Impacts of ocean gateway and basin width on Tertiary tropical climate variability in a prototype model
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An S-I (2011) Atmospheric responses of Gill-type and Lindzen-Nigam models to global warming. J Clim. doi: 10.1175/2011JCLI3971.1
An S-I, Jin F-F (2000) An eigen analysis of the interdecadal changes in the structure and frequency of ENSO mode. Geophys Res Lett 27:1573–1576
Battisti DS, Hirst AC (1989) Interannual variability in the tropical atmosphere/ocean system: influence of the basic state and ocean geometry. J Atmos Sci 46:1687–1712
Bice KL, Marotzke J (2001) Numerical evidence against reversed thermohaline circulation in the warm Paleocene/Eocene ocean. J Geophys Res 106:11529–11542
Bjerknes J (1966) A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature. Tellus 18:820–829
Cannariato KG, Ravelo AC (1997) Pliocene–Pleistocene evolution of eastern tropical Pacific surface water circulation and thermocline depth. Paleoceanography 12:805–820
Chaisson WP, Ravelo AC (2000) Pliocene development of the east–west hydrographic gradient in the equatorial Pacific. Paleoceanography 15:497–505
Haug GH, Tiedemann R, Zahn R, Ravelo AC (2001) Role of Panama uplift on oceanic freshwater balance. Geology 29:207–210
Heinemann M, Jungclaus JH, Marotzke J (2009) Warm Paleocene/Eocene climate as simulated in ECHAM5/MPI-OM. Clim Past 5:785–802
Jian Z, Yu Y, Li B, Wang J, Zhang X, Zhou Z (2006) Phased evolution of the south-north hydrographic gradient in the South China Sea since the middle Miocene. Palaeogeogr Palaeoclimatol Palaeoecol 230:251–263
Jin F-F (1997) An equatorial ocean recharge paradigm for ENSO. Part I: Conceptual model. J Atmos Sci 54:811–829
Klocker A, Prange M, Schulz M (2005) Testing the influence of the central american seaway on orbitally forced Northern Hemisphere glaciation. Geophy Res Lett 32:L03703. doi: 10.1029/2004GL021564
Li Q, Li B, Zhong G, McGowran B, Zhou Z, Wang J, Wang P (2006) Late Miocene development of the western Pacific warm pool: planktonic foraminifer and oxygen isotopic evidence. Palaeogeogr Palaeoclimatol Palaeoecol 237:465–482
Lindzen RS, Nigam S (1987) On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics. J Atmos Sci 44:2418–2436
Maier-Reimerm E, Mikolajewicz U, Crowley T (1990) Ocean general circulation model sensitivity experiment with an open Central American Isthmus. Paleoceanography 5:349–366
Ruddiman WF (2008) Earth’s Climate Past and Future, 2nd edn. W H Freeman and Company, New York, p 388
Sato K, Oda M, Chiyonobu S, Kimoto K, Domitsu H, Ingle JC Jr (2008) Establishment of the western Pacific warm pool during the Pliocene: Evidence from planktonic foraminifera, oxygen isotopes, and Mg/Ca ratios. Palaeogeogr Palaeoclimatol Palaeoecol 265:140–147
Step et al (2007) Early Pliocene increase in thermocline overturning preconditioned the development of the modern equatorial Pacific cold tongue. submitted to J Climate
Steph S, Tiedemann R, Groeneveld J, Sturm A, Nürnberg D (2006) Plioecne changes in tropical east Pacific upper ocean stratification: response to tropical gateway. In: Tiedemann R, Mix AC, Richter C, Ruddiman WE (eds) Proceedings of theOcean Drilling Program. Scientific Results. Ocean Drilling Program, College Station, pp 1–51
Timm O, Timmermann A (2007) Simulation of the last 21000 years using accelerated transient boundary conditions. J Clim 20:4377–4401