daisyworld
Download
Skip this Video
Download Presentation
Daisyworld

Loading in 2 Seconds...

play fullscreen
1 / 53

Daisyworld - PowerPoint PPT Presentation


  • 96 Views
  • Uploaded on

Daisyworld. What is a System?. Definition : A system is a group of different components that interact with each other Example : The climate system includes the atmosphere, oceans, polar caps, clouds, vegetation…and lots of other things. How do we study systems? Identify the components

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about ' Daisyworld' - mary


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
what is a system
What is a System?
  • Definition: A system is a group of different components that interact with each other
  • Example: The climate system includes the atmosphere, oceans, polar caps, clouds, vegetation…and lots of other things
slide3

How do we study systems?

  • Identify the components
  • Determine the nature of the
  • interactions between components
systems notation
Systems Notation

= system component

= positive coupling

= negative coupling

positive coupling
Positive Coupling

Atmospheric

CO2

Greenhouse

effect

  • An increase in atmospheric CO2 causes
  • a corresponding increase in the greenhouse
  • effect, and thus in Earth’s surface temperature
  • Conversely, a decrease in atmospheric CO2
  • causes a decrease in the greenhouse effect
negative coupling
Negative Coupling

Earth’s albedo

(reflectivity)

Earth’s

surface

temperature

  • An increase in Earth’s albedo causes a
  • corresponding decrease in the Earth’s surface
  • temperature by reflecting more sunlight back to
  • space
  • Or, a decrease in albedo causes an increase in
  • surface temperature
slide7

Equilibrium State:

Conditions under which the system will remain indefinitely

--If left unperturbed

slide13

When pushed by a perturbation, a stable equilibrium state, returns to (or near) the original state.

gaia hypothesis
Earth as a single living superorganism (James Lovelock)

Gaia - a new look at life on Earth, Oxford University Press, 1979.

Gaia hypothesis
lovelock s questions
Lovelock’s Questions

James Lovelock: NASA atmospheric chemist analyzing distant Martian atmosphere.

Why has temp of earth’s surface remained in narrow range for last 3.6 billion years when heat of sun has increased by 25%?

lovelock s questions1
Lovelock’s Questions

Why has oxygen remained near 21%?

Martian atmosphere in chemical equilibrium, whereas Earth’s atmosphere in unnatural low-entropy state.

our earth is a u nique planet in the solar system
Our Earth is a Unique Planet in the Solar System

Loss of carbon ::

No lithosphere motion on Mars to release carbon

Runaway greenhouse ::

No water cycle to remove carbon from atmosphere

Earth

Harbor of Life

Earth is unique in our solar system in its capacity to sustain highly diversified life

from Guy Brasseur (NCAR)

lovelock s answers
Lovelock´s answers

Earth can’t be understood without considering role of life

Abiotic factors

(physical, geological and chemical)

determine biological possibilities

Biotic factors feed back to control abiotic factors

Increased Planetary

Temperature

Increased Planetary Albedo

Sparser Vegetation, More Desertification

Reduced Temperature

gaia hypothesis1
Gaia Hypothesis

Organisms have a significant influence on their environment

Species of organisms that affect environment in a way to optimize their fitness leave more of the same – compare with natural selection.

Life and environment evolve as a single system – not only the species evolve, but the environment that favors the dominant species is sustained

daisy world
Daisy world

White daisies

Black daisies

Available fertile land

about daisyworld
About Daisyworld…
  • Daisyworld: a mythical planet with dark soil, white daisies, and a sun shining on it.
    • The dark soil have low albedo – they absorb solar energy, warming the planet.
    • The white daisies have high albedo – they reflect solar energy, cooling the planet.
temperature affects the number of daisies
Temperature affects the number of daisies
  • At 25° C many daisies cover the planet.
  • Daisies can’t survive below 5° C or above 40° C.
daisies can live between a min t a max t

daisy

coverage

daisy

coverage

T

T

optimum

Daisy coverage

T

min.

max.

Daisies can live between a min.T & a max. T
slide27
ENSC 425/625 Chapter 3UNBC

Effects of daisy coverage on T

daisy

coverage

daisy

coverage

T

T

P1

Effects of T on

daisy coverage

Daisy coverage

P2

T

  • Intersection of 2 curves means the 2 effects are balanced => equilibrium points P1 & P2.
feedback loops
ENSC 425/625 Chapter 3UNBC

Effects of daisy coverage on T

P1

Effects of T on

daisy coverage

Daisy coverage

P2

T

Feedback loops
perturb daisy coverage at p 1 sys returns to p 1 stable equil pt

P1

Daisy coverage

P2

T

Perturb daisy coverage at P1 => sys. returns to P1 (stable equil. pt.)

