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Edward Norton Lorenz

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Edward Norton Lorenz (May 23, 1917 – April 16, 2008) was an American mathematician and meteorologist who established the theoretical basis of weather and climate predictability , as well as the basis for computer-aided atmospheric physics and meteorology . He is best known as the founder of modern chaos theory , a branch of mathematics focusing on the behavior of dynamical systems that are highly sensitive to initial conditions .

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106-592: His discovery of deterministic chaos "profoundly influenced a wide range of basic sciences and brought about one of the most dramatic changes in mankind's view of nature since Sir Isaac Newton," according to the committee that awarded him the 1991 Kyoto Prize for basic sciences in the field of earth and planetary sciences. Lorenz was born in 1917 in West Hartford, Connecticut . He acquired an early love of science from both sides of his family. His father, Edward Henry Lorenz (1882-1956), majored in mechanical engineering at

212-485: A polynomial equation such as x 2 + x − 1 = 0. {\displaystyle x^{2}+x-1=0.} The general root-finding algorithms apply to polynomial roots, but, generally they do not find all the roots, and when they fail to find a root, this does not imply that there is no roots. Specific methods for polynomials allow finding all roots or the real roots; see real-root isolation . Solving systems of polynomial equations , that

318-444: A K-system . A chaotic system may have sequences of values for the evolving variable that exactly repeat themselves, giving periodic behavior starting from any point in that sequence. However, such periodic sequences are repelling rather than attracting, meaning that if the evolving variable is outside the sequence, however close, it will not enter the sequence and in fact, will diverge from it. Thus for almost all initial conditions,

424-467: A linear map (or linear function ) f ( x ) {\displaystyle f(x)} is one which satisfies both of the following properties: Additivity implies homogeneity for any rational α , and, for continuous functions , for any real α . For a complex α , homogeneity does not follow from additivity. For example, an antilinear map is additive but not homogeneous. The conditions of additivity and homogeneity are often combined in

530-524: A nonlinear system (or a non-linear system ) is a system in which the change of the output is not proportional to the change of the input. Nonlinear problems are of interest to engineers , biologists , physicists , mathematicians , and many other scientists since most systems are inherently nonlinear in nature. Nonlinear dynamical systems , describing changes in variables over time, may appear chaotic, unpredictable, or counterintuitive, contrasting with much simpler linear systems . Typically,

636-1343: A classic of chaos theory. Non-linear Collective intelligence Collective action Self-organized criticality Herd mentality Phase transition Agent-based modelling Synchronization Ant colony optimization Particle swarm optimization Swarm behaviour Social network analysis Small-world networks Centrality Motifs Graph theory Scaling Robustness Systems biology Dynamic networks Evolutionary computation Genetic algorithms Genetic programming Artificial life Machine learning Evolutionary developmental biology Artificial intelligence Evolutionary robotics Reaction–diffusion systems Partial differential equations Dissipative structures Percolation Cellular automata Spatial ecology Self-replication Conversation theory Entropy Feedback Goal-oriented Homeostasis Information theory Operationalization Second-order cybernetics Self-reference System dynamics Systems science Systems thinking Sensemaking Variety Ordinary differential equations Phase space Attractors Population dynamics Chaos Multistability Bifurcation Rational choice theory Bounded rationality In mathematics and science ,

742-418: A coastline's length varies with the scale of the measuring instrument, resembles itself at all scales, and is infinite in length for an infinitesimally small measuring device. Arguing that a ball of twine appears as a point when viewed from far away (0-dimensional), a ball when viewed from fairly near (3-dimensional), or a curved strand (1-dimensional), he argued that the dimensions of an object are relative to

848-483: A concrete experiment. And Boris Chirikov himself is considered as a pioneer in classical and quantum chaos. The main catalyst for the development of chaos theory was the electronic computer. Much of the mathematics of chaos theory involves the repeated iteration of simple mathematical formulas, which would be impractical to do by hand. Electronic computers made these repeated calculations practical, while figures and images made it possible to visualize these systems. As

954-524: A dual nature of chaos and order with distinct predictability", in contrast to the conventional view of "weather is chaotic". Discrete chaotic systems, such as the logistic map , can exhibit strange attractors whatever their dimensionality . In contrast, for continuous dynamical systems, the Poincaré–Bendixson theorem shows that a strange attractor can only arise in three or more dimensions. Finite-dimensional linear systems are never chaotic; for

1060-481: A dynamical system to display chaotic behavior, it must be either nonlinear or infinite-dimensional. The Poincaré–Bendixson theorem states that a two-dimensional differential equation has very regular behavior. The Lorenz attractor discussed below is generated by a system of three differential equations such as: where x {\displaystyle x} , y {\displaystyle y} , and z {\displaystyle z} make up

1166-505: A few days (unproven); the inner solar system, 4 to 5 million years. In chaotic systems, the uncertainty in a forecast increases exponentially with elapsed time. Hence, mathematically, doubling the forecast time more than squares the proportional uncertainty in the forecast. This means, in practice, a meaningful prediction cannot be made over an interval of more than two or three times the Lyapunov time. When meaningful predictions cannot be made,

