details for today: date:9 th december 2004 by:mark cresswell followed by:nothing chaos 69eg3137 –...

22
Details for Today: DATE: 9 th December 2004 BY: Mark Cresswell FOLLOWED BY: Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Upload: lynne-warner

Post on 12-Jan-2016

217 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Details for Today:

DATE: 9th December 2004BY: Mark Cresswell

FOLLOWED BY: Nothing

Chaos

69EG3137 – Impacts & Models of Climate Change

Page 2: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lecture Topics• Introduction

• Lorenz and chaos

• The attractor

• Bifurcation

• Mandelbrot and Helge von Koch

• Summary

Page 3: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Introduction• If atmospheric processes were constant, or

strictly periodic, describing them mathematically would be easy…..weather forecasting would also be easy….and meteorology would be boring!

• Instead, the atmosphere exhibits variability and fluctuations that are irregular

• In order to deal quantitatively with uncertainty, it is necessary to use the tools of probability – the mathematical language of uncertainty

Page 4: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Introduction• Computer models generate deterministic

solutions of the future state of the atmosphere• Such model solutions do not provide an estimate

of uncertainty – if re-run with the same starting conditions, they generate the same solution

• These models could NEVER generate forecasts with NO uncertainty because of their limited model physics and the fact some processes operate at very small spatial scales – far smaller than the finest resolution of the model

Page 5: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lorenz and Chaos• Even if all relevant physics could be

included in atmospheric models we would still not escape uncertainty because of dynamical chaos

• This was a problem discovered by Ed Lorenz in 1963 - and effectively rules out any hope of an uncertainty-free forecast

• Lorenz began to formulate his ideas on weather predictability and chaos from an accidental discovery in his lab

Page 6: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

The effect of 0.506 instead of 0.506127 !!

Page 7: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lorenz and Chaos• What Lorenz observed was to become

known as the butterfly effect

The flapping of a single butterfly's wing today produces a tiny change in the state of the atmosphere. Over a period of time,

what the atmosphere actually does diverges from what it would have done. So, in a month's time, a tornado that would have

devastated the Indonesian coast doesn't happen. Or maybe one that wasn't going to happen, does.

(Ian Stewart, Does God Play Dice? The Mathematics of Chaos, pg. 141)

Page 8: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lorenz and Chaos• Lorenz found that the time evolution of a

non-linear dynamical system (like the atmosphere) is very sensitive to the initial conditions of that system

• If 2 realisations of the system are started from 2 very slightly different initial conditions, the two solutions will eventually diverge markedly

Page 9: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lorenz and Chaos• Since the atmosphere is always

incompletely observed, even a model with perfect physics will never start exactly like the real world – but will have gaps where initial conditions are unknown or slightly inaccurate

• These small errors and unknown values will accumulate and be magnified over time such that model and reality diverge over time

Page 10: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Lorenz and Chaos

Page 11: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

The Attractor• Lorenz decided to produce an experimental

set of equations to investigate chaos further

• He took the basic equations for convection – and stripped them down to an unrealistically small equation that retained a sensitive dependence on initial conditions

• Later, it was discovered that his equations exactly described the motion of a simple water wheel

Page 12: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

The Attractor• The simple equations gave rise to entirely

random behaviour – BUT when the results were graphed they showed something extraordinary

• The output always stayed on a curve – a double spiral. Previously, only a steady state or perfectly periodic state was known about

• Lorenz’s new state was ordered – but never repeated themselves nor followed a steady state

Page 13: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

The Attractor• When output from

Lorenz’s equations are visualised, we see a strange attractor….

• Now known as the Lorenz Attractor

Page 14: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Bifurcation• A similar problem occurs in ecology, and the

prediction of biological populations

• The equation would be simple if population just rises indefinitely, but the effect of predators and a limited food supply make this equation incorrect…so the simplest equation taking this into account is:

next year's population = r * this year's population * (1 - this year's population)

r = growth rate

Page 15: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Bifurcation• A biologist, Brian May decided to change the

growth rate and plot the results graphically

• As the growth rate increased, the final population would increase as well

• But…strangely.. As the rate passed a threshold the line broke into 2 and became 2 different populations

• As the rate increased, the populations would break again – but unpredictably – chaotically!

Page 16: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Bifurcation

Bifurcation

Upon closer inspection, it is possible to see white strips. Looking closer at these strips reveals little windows of order, where the equation goes through the bifurcations again before returning to chaos

Page 17: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Mandelbrot• An employee of IBM, Benoit Mandelbrot was a

mathematician studying the self-similarity of May and Lorenz’s work

• One of the areas he was studying was cotton price fluctuations

• No matter how the data on cotton prices was analysed, the results did not fit the normal distribution. Mandelbrot eventually obtained all of the available data on cotton prices, dating back to 1900

Page 18: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Mandelbrot• The numbers that produced aberrations from

the point of view of normal distribution produced symmetry from the point of view of scaling

• Each particular price change was random and unpredictable. But the sequence of changes was independent on scale: curves for daily price changes and monthly price changes matched perfectly

Page 19: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Mandelbrot• At one point, he was wondering about the

length of a coastline. A map of a coastline will show many bays. However, measuring the length of a coastline off a map will miss minor bays that were too small to show on the map

• walking along the coastline misses microscopic bays in between grains of sand. No matter how much a coastline is magnified, there will be more bays visible if it is magnified more

Page 20: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

MandelbrotOne mathematician, Helge von Koch, captured the ideas of Mandelbrot in a mathematical construction called the Koch curve. The Koch curve brings up an interesting paradox. Each time new triangles are added to the figure, the length of the line gets longer. However, the inner area of the Koch curve remains less than the area of a circle drawn around the original triangle. Essentially, it is a line of infinite length surrounding a finite area

Page 21: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Summary• Climate does repeat itself (consider the 4

seasons of Spring, Summer, Autumn and Winter) – but NEVER EXACTLY

• Models cannot replicate a system if it is missing information about initial conditions

• Uncertainty degrades predictability

• Randomness and unknown forcings generate seemingly chaotic turbulence – but such randomness actually has order

Page 22: Details for Today: DATE:9 th December 2004 BY:Mark Cresswell FOLLOWED BY:Nothing Chaos 69EG3137 – Impacts & Models of Climate Change

Summary• We will NEVER be able to generate accurate

weather forecasts or climate predictions because chaos arises from uncertainty

• Improvements in model physics will have a limited effect (garbage in = garbage out)

• Parallel improvements in observing systems will help to produce model simulations that see the influence of chaos occurring later in the integration – and hence providing longer lead-time forecasts