In 1963, Lorenz developed a simple math model for atmospheric convection.
— Fermat's Library (@fermatslibrary) March 8, 2018
x' = σ(y-x)
y' = x(ρ-z)-y
z' = xy-βz
The equations relate the properties of a 2D fluid layer uniformly warmed from below and cooled from above. Here is a set of chaotic solutions - The Lorenz attractor pic.twitter.com/LMlPKIIrlO
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March 08, 2018 at 05:43AM
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