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1272-406: A fourth or higher derivative are called accordingly hyperjerk systems. A jerk system's behavior is described by a jerk equation, and for certain jerk equations, simple electronic circuits can model solutions. These circuits are known as jerk circuits. One of the most interesting properties of jerk circuits is the possibility of chaotic behavior. In fact, certain well-known chaotic systems, such as

1378-423: A frictionless pendulum under the influence of gravity . Using Lagrangian mechanics , it may be shown that the motion of a pendulum can be described by the dimensionless nonlinear equation where gravity points "downwards" and θ {\displaystyle \theta } is the angle the pendulum forms with its rest position, as shown in the figure at right. One approach to "solving" this equation

1484-622: A graduate student in Chihiro Hayashi's laboratory at Kyoto University, Yoshisuke Ueda was experimenting with analog computers and noticed, on November 27, 1961, what he called "randomly transitional phenomena". Yet his advisor did not agree with his conclusions at the time, and did not allow him to report his findings until 1970. Edward Lorenz was an early pioneer of the theory. His interest in chaos came about accidentally through his work on weather prediction in 1961. Lorenz and his collaborator Ellen Fetter and Margaret Hamilton were using

1590-507: A reasonable degree of accuracy. However, the recognition of chaos has led to improvements in weather forecasting , as now forecasters recognize that measurements are imperfect and thus run many simulations starting from slightly different conditions, called ensemble forecasting . Of the seminal significance of Lorenz's work, Kerry Emanuel , a prominent meteorologist and climate scientist at MIT, has stated: "By showing that certain deterministic systems have formal predictability limits, Ed put

1696-449: A sequence of data again, and to save time he started the simulation in the middle of its course. He did this by entering a printout of the data that corresponded to conditions in the middle of the original simulation. To his surprise, the weather that the machine began to predict was completely different from the previous calculation. The culprit: a rounded decimal number on the computer printout. The computer worked with 6-digit precision, but

1802-412: A simple digital computer, a Royal McBee LGP-30 , to run weather simulations. They wanted to see a sequence of data again, and to save time they started the simulation in the middle of its course. They did this by entering a printout of the data that corresponded to conditions in the middle of the original simulation. To their surprise, the weather the machine began to predict was completely different from

1908-494: A symposium, named MIT on Chaos and Climate, in honor of the 100th anniversary of the birth of Lorenz and Charney . The two-day event featured presentations from world-renowned experts on the many scientific contributions that the two pioneers made on the fields of numerical weather prediction , physical oceanography , atmospheric dynamics , and experimental fluid dynamics , as well as the personal legacy they left behind of integrity, optimism, and collaboration. A video produced for

2014-428: A unique evolution and is fully determined by their initial conditions, with no random elements involved. In other words, the deterministic nature of these systems does not make them predictable. This behavior is known as deterministic chaos , or simply chaos . The theory was summarized by Edward Lorenz as: Chaos: When the present determines the future but the approximate present does not approximately determine

2120-472: A variety of disciplines, including meteorology , anthropology , sociology , environmental science , computer science , engineering , economics , ecology , and pandemic crisis management . The theory formed the basis for such fields of study as complex dynamical systems , edge of chaos theory and self-assembly processes. Chaos theory concerns deterministic systems whose behavior can, in principle, be predicted. Chaotic systems are predictable for

2226-410: A week ahead. This does not mean that one cannot assert anything about events far in the future—only that some restrictions on the system are present. For example, we know that the temperature of the surface of the earth will not naturally reach 100 °C (212 °F) or fall below −130 °C (−202 °F) on earth (during the current geologic era ), but we cannot predict exactly which day will have

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2332-504: A while and then 'appear' to become random. The amount of time for which the behavior of a chaotic system can be effectively predicted depends on three things: how much uncertainty can be tolerated in the forecast, how accurately its current state can be measured, and a time scale depending on the dynamics of the system, called the Lyapunov time . Some examples of Lyapunov times are: chaotic electrical circuits, about 1 millisecond; weather systems,

2438-881: Is a second countable , complete metric space , then topological transitivity implies the existence of a dense set of points in X that have dense orbits. For a chaotic system to have dense periodic orbits means that every point in the space is approached arbitrarily closely by periodic orbits. The one-dimensional logistic map defined by x → 4 x (1 – x ) is one of the simplest systems with density of periodic orbits. For example, 5 − 5 8 {\displaystyle {\tfrac {5-{\sqrt {5}}}{8}}}  → 5 + 5 8 {\displaystyle {\tfrac {5+{\sqrt {5}}}{8}}}  → 5 − 5 8 {\displaystyle {\tfrac {5-{\sqrt {5}}}{8}}} (or approximately 0.3454915 → 0.9045085 → 0.3454915)

2544-637: Is a simple harmonic oscillator corresponding to oscillations of the pendulum near the bottom of its path. Another linearization would be at θ = π {\displaystyle \theta =\pi } , corresponding to the pendulum being straight up: since sin ⁡ ( θ ) ≈ π − θ {\displaystyle \sin(\theta )\approx \pi -\theta } for θ ≈ π {\displaystyle \theta \approx \pi } . The solution to this problem involves hyperbolic sinusoids , and note that unlike

