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Introduction

"Daisyworld, a computer simulation, is a hypothetical world orbiting a star whose radiant energy is slowly increasing or decreasing. It is meant to mimic important elements of the Earth-Sun system, and was introduced by James Lovelock and Andrew Watson in a paper published in 1983 to illustrate the plausibility of the Gaia hypothesis. In the original 1983 version, Daisyworld is seeded with two varieties of daisy as its only life forms: black daisies and white daisies. White petaled daisies reflect light, while black petaled daisies absorb light. The simulation tracks the two daisy populations and the surface temperature of Daisyworld as the sun's rays grow more powerful."

Daisy World Wikipedia page

Gaia Hypothesis Wikipedia page

A Simple Model

First let's consider a simple model. In this model, we will consider one type of daisy that initially covers 1% of the Earth (at \(t = 0\)). The rate of change of the amount of daisies will depend several factors:

We can combine these things in a differential equation. The rate of change in area covered by the daisy species is given by: \[ \frac{dF}{dt}= F(1-F)(G - D) \] We can roughly calculate the amount of covered area at time \(n + 1\) like so: \[F_{n+1} = F_n + \left.\frac{dF}{dt}\right|_{t=n}\]

05101520253035404550 Time (one million years) 0.00.10.20.30.40.50.60.70.80.91.0 Fraction of Earth

Legend
Blue: Bare Earth
Pink: Daisies

Growth Rate is 0.40

Death Rate is 0.20

A More Complicated Model...

Here are some parameters we will be using

Let's get started!

The Sun is an important factor in this model. The Sun has a solar flux of 917 \(W m^{-2}\). This is a baseline amount of power that the Sun emits to Daisy World.

Like any star, the Sun gets hotter and hotter as it ages. The solar luminosity of the sun starts at 0.6 at time \(t=0\), and increases linearly to 1.8 at time \(t=200\). This represents the proportion of the solar flux that the Sun actually emits

Daisy World would be in big trouble if it absorbed all of the energy received by the Sun. Albedo is a measure of how much energy is reflected back into space. We will use \(A_P\) to denote the albedo of Daisy World. For example, if \(A_P = 0.5\), this means that 50% of the incoming solar power is reflected.

Because our time scale is on the scale of millions of years, we will assume that the planet is in radiative equilibrium. This means that the amount of energy that Daisy World absorbs is equal to the amount it emits. The amount of energy absorbed by Daisy World (per unit area) is given by \[X\times L\times(1-A_{P})\] This also represents the amount of energy emitted. We can now use the Stefan-Boltzmann Law to estimate average global temperature, \(T_P\). We will assume Daisy World is an ideal blackbody with emissivity = 1. \[\frac{P}{S}=\sigma T^4\] Plugging in known values gives us \[X\times L\times(1-A_P)=\sigma T_P^4\] We can use this equation to solve for \(T_P\)

Now we can introduce the daisies! Daisies have the special ability to affect temperature because of their albedo. Uncovered Daisy World area has an albedo of \(A_U=0.5\). We will start by assuming that black daisies have an albedo of \(A_B=0.25\) and white daisies have an albedo of \(A_W=0.75\). The albedo of the planet can be calculated as follows: \[A_{P} = F_UA_{U} + F_BA_{B} + F_WA_{W} \] Daisy World starts off empty because daisies can only survive in temperatures between 5 and 40 degrees Celsius. This means that \(F_B=F_W=0\) and \(F_U=1\), so \(A_P = A_U\).

Here we make an important distinction. There is a difference between the average global temperature \(T_P\) and the local temperature \(T_{B}\) or \(T_W\) for a given color of daisies. Daisies can only survive when their local temperature is between 5 and 40 Celsius. At the start of the simulation, \(T_P=T_B=T_W\) because there are no daisies. Once daisies begin to grow however, these temperatures will differ. The local temperature for a species is given by the following equation: \[T_{B/W} = H \times (A_P-A_{B/W}) + T_P\] Here, \(H\) is a constant that simply controls how much the local temperature differs from the average global temperature.

The growth factor helps determine the growth rate of daisies. It is 0 when outside this temperature range. When inside the range, it follows the given quadratic function: \[G_{B/W} = 1-0.003265\times(22.5-T_{B/W})^2\] The overall rate of change of a given amount of daisy is given by the following equation: \[\frac{dF_{B/W}}{dt} = F_{B/W}\times(F_U\times G_{B/W} - D)+0.001\] The "+ 0.001" causes daisies to spontaneously sprout once the local temperature is within the acceptable range.

We've also added an interesting [PLAGUE] option...

During a plague, the death rate is bumped to 0.9. After the plague ends, it returns to normal

And that's about it! Explore how this system works using the graphs below

Legend
Black: Black Daisies
White: White Daisies
Brown: Uncovered Area
Orange: Empty Planet Temperature
Purple: Daisy World Temperature

020406080100120140160180200 Time (one million years) 0.00.10.20.30.40.50.60.70.80.91.0 Fraction of Earth

Uncovered land albedo is 0.50

Black daisy albedo is 0.25

White daisy albedo is 0.75

Death rate is 0.30

Optimal temperature is 22.5 C

Temperature range is 35 C

Heat Absorb Factor is 20

Plagues last for 10 years

020406080100120140160180200 Time (one million years) 0 10 20 30 40 50 60 70 80 Temperature (C)

Current Time: 0


The maximum amount of black daisies is ?

The maximum amount of white daisies is ?