indian Ocean.";
var note20 = "Wavelet transforms determine the variation in signal intensity within a hierarchy of frequency bands as a function of time [Emery and Thomson, 2001].";
var emery_thomson01 = "W. J. Emery, R. E. Thomson, Data Analysis Methods in Physical Oceanography (Elsevier Science, ed. 2, Amsterdam, 2001).";