2650-427: Is a spontaneous order. The essence here is that most orders in nature arise from the spontaneous breakdown of various symmetries. This large family of phenomena includes elasticity, superconductivity, ferromagnetism, and many others. According to the supersymmetric theory of stochastic dynamics , chaos, or more precisely, its stochastic generalization, is also part of this family. The corresponding symmetry being broken

2756-562: Is a weaker version of topological mixing . Intuitively, if a map is topologically transitive then given a point x and a region V , there exists a point y near x whose orbit passes through V . This implies that it is impossible to decompose the system into two open sets. An important related theorem is the Birkhoff Transitivity Theorem. It is easy to see that the existence of a dense orbit implies topological transitivity. The Birkhoff Transitivity Theorem states that if X

2862-431: Is always useful whether or not the resulting ordinary differential equation(s) is solvable. Another common (though less mathematical) tactic, often exploited in fluid and heat mechanics, is to use scale analysis to simplify a general, natural equation in a certain specific boundary value problem . For example, the (very) nonlinear Navier-Stokes equations can be simplified into one linear partial differential equation in

2968-486: Is an (unstable) orbit of period 2, and similar orbits exist for periods 4, 8, 16, etc. (indeed, for all the periods specified by Sharkovskii's theorem ). Sharkovskii's theorem is the basis of the Li and Yorke (1975) proof that any continuous one-dimensional system that exhibits a regular cycle of period three will also display regular cycles of every other length, as well as completely chaotic orbits. Some dynamical systems, like

3074-746: Is an example of a chaotic system. Topological mixing is often omitted from popular accounts of chaos, which equate chaos with only sensitivity to initial conditions. However, sensitive dependence on initial conditions alone does not give chaos. For example, consider the simple dynamical system produced by repeatedly doubling an initial value. This system has sensitive dependence on initial conditions everywhere, since any pair of nearby points eventually becomes widely separated. However, this example has no topological mixing, and therefore has no chaos. Indeed, it has extremely simple behavior: all points except 0 tend to positive or negative infinity. A map f : X → X {\displaystyle f:X\to X}

3180-798: Is based upon convolution integral which mediates interaction between spatially distributed maps: ψ n + 1 ( r → , t ) = ∫ K ( r → − r → , , t ) f [ ψ n ( r → , , t ) ] d r → , {\displaystyle \psi _{n+1}({\vec {r}},t)=\int K({\vec {r}}-{\vec {r}}^{,},t)f[\psi _{n}({\vec {r}}^{,},t)]d{\vec {r}}^{,}} , where kernel K ( r → − r → , , t ) {\displaystyle K({\vec {r}}-{\vec {r}}^{,},t)}

3286-508: Is being developed in a branch of mathematical analysis known as functional analysis . The above set of three ordinary differential equations has been referred to as the three-dimensional Lorenz model. Since 1963, higher-dimensional Lorenz models have been developed in numerous studies for examining the impact of an increased degree of nonlinearity, as well as its collective effect with heating and dissipations, on solution stability. The straightforward generalization of coupled discrete maps

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3392-432: Is finding the common zeros of a set of several polynomials in several variables is a difficult problem for which elaborated algorithms have been designed, such as Gröbner base algorithms. For the general case of system of equations formed by equating to zero several differentiable functions , the main method is Newton's method and its variants. Generally they may provide a solution, but do not provide any information on

3498-448: Is generated by the Rössler equations , which have only one nonlinear term out of seven. Sprott found a three-dimensional system with just five terms, that had only one nonlinear term, which exhibits chaos for certain parameter values. Zhang and Heidel showed that, at least for dissipative and conservative quadratic systems, three-dimensional quadratic systems with only three or four terms on

3604-552: Is one-dimensional heat transport with Dirichlet boundary conditions , the solution of which can be written as a time-dependent linear combination of sinusoids of differing frequencies; this makes solutions very flexible. It is often possible to find several very specific solutions to nonlinear equations, however the lack of a superposition principle prevents the construction of new solutions. First order ordinary differential equations are often exactly solvable by separation of variables , especially for autonomous equations. For example,

3710-497: Is propagator derived as Green function of a relevant physical system, f [ ψ n ( r → , t ) ] {\displaystyle f[\psi _{n}({\vec {r}},t)]} might be logistic map alike ψ → G ψ [ 1 − tanh ⁡ ( ψ ) ] {\displaystyle \psi \rightarrow G\psi [1-\tanh(\psi )]} or complex map . For examples of complex maps

3816-424: Is said to be topologically transitive if for any pair of non-empty open sets U , V ⊂ X {\displaystyle U,V\subset X} , there exists k > 0 {\displaystyle k>0} such that f k ( U ) ∩ V ≠ ∅ {\displaystyle f^{k}(U)\cap V\neq \emptyset } . Topological transitivity

3922-567: Is that a butterfly flapping its wings in Brazil can cause a tornado in Texas . Small differences in initial conditions, such as those due to errors in measurements or due to rounding errors in numerical computation , can yield widely diverging outcomes for such dynamical systems, rendering long-term prediction of their behavior impossible in general. This can happen even though these systems are deterministic , meaning that their future behavior follows

