by Ben Brown-Steiner
Imagine the earth’s climate system as a foreign sports car owned by a playful friend. Your friend is happy to let you look and listen to the car and will on occasion give you a ride in it. But he’s unwilling to let you look under the hood or study the user’s manual. If you want to try and understand how the car works, and maybe even build your own, you are going to need to be clever and use all the tools at your disposal to figure out how this car works.
Imagine the earth’s climate system as a foreign sports car owned by a playful friend. Your friend is happy to let you look and listen to the car and will on occasion give you a ride in it. But he’s unwilling to let you look under the hood or study the user’s manual. If you want to try and understand how the car works, and maybe even build your own, you are going to need to be clever and use all the tools at your disposal to figure out how this car works.
This is
very much like how earth scientists try to understand the real world. The real
world, even more so than the foreign sports car, is very complex and intricate.
We are unable to look under reality’s hood or read reality’s users manual. What
we are able to do is to make careful observations, come up with theories as to
how the real world works, test our theories with experiments and create models
to test and explore our understanding.
When you
start to build your own car, the first thing you are going to gather are the
major parts: a frame, an engine, wheels, rods, doors, spark plugs, fuel and so
on. For the Earth’s climate, instead of parts we have variables: ocean
temperature, relative humidity, solar radiation, CO2 concentrations, and many
others.
However,
you need a plan to put your parts together.
You need an understanding of some of the interactions between the parts
you have and the function of your car. You know that fuel needs to be injected
into the engine in a particular way. You know that the wheels need to be
connected both to the engine and to the brakes if you ever want to actually
drive your car. Earth scientists know that sunlight heats the surface of the
earth, which in turn heats the atmosphere. They know that warm air holds more water
than cold air. Any successful climate model needs to have these elementary
parts.
To put
these parts together you need a design framework. For our car, this is a
engineering schematic of the parts and their functionality. We know when brakes
are applied, the velocity of the car decreases. For earth scientists, this is
typically in the form of code and equations. We know that precipitation falls
as rain if the temperature is above freezing and falls as snow if the
temperature is below freezing.
During our
first attempt, there are many things we don’t know. We know that there is an
interaction between the stick shift and the engine. We know that there is some
interaction between the oceans and the atmosphere. But we don’t know the exact
details. To begin to understand these unknowns we must make careful
observations of the thing we’re trying to model and come up with tentative
hypothesis and theories. We can listen to the revving of the engine or make
observations of ocean and atmospheric temperatures.
You then
put together a scheme that you think might work like the real thing. You design
some system (or write some code) that combines what you know with the things
you have hypothesized. Because you know that you are uncertain about particular
interactions, you make those parts easy to observe and easy to modify or swap
out with another part. This is what often is described as a parameterization or
a scheme in a climate model. It’s a variable or equation that you know you’ll
have to tweak or change out later on.
For instance, after
you run the car you notice that your car moves backwards when you think it
should be moving forwards or your climate snows when it should be raining. You
look carefully at your variables and design and equations and parameters and
try to find the error. You may have had your wires mismatched our you may have
had inaccurately represented the relationship between moisture and temperature.
The next
step takes this newfound understanding and incorporates it into your next
model. You fix your mistakes and you tune your parameterizations. Then you test
it again and repeat the whole process over and over until your understanding
grows. Fundamentally, this is is the way that science functions. It is an
interactive process. It’s never ending. You test and tune and observe and
reformulate and repeat. Eventually, if you are clever and lucky, your model
gets better and you gain a deeper understanding.
Unfortunately,
since we are not able to look at the actual foreign sports car (because our friend
is too secretive) and since we will never see the inner workings of the real
world, we are never going to have a perfect model. Models by definition are
simplifications of the real thing. You strive to have a really good
simplification that provides insight and understanding. And you keep trying.
This is science.
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