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Article #205Re: Lorenz' Weather
From: Matt Kennel
Date: Mon, 16 Nov 1992 05:30
Date: Mon, 16 Nov 1992 05:30
54 lines
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2873 bytes
mroussel@alchemy.chem.utoronto.ca (Marc Roussel) writes: : > dX/dt = a(Y-X) : > dY/dt = bX-Y-XZ : > dZ/dt = XY - cZ : > : > where a = 10 : > c = 8/3 : > b = control parameter (try 28) : : These are indeed the Lorenz equations (as they are now known) but : these aren't the original weather simulation equations where Lorenz : noticed sensitive dependence on initial conditions. Lorenz actually : started out with some specialized version of the Navier-Stokes equation : (a PDE) and noticed sensitive dependence in these equations under the conditions : of his weather simulation. The Lorenz ODEs shown above are a truncation : of the Navier-Stokes equation for the special case of (I think) : Rayleigh-Benard convection under certain fairly restrictive conditions. There is a physical system for which the Lorenz equations are a "not incredibly bad" approximation (to use them for simple R-B convection is a "well that's really pretty cheezy" approximation). It's called a thermosyphon, and it actually gets used for some engineering applications but I don't know how really. Think of a loop of pipe in an 'O' standing up vertically, like a bicycle wheel, with fluid in the interior. Now, keep the walls on the bottom half of the "O" hot, and the walls on the top half cold. Given enough of a temperature difference, you can start to get convective motion of the fluid as it tries to transport heat from hot to cold. In this circumstance, the "X" variable is proportional to fluid velocity (in some complicated nondimensionalization), the Y and Z variables are coefficients sine and cosine modes of the temperature. "a" is the Prandtl number of the fluid (ratio of shear viscosity to thermal diffusivity), "b" is the Rayleigh number (proportional to temperature difference between hot and cold boundary conditions and other geometrical factors), and "c" is always one. : Lorenz cooked up these equations as a simple example of what he was : seeing in his more sophisticated weather models. : Marc R. Roussel : mroussel@alchemy.chem.utoronto.ca -- -Matt Kennel mbk@inls1.ucsd.edu -Institute for Nonlinear Science, University of California, San Diego -*** AD: Archive for nonlinear dynamics papers & programs: FTP to -*** lyapunov.ucsd.edu, username "anonymous".
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Path: arc1-ca.pugleaf.net!sparky!uunet!zaphod.mps.ohio-state.edu!wupost!emory!swrinde!network.ucsd.edu!lyapunov.ucsd.edu!mbk From: mbk@lyapunov.ucsd.edu (Matt Kennel) Newsgroups: sci.fractals Subject: Re: Lorenz' Weather Date: 16 Nov 1992 05:30:50 GMT Organization: Institute For Nonlinear Science, UCSD Lines: 54 Message-ID: <1e7bmaINNslq@network.ucsd.edu> References: <1992Nov12.201358.3135@alchemy.chem.utoronto.ca> NNTP-Posting-Host: lyapunov.ucsd.edu X-Newsreader: Tin 1.1 PL3