4028-409: Is the topological supersymmetry which is hidden in all stochastic (partial) differential equations , and the corresponding order parameter is a field-theoretic embodiment of the butterfly effect. James Clerk Maxwell first emphasized the " butterfly effect ", and is seen as being one of the earliest to discuss chaos theory, with work in the 1860s and 1870s. An early proponent of chaos theory

4134-438: Is the third derivative of position , with respect to time. As such, differential equations of the form are sometimes called jerk equations . It has been shown that a jerk equation, which is equivalent to a system of three first order, ordinary, non-linear differential equations, is in a certain sense the minimal setting for solutions showing chaotic behavior. This motivates mathematical interest in jerk systems. Systems involving

4240-462: Is to start with a point in the basin of attraction of the attractor, and then simply plot its subsequent orbit. Because of the topological transitivity condition, this is likely to produce a picture of the entire final attractor, and indeed both orbits shown in the figure on the right give a picture of the general shape of the Lorenz attractor. This attractor results from a simple three-dimensional model of

4346-480: Is to use d θ / d t {\displaystyle d\theta /dt} as an integrating factor , which would eventually yield which is an implicit solution involving an elliptic integral . This "solution" generally does not have many uses because most of the nature of the solution is hidden in the nonelementary integral (nonelementary unless C 0 = 2 {\displaystyle C_{0}=2} ). Another way to approach

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4452-511: Is very general in that x {\displaystyle x} can be any sensible mathematical object (number, vector, function, etc.), and the function f ( x ) {\displaystyle f(x)} can literally be any mapping , including integration or differentiation with associated constraints (such as boundary values ). If f ( x ) {\displaystyle f(x)} contains differentiation with respect to x {\displaystyle x} ,

4558-713: The Julia set f [ ψ ] = ψ 2 {\displaystyle f[\psi ]=\psi ^{2}} or Ikeda map ψ n + 1 = A + B ψ n e i ( | ψ n | 2 + C ) {\displaystyle \psi _{n+1}=A+B\psi _{n}e^{i(|\psi _{n}|^{2}+C)}} may serve. When wave propagation problems at distance L = c t {\displaystyle L=ct} with wavelength λ = 2 π / k {\displaystyle \lambda =2\pi /k} are considered

4664-608: The Lorenz weather system. The Lorenz attractor is perhaps one of the best-known chaotic system diagrams, probably because it is not only one of the first, but it is also one of the most complex, and as such gives rise to a very interesting pattern that, with a little imagination, looks like the wings of a butterfly. Unlike fixed-point attractors and limit cycles , the attractors that arise from chaotic systems, known as strange attractors , have great detail and complexity. Strange attractors occur in both continuous dynamical systems (such as

4770-557: The Massachusetts Institute of Technology , and his maternal grandfather, Lewis M. Norton , developed the first course in chemical engineering at MIT in 1888. Meanwhile, his mother, Grace Peloubet Norton (1887-1943), instilled in Lorenz a deep interest in games, particularly chess. Later in life, Lorenz lived in Cambridge, Massachusetts with his wife, Jane Loban (1919–2001), and their three children, Nancy, Cheryl, and Edward. He

4876-529: The Navier–Stokes equations in fluid dynamics and the Lotka–Volterra equations in biology. One of the greatest difficulties of nonlinear problems is that it is not generally possible to combine known solutions into new solutions. In linear problems, for example, a family of linearly independent solutions can be used to construct general solutions through the superposition principle . A good example of this

4982-634: The Swedish Academy of Sciences , considered to be nearly equal to a Nobel Prize . He was also awarded the Kyoto Prize for basic sciences in the field of earth and planetary sciences in 1991, the Buys Ballot Award in 2004, and the Tomassoni Award in 2008. In 2018, a short documentary was made about Lorenz's immense scientific legacy on everything from how we predict weather to our understanding of

5088-613: The United States Army Air Forces during World War II , leading him to pursue graduate studies in meteorology at the Massachusetts Institute of Technology . He earned both a master's and doctoral degree in meteorology from MIT in 1943 and 1948. His doctoral dissertation, titled "A Method of Applying the Hydrodynamic and Thermodynamic Equations to Atmospheric Models" and performed under advisor James Murdoch Austin , described an application of fluid dynamical equations to

5194-425: The system state , t {\displaystyle t} is time, and σ {\displaystyle \sigma } , ρ {\displaystyle \rho } , β {\displaystyle \beta } are the system parameters . Five of the terms on the right hand side are linear, while two are quadratic; a total of seven terms. Another well-known chaotic attractor

5300-728: The " butterfly effect ", so-called because of the title of a paper given by Edward Lorenz in 1972 to the American Association for the Advancement of Science in Washington, D.C., entitled Predictability: Does the Flap of a Butterfly's Wings in Brazil set off a Tornado in Texas? . The flapping wing represents a small change in the initial condition of the system, which causes a chain of events that prevents

5406-444: The Lorenz attractor and the Rössler map , are conventionally described as a system of three first-order differential equations that can combine into a single (although rather complicated) jerk equation. Another example of a jerk equation with nonlinearity in the magnitude of x {\displaystyle x} is: Here, A is an adjustable parameter. This equation has a chaotic solution for A =3/5 and can be implemented with

