Is our climate headed for a mathematical tipping point Victor J. Donnay

For most of us, two degrees Celsius
is a tiny difference in temperature,

not even enough to make
you crack a window.

But scientists have warned that as
CO2 levels in the atmosphere rise,

an increase in the Earth’s temperature
by even this amount

can lead to catastrophic effects
all over the world.

How can such a small measurable
change in one factor

lead to massive and unpredictable
changes in other factors?

The answer lies in the concept of a
mathematical tipping point,

which we can understand through the
familiar game of billiards.

The basic rule of billiard motion is

that a ball will go straight
until it hits a wall,

then bounce off at an angle equal
to its incoming angle.

For simplicity’s sake, we’ll assume that
there is no friction,

so balls can keep moving indefinitely.

And to simplify the situation further,

let’s look at what happens with only
one ball on a perfectly circular table.

As the ball is struck and begins to move
according to the rules,

it follows a neat star-shaped pattern.

If we start the ball at
different locations,

or strike it at different angles,
some details of the pattern change,

but its overall form remains the same.

With a few test runs, and some basic
mathematical modeling,

we can even predict a ball’s path
before it starts moving,

simply based on its starting conditions.

But what would happen
if we made a minor change

in the table’s shape
by pulling it apart a bit,

and inserting two small straight edges
along the top and bottom?

We can see that as the ball bounces
off the flat sides,

it begins to move all over the table.

The ball is still obeying the same rules
of billiard motion,

but the resulting movement no longer
follows any recognizable pattern.

With only a small change
to the constraints

under which the system operates,

we have shifted the billiard motion

from behaving in a stable
and predictable fashion,

to fluctuating wildly,

thus creating what mathematicians
call chaotic motion.

Inserting the straight edges into
the table acts as a tipping point,

switching the systems behavior
from one type of behavior (regular),

to another type of behavior (chaotic).

So what implications does this simple
example have for the much more complicated

reality of the Earth’s climate?

We can think of the shape of the table as
being analogous to the CO2 level

and Earth’s average temperature:

Constraints that impact the
system’s performance

in the form of the ball’s motion
or the climate’s behavior.

During the past 10,000 years,

the fairly constant CO2 atmospheric
concentration of

270 parts per million kept the climate
within a self-stabilizing pattern,

fairly regular and hospitable
to human life.

But with CO2 levels now at 400
parts per million,

and predicted to rise to between
500 and 800 parts per million

over the coming century,
we may reach a tipping point where

even a small additional change
in the global average temperature

would have the same effect as
changing the shape of the table,

leading to a dangerous shift in the
climate’s behavior,

with more extreme and intense
weather events,

less predictability, and most importantly,
less hospitably to human life.

The hypothetical models that
mathematicians study in detail

may not always look like
actual situations,

but they can provide a framework
and a way of thinking

that can be applied to help understand the
more complex problems of the real world.

In this case, understanding
how slight changes

in the constraints impacting a system
can have massive impacts

gives us a greater appreciation for
predicting the dangers

that we cannot immediately percieve
with our own senses.

Because once the results do become visible,
it may already be too late.