Nat. Hazards Earth Syst. Sci., 11, 383–399, 2011 www.nat-hazards-earth-syst-sci.netdoi:nhess © Author(sCC Attribution 3.0 License. Natural Hazards

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Date: 2014-12-04 01:55:38 Partial differential equations Ordinary differential equations Dynamical systems Nonlinear Schrödinger equation Wave Damped wave Damping Eigenvalues and eigenvectors Rogue wave Algebra Mathematics Calculus		Nat. Hazards Earth Syst. Sci., 11, 383–399, 2011 www.nat-hazards-earth-syst-sci.netdoi:nhess © Author(sCC Attribution 3.0 License. Natural Hazards Add to Reading List Source URL: www.nat-hazards-earth-syst-sci.net Download Document from Source Website File Size: 4,61 MB Share Document on Facebook

	Nat. Hazards Earth Syst. Sci., 11, 383–399, 2011 www.nat-hazards-earth-syst-sci.netdoi:nhess © Author(sCC Attribution 3.0 License. Natural Hazards DocID: 1aF5m - View Document
	Why does El Niño advance eastward? A schematic, eastward-propagating El Niño can be formulated in a steady, damped, linear system based on the Gill atmosphere and a single-active-layer ocean whose SST is related to the DocID: 107zT - View Document
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