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5512-565: The Lorenz system) and in some discrete systems (such as the Hénon map ). Other discrete dynamical systems have a repelling structure called a Julia set , which forms at the boundary between basins of attraction of fixed points. Julia sets can be thought of as strange repellers. Both strange attractors and Julia sets typically have a fractal structure, and the fractal dimension can be calculated for them. In contrast to single type chaotic solutions, recent studies using Lorenz models have emphasized

5618-618: The MIT Department of Meteorology and Physical Oceanography merged with the Department of Geology to become the current MIT Department of Earth, Atmospheric and Planetary Sciences, where Lorenz remained a professor before becoming an emeritus professor in 1987. In the late 1940s and early 1950s, Lorenz worked with Victor Starr on the General Circulation Project at MIT to understand the role the weather system played in determining

5724-400: The above list. Sensitivity to initial conditions means that each point in a chaotic system is arbitrarily closely approximated by other points that have significantly different future paths or trajectories. Thus, an arbitrarily small change or perturbation of the current trajectory may lead to significantly different future behavior. Sensitivity to initial conditions is popularly known as

5830-476: The apparent randomness of chaotic complex systems , there are underlying patterns, interconnection, constant feedback loops , repetition, self-similarity , fractals and self-organization . The butterfly effect , an underlying principle of chaos, describes how a small change in one state of a deterministic nonlinear system can result in large differences in a later state (meaning there is sensitive dependence on initial conditions). A metaphor for this behavior

5936-424: The behavior of a nonlinear system is described in mathematics by a nonlinear system of equations , which is a set of simultaneous equations in which the unknowns (or the unknown functions in the case of differential equations ) appear as variables of a polynomial of degree higher than one or in the argument of a function which is not a polynomial of degree one. In other words, in a nonlinear system of equations,

6042-476: The benefit of a theory to explain what they were seeing. Despite initial insights in the first half of the twentieth century, chaos theory became formalized as such only after mid-century, when it first became evident to some scientists that linear theory , the prevailing system theory at that time, simply could not explain the observed behavior of certain experiments like that of the logistic map . What had been attributed to measure imprecision and simple " noise "

6148-490: The book "The Essence of Chaos," in the chapter "Our Chaotic Weather" from 1993, authored by Edward Lorenz and Krzysztof Haman , the authors delved into the challenges of weather forecasting. The work discusses the consequences of chaos in the atmosphere and its impact on weather prediction. They describe a scenario in which meteorologists, in the computer age, generate multiple long-term weather forecasts based on different yet similar initial atmospheric conditions. Differences in

6254-404: The case of transient, laminar, one dimensional flow in a circular pipe; the scale analysis provides conditions under which the flow is laminar and one dimensional and also yields the simplified equation. Other methods include examining the characteristics and using the methods outlined above for ordinary differential equations. A classic, extensively studied nonlinear problem is the dynamics of

6360-421: The discrete-time case, this is true for all continuous maps on metric spaces . In these cases, while it is often the most practically significant property, "sensitivity to initial conditions" need not be stated in the definition. If attention is restricted to intervals , the second property implies the other two. An alternative and a generally weaker definition of chaos uses only the first two properties in

6466-673: The energetics of the general circulation of the atmosphere. From this work, in 1967, Lorenz published a landmark paper, titled "The Nature and Theory of the General Circulation of the Atmosphere," on atmospheric circulation from an energetic perspective, which advanced the concept of available potential energy . In the 1950s, Lorenz became interested in and started work on numerical weather prediction , which relied on computers to forecast weather by processing observational data on such things as temperature, pressure, and wind. This interest

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6572-580: The equation is not a linear function of u {\displaystyle u} and its derivatives. Note that if the u 2 {\displaystyle u^{2}} term were replaced with u {\displaystyle u} , the problem would be linear (the exponential decay problem). Second and higher order ordinary differential equations (more generally, systems of nonlinear equations) rarely yield closed-form solutions, though implicit solutions and solutions involving nonelementary integrals are encountered. Common methods for

6678-627: The equation(s) to be solved cannot be written as a linear combination of the unknown variables or functions that appear in them. Systems can be defined as nonlinear, regardless of whether known linear functions appear in the equations. In particular, a differential equation is linear if it is linear in terms of the unknown function and its derivatives, even if nonlinear in terms of the other variables appearing in it. As nonlinear dynamical equations are difficult to solve, nonlinear systems are commonly approximated by linear equations ( linearization ). This works well up to some accuracy and some range for

6784-852: The event highlights the indelible mark made by Charney and Lorenz on MIT and the field of meteorology as a whole. Lorenz published many books and articles, a selection of which can be found below. A more complete list can be found on the Lorenz Center website: link Archived 2019-04-05 at the Wayback Machine Deterministic chaos Chaos theory (or chaology ) is an interdisciplinary area of scientific study and branch of mathematics . It focuses on underlying patterns and deterministic laws of dynamical systems that are highly sensitive to initial conditions . These were once thought to have completely random states of disorder and irregularities. Chaos theory states that within

6890-480: The following jerk circuit; the required nonlinearity is brought about by the two diodes: In the above circuit, all resistors are of equal value, except R A = R / A = 5 R / 3 {\displaystyle R_{A}=R/A=5R/3} , and all capacitors are of equal size. The dominant frequency is 1 / 2 π R C {\displaystyle 1/2\pi RC} . The output of op amp 0 will correspond to