A large perturb.

=> daisies all die

from extreme T

slide30

Daisy coverage

P1

P2

T

Large incr. in daisy cover => very low T =>

decr. in daisy cov. => very high T => lifeless.

slide31
ENSC 425/625 Chapter 3UNBC

daisy

coverage

T

Daisy coverage

P1

P2

T

  • From P2, incr. daisy cov. => decr. T =>

further incr. in daisy cov. => converge to P1

unstable

equilib. pt.

gradual incr in solar luminosity
ENSC 425/625 Chapter 3UNBC

P1

P1

P2

Daisy coverage

To

Tf

Teq

P2

T

Gradual incr. in solar luminosity

For any particular value

of daisy cov., T incr.

The effect of T on

Daisy unchanged

an equation for the black daisies
An equation for the black daisies

αb

( 1 – αb – αw)

β(Tb)

- γαb

dαb/dt =

= αb (αg β(Tb) – γ)

b(T) is a function that is zero at 5C, rises to a maximum of

one at 22.5C and then falls to zero again at 40C

A simple and convenient choice is

an equation for the white daisies
An equation for the white daisies

We use a similar equation for the white daisies:

dαw/dt = αw (αg β(Tw) – γ)

We don’t have to use the same b(T) and g but it

keeps things simple. We can use different ones

later if we want to.

heat flow
Heat Flow

Because different regions of Daisyworld are at different

temperatures, there will be heat flow. We include this in

the model using the equations

Note that if q=0 the whole planet is at the same temperature,

i.e., the heat flow is very rapid indeed. As q increases, so do

the temperature differences.

Don’t worry about the 4th powers; they’re only there to make

the calculations easier and don’t make any real difference.

gaia hypothesis2
Gaia Hypothesis
  • Proposed by James Lovelock
      • Developed in 1960s
      • First published in 1975
  • Definition of Gaia:
      • a complex entity involving the Earth\'s biosphere, atmosphere, oceans, and soil; the totality constituting a feedback or cybernetic system which seeks an optimal physical and chemical environment for life on this planet. (Lovelock)
daisyworld model
Daisyworld Model
  • Daisyworld is a hypothetical planet orbiting a sun that increases in intensity
  • The planet is inhabited by 2 species
      • Black daisies
      • White daisies
  • Original Daisyworld model consisted of a system of differential equations
      • This project uses these equations to build a 2D cellular automata representation of Daisyworld
daisyworld model 2
Daisyworld Model (2)
  • Temperature of Daisyworld is based on the assumption that the planet is in radiative equilibrium (i.e. energy emitted = energy absorbed)
  • Albedo of the planet is computed based on the albedos of each type of daisy and the area covered by them
daisyworld model 3
Daisyworld Model (3)
  • Area of daisies is modified according to the following equations
daisyworld model 4
Daisyworld Model (4)
  • 2D CA rules:
      • If da/dt > 0
        • If neighbors with no daisies < spreading threshold
          • Bare neighbors grow daisy with probability: p = c*da/dt
        • Else if neighbors with no daisies >= spreading threshold
          • Start new patch of daisies
      • If da/dt <= 0
        • Daisies die with probability p = -da/dt
example of daisy crowding
Example of Daisy Crowding
  • Spreading-threshold = 6

=> Start new patch of daisies

=> Don’t start new patch

parameter settings
Parameter Settings
  • Two different temperature models
      • Automatic linear increase of solar luminosity
      • Manual adjustment of solar luminosity
  • Death-rate: 0.3
  • Albedo of white daisies: 0.75
  • Albedo of black daisies: 0.25
  • Albedo of bare land: 0.50
  • Spreading threshold: 8
  • Optimal daisy growth temperature: 22.5 C
spatial daisyworld vs mathematical daisyworld
Spatial Daisyworld vs. Mathematical Daisyworld

Area Occupied by Daisies

(Mathematical Model)

(Spatial Model)

spatial daisyworld vs mathematical daisyworld 2
Spatial Daisyworld vs. Mathematical Daisyworld (2)

Temperature of Daisyworld

(Mathematical Model)

(Spatial Model)

the effects of death rate on daisyworld
The Effects of Death Rate on Daisyworld

death-rate = 0.3

death-rate = 0.1

death-rate = 0.5

daisyworld with four species of daisies
Daisyworld with Four Species of Daisies

Area covered by daisies

Temperature of Daisyworld