6996-419: The forecast results arise due to the sensitivity of the system to initial conditions. Lorenz's insights on deterministic chaos resonated widely starting in the 1970s and 80s, when it spurred new fields of study in virtually every branch of science, from biology to geology to physics. In meteorology, it led to the conclusion that it may be fundamentally impossible to predict weather beyond two or three weeks with

7102-429: The future. Chaotic behavior exists in many natural systems, including fluid flow, heartbeat irregularities, weather and climate. It also occurs spontaneously in some systems with artificial components, such as road traffic . This behavior can be studied through the analysis of a chaotic mathematical model or through analytical techniques such as recurrence plots and Poincaré maps . Chaos theory has applications in

7208-453: The hottest temperature of the year. In more mathematical terms, the Lyapunov exponent measures the sensitivity to initial conditions, in the form of rate of exponential divergence from the perturbed initial conditions. More specifically, given two starting trajectories in the phase space that are infinitesimally close, with initial separation δ Z 0 {\displaystyle \delta \mathbf {Z} _{0}} ,

7314-408: The importance of considering various types of solutions. For example, coexisting chaotic and non-chaotic may appear within the same model (e.g., the double pendulum system) using the same modeling configurations but different initial conditions. The findings of attractor coexistence, obtained from classical and generalized Lorenz models, suggested a revised view that "the entirety of weather possesses

7420-458: The input values, but some interesting phenomena such as solitons , chaos , and singularities are hidden by linearization. It follows that some aspects of the dynamic behavior of a nonlinear system can appear to be counterintuitive, unpredictable or even chaotic. Although such chaotic behavior may resemble random behavior, it is in fact not random. For example, some aspects of the weather are seen to be chaotic, where simple changes in one part of

7526-692: The kernel K {\displaystyle K} may have a form of Green function for Schrödinger equation :. K ( r → − r → , , L ) = i k exp ⁡ [ i k L ] 2 π L exp ⁡ [ i k | r → − r → , | 2 2 L ] {\displaystyle K({\vec {r}}-{\vec {r}}^{,},L)={\frac {ik\exp[ikL]}{2\pi L}}\exp[{\frac {ik|{\vec {r}}-{\vec {r}}^{,}|^{2}}{2L}}]} . In physics , jerk

7632-531: The last nail in the coffin of the Cartesian universe and fomented what some have called the third scientific revolution of the 20th century, following on the heels of relativity and quantum physics." Late in his career, Lorenz began to be recognized with international accolades for the importance of his work on deterministic chaos. In 1983, along with colleague Henry Stommel , he was awarded the Crafoord Prize from

7738-478: The late 1950s, Lorenz was skeptical of the appropriateness of the linear statistical models in meteorology, as most atmospheric phenomena involved in weather forecasting are non-linear . It was during this time that his discovery of deterministic chaos came about. In 1961, Lorenz was using a simple digital computer, a Royal McBee LGP-30 , to simulate weather patterns by modeling 12 variables, representing things like temperature and wind speed. He wanted to see

7844-408: The nonlinear equation has u = 1 x + C {\displaystyle u={\frac {1}{x+C}}} as a general solution (and also the special solution u = 0 , {\displaystyle u=0,} corresponding to the limit of the general solution when C tends to infinity). The equation is nonlinear because it may be written as and the left-hand side of

7950-511: The number of solutions. A nonlinear recurrence relation defines successive terms of a sequence as a nonlinear function of preceding terms. Examples of nonlinear recurrence relations are the logistic map and the relations that define the various Hofstadter sequences . Nonlinear discrete models that represent a wide class of nonlinear recurrence relationships include the NARMAX (Nonlinear Autoregressive Moving Average with eXogenous inputs) model and

8056-560: The observer and may be fractional. An object whose irregularity is constant over different scales ("self-similarity") is a fractal (examples include the Menger sponge , the Sierpiński gasket , and the Koch curve or snowflake , which is infinitely long yet encloses a finite space and has a fractal dimension of circa 1.2619). In 1982, Mandelbrot published The Fractal Geometry of Nature , which became

8162-408: The one-dimensional logistic map defined by x → 4 x (1 – x ), are chaotic everywhere, but in many cases chaotic behavior is found only in a subset of phase space. The cases of most interest arise when the chaotic behavior takes place on an attractor , since then a large set of initial conditions leads to orbits that converge to this chaotic region. An easy way to visualize a chaotic attractor

8268-416: The onset of SDIC (i.e., prior to significant separations of initial nearby trajectories). A consequence of sensitivity to initial conditions is that if we start with a limited amount of information about the system (as is usually the case in practice), then beyond a certain time, the system would no longer be predictable. This is most prevalent in the case of weather, which is generally predictable only about

8374-504: The phase space, though it is common to just refer to the largest one. For example, the maximal Lyapunov exponent (MLE) is most often used, because it determines the overall predictability of the system. A positive MLE is usually taken as an indication that the system is chaotic. In addition to the above property, other properties related to sensitivity of initial conditions also exist. These include, for example, measure-theoretical mixing (as discussed in ergodic theory) and properties of

8480-426: The practical problem of predicting the motion of storms. Lorenz spent the entirety of his scientific career at the Massachusetts Institute of Technology . In 1948, he joined the MIT Department of Meteorology as a research scientist. In 1955, he became an assistant professor in the department and was promoted to professor in 1962. From 1977 to 1981, Lorenz served as head of the Department of Meteorology at MIT. In 1983,

8586-414: The predictability of large-scale phenomena. Had the butterfly not flapped its wings, the trajectory of the overall system could have been vastly different. As suggested in Lorenz's book entitled The Essence of Chaos , published in 1993, "sensitive dependence can serve as an acceptable definition of chaos". In the same book, Lorenz defined the butterfly effect as: "The phenomenon that a small alteration in

8692-439: The present state—and in any real system such errors seem inevitable—an acceptable prediction of an instantaneous state in the distant future may well be impossible....In view of the inevitable inaccuracy and incompleteness of weather observations, precise very-long-range forecasting would seem to be nonexistent." His description of the butterfly effect , the idea that small changes can have large consequences, followed in 1969. In

8798-777: The previous calculation. They tracked this down to the computer printout. The computer worked with 6-digit precision, but the printout rounded variables off to a 3-digit number, so a value like 0.506127 printed as 0.506. This difference is tiny, and the consensus at the time would have been that it should have no practical effect. However, Lorenz discovered that small changes in initial conditions produced large changes in long-term outcome. Lorenz's discovery, which gave its name to Lorenz attractors , showed that even detailed atmospheric modeling cannot, in general, make precise long-term weather predictions. In 1963, Benoit Mandelbrot , studying information theory , discovered that noise in many phenomena (including stock prices and telephone circuits)

8904-513: The printout rounded variables off to a 3-digit number, so a value like 0.506127 printed as 0.506. This difference is tiny, and the consensus at the time would have been that it should have no practical effect. However, Lorenz discovered that small changes in initial conditions produced large changes in long-term results. Lorenz's discovery, which gave its name to Lorenz attractors , showed that even detailed atmospheric modelling cannot, in general, make precise long-term weather predictions. His work on

9010-535: The problem is to linearize any nonlinearity (the sine function term in this case) at the various points of interest through Taylor expansions . For example, the linearization at θ = 0 {\displaystyle \theta =0} , called the small angle approximation, is since sin ⁡ ( θ ) ≈ θ {\displaystyle \sin(\theta )\approx \theta } for θ ≈ 0 {\displaystyle \theta \approx 0} . This

9116-429: The qualitative analysis of nonlinear ordinary differential equations include: The most common basic approach to studying nonlinear partial differential equations is to change the variables (or otherwise transform the problem) so that the resulting problem is simpler (possibly linear). Sometimes, the equation may be transformed into one or more ordinary differential equations , as seen in separation of variables , which

9222-499: The related nonlinear system identification and analysis procedures. These approaches can be used to study a wide class of complex nonlinear behaviors in the time, frequency, and spatio-temporal domains. A system of differential equations is said to be nonlinear if it is not a system of linear equations . Problems involving nonlinear differential equations are extremely diverse, and methods of solution or analysis are problem dependent. Examples of nonlinear differential equations are

9328-420: The result will be a differential equation . A nonlinear system of equations consists of a set of equations in several variables such that at least one of them is not a linear equation . For a single equation of the form f ( x ) = 0 , {\displaystyle f(x)=0,} many methods have been designed; see Root-finding algorithm . In the case where f is a polynomial , one has

9434-586: The right conditions, chaos spontaneously evolves into a lockstep pattern. In the Kuramoto model , four conditions suffice to produce synchronization in a chaotic system. Examples include the coupled oscillation of Christiaan Huygens ' pendulums, fireflies, neurons , the London Millennium Bridge resonance, and large arrays of Josephson junctions . Moreover, from the theoretical physics standpoint, dynamical chaos itself, in its most general manifestation,

9540-672: The right-hand side cannot exhibit chaotic behavior. The reason is, simply put, that solutions to such systems are asymptotic to a two-dimensional surface and therefore solutions are well behaved. While the Poincaré–Bendixson theorem shows that a continuous dynamical system on the Euclidean plane cannot be chaotic, two-dimensional continuous systems with non-Euclidean geometry can still exhibit some chaotic properties. Perhaps surprisingly, chaos may occur also in linear systems, provided they are infinite dimensional. A theory of linear chaos

9646-645: The small angle approximation, this approximation is unstable, meaning that | θ | {\displaystyle |\theta |} will usually grow without limit, though bounded solutions are possible. This corresponds to the difficulty of balancing a pendulum upright, it is literally an unstable state. One more interesting linearization is possible around θ = π / 2 {\displaystyle \theta =\pi /2} , around which sin ⁡ ( θ ) ≈ 1 {\displaystyle \sin(\theta )\approx 1} : This corresponds to

9752-420: The state of a dynamical system will cause subsequent states to differ greatly from the states that would have followed without the alteration." The above definition is consistent with the sensitive dependence of solutions on initial conditions (SDIC). An idealized skiing model was developed to illustrate the sensitivity of time-varying paths to initial positions. A predictability horizon can be determined before

9858-482: The superposition principle An equation written as is called linear if f ( x ) {\displaystyle f(x)} is a linear map (as defined above) and nonlinear otherwise. The equation is called homogeneous if C = 0 {\displaystyle C=0} and f ( x ) {\displaystyle f(x)} is a homogeneous function . The definition f ( x ) = C {\displaystyle f(x)=C}

9964-501: The system appears random. In common usage, "chaos" means "a state of disorder". However, in chaos theory, the term is defined more precisely. Although no universally accepted mathematical definition of chaos exists, a commonly used definition, originally formulated by Robert L. Devaney , says that to classify a dynamical system as chaotic, it must have these properties: In some cases, the last two properties above have been shown to actually imply sensitivity to initial conditions. In

10070-412: The system produce complex effects throughout. This nonlinearity is one of the reasons why accurate long-term forecasts are impossible with current technology. Some authors use the term nonlinear science for the study of nonlinear systems. This term is disputed by others: Using a term like nonlinear science is like referring to the bulk of zoology as the study of non-elephant animals. In mathematics ,

10176-511: The topic, assisted by Ellen Fetter , culminated in the publication of his 1963 paper "Deterministic Nonperiodic Flow" in Journal of the Atmospheric Sciences , and with it, the foundation of chaos theory . He states in that paper: "Two states differing by imperceptible amounts may eventually evolve into two considerably different states ... If, then, there is any error whatever in observing

10282-423: The two trajectories end up diverging at a rate given by where t {\displaystyle t} is the time and λ {\displaystyle \lambda } is the Lyapunov exponent. The rate of separation depends on the orientation of the initial separation vector, so a whole spectrum of Lyapunov exponents can exist. The number of Lyapunov exponents is equal to the number of dimensions of

10388-507: The universe. Lorenz is remembered by colleagues and friends for his quiet demeanor, gentle humility, and love of nature. He was described as "a genius with a soul of an artist" by his close friend and collaborator Jule Charney . In 2011, The Lorenz Center, a climate think tank devoted to fundamental scientific inquiry, was founded at MIT in honor of Lorenz and his pioneering work on chaos theory and climate science . In February 2018, The Edward Lorenz Center and Henry Houghton Fund hosted

10494-406: The variable evolves chaotically with non-periodic behavior. Topological mixing (or the weaker condition of topological transitivity) means that the system evolves over time so that any given region or open set of its phase space eventually overlaps with any other given region. This mathematical concept of "mixing" corresponds to the standard intuition, and the mixing of colored dyes or fluids

10600-406: The x variable, the output of 1 corresponds to the first derivative of x and the output of 2 corresponds to the second derivative. Similar circuits only require one diode or no diodes at all. See also the well-known Chua's circuit , one basis for chaotic true random number generators. The ease of construction of the circuit has made it a ubiquitous real-world example of a chaotic system. Under

10706-408: Was Henri Poincaré . In the 1880s, while studying the three-body problem , he found that there can be orbits that are nonperiodic, and yet not forever increasing nor approaching a fixed point. In 1898, Jacques Hadamard published an influential study of the chaotic motion of a free particle gliding frictionlessly on a surface of constant negative curvature, called " Hadamard's billiards ". Hadamard

10812-620: Was able to show that all trajectories are unstable, in that all particle trajectories diverge exponentially from one another, with a positive Lyapunov exponent . Chaos theory began in the field of ergodic theory . Later studies, also on the topic of nonlinear differential equations , were carried out by George David Birkhoff , Andrey Nikolaevich Kolmogorov , Mary Lucy Cartwright and John Edensor Littlewood , and Stephen Smale . Although chaotic planetary motion had not been observed, experimentalists had encountered turbulence in fluid motion and nonperiodic oscillation in radio circuits without

10918-465: Was an avid outdoorsman, who enjoyed hiking, climbing, and cross-country skiing. He kept up with these pursuits until very late in his life. On April 16, 2008, Lorenz died at his home in Cambridge from cancer at the age of 90. Lorenz received a bachelor's degree in mathematics from Dartmouth College in 1938 and a master's degree in mathematics from Harvard in 1940. He worked as a weather forecaster for

11024-477: Was considered by chaos theorists as a full component of the studied systems. In 1959 Boris Valerianovich Chirikov proposed a criterion for the emergence of classical chaos in Hamiltonian systems ( Chirikov criterion ). He applied this criterion to explain some experimental results on plasma confinement in open mirror traps. This is regarded as the very first physical theory of chaos, which succeeded in explaining

11130-423: Was patterned like a Cantor set , a set of points with infinite roughness and detail Mandelbrot described both the "Noah effect" (in which sudden discontinuous changes can occur) and the "Joseph effect" (in which persistence of a value can occur for a while, yet suddenly change afterwards). In 1967, he published " How long is the coast of Britain? Statistical self-similarity and fractional dimension ", showing that

11236-631: Was sparked, in part, after a visit to the Institute for Advanced Study in Princeton, New Jersey, where he met Jule Charney , then head of the IAS's Meteorological Research Group and a leading dynamical meteorologist at the time. (Charney would later join Lorenz at MIT in 1957 as a professor of meteorology.) In 1953, Lorenz took over leadership of a project at MIT that ran complex simulations of weather models that he used to evaluate statistical forecasting techniques. By

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