11 Type 3: Causal Arguments

Causal Arguments

Causal arguments attempt to make a case that one thing led to another. They answer the question “What caused it?” Causes are often complex and multiple. Before we choose a strategy for a causal argument it can help to identify our purpose. Why do we need to know the cause? How will it help us?

 

Purposes of causal arguments

 

To get a complete picture of how and why something happened

In this case, we will want to look for multiple causes, each of which may play a different role. Some might be background conditions, others might spark the event, and others may be influences that sped up the event once it got started. In this case, we often speak of near causes that are close in time or space to the event itself, and remote causes, that are further away or further in the past. We can also describe a chain of causes, with one thing leading to the next, which leads to the next. It may even be the case that we have a feedback loop where a first event causes a second event and the second event triggers more of the first, creating an endless circle of causation. For example, as sea ice melts in the arctic, the dark water absorbs more heat, which warms it further, which melts more ice, which makes the water absorb more heat, etc. If the results are bad, this is called a vicious circle.

 

To decide who is responsible

Sometimes if an event has multiple causes, we may be most concerned with deciding who bears responsibility and how much. In a car accident, the driver might bear responsibility and the car manufacturer might bear some as well. We will have to argue that the responsible party caused the event but we will also have to show that there was a moral obligation not to do what the party did. That implies some degree of choice and knowledge of possible consequences. If the driver was following all good driving regulations and triggered an explosion by activating the turn signal, clearly the driver cannot be held responsible.

In order to determine that someone is responsible, there must be a clearly defined domain of responsibility for that person or entity. To convince readers that a certain party is responsible, readers have to agree on what the expectations for that party in their particular role are. For example, if a patient misreads the directions for taking a drug and accidentally overdoses, does the drug manufacturer bear any responsibility? What about the pharmacist? To decide that, we need to agree on how much responsibility the manufacturer has for making the directions foolproof and how much the pharmacist has for making sure the patient understands them. Sometimes a person can be held responsible for something they didn’t do if the action omitted fell under their domain of responsibility.

 

To figure out how to make something happen

In this case we need to zero in on a factor or factors that will push the event forward. Such a factor is sometimes called a precipitating cause. The success of this push will depend on circumstances being right for it, so we will likely also need to describe the conditions that have to be in place for the precipitating cause to actually precipitate the event. If there are likely factors that could block the event, we need to show that those can be eliminated. For example, if we propose a particular surgery to fix a heart problem, we will also need to show that the patient can get to a hospital that performs the surgery and get an appointment. We will certainly need to show that the patient is likely to tolerate the surgery.

 

To stop something from happening

In this case, we do not need to describe all possible causes. We want to find a factor that is so necessary to the bad result that if we get rid of that factor, the result cannot occur. Then if we eliminate that factor, we can block the bad result. If we cannot find a single such factor, we may at least be able to find one that will make the bad result less likely. For example, to reduce wildfire risk in California, we cannot get rid of all fire whatsoever, but we can repair power lines and aging gas and electric infrastructure to reduce the risk that defects in this system will spark a fire. Or we could try to reduce the damage fires cause by focusing on clearing underbrush.

 

To predict what might happen in future

As Jeanne Fahnestock and Marie Secor put it in A Rhetoric of Argument, “When you argue for a prediction, you try to convince your reader that all the causes needed to bring about an event are in place or will fall into place.” You also may need to show that nothing will intervene to block the event from happening. One common way to support a prediction is by comparing it to a past event that has already played out. For example, we might argue that humans have survived natural disasters in the past, so we will survive the effects of climate change as well. As Fahnestock and Secor point out, however, “the argument is only as good as the analogy, which sometimes must itself be supported.” How comparable are the disasters of the past to the likely effects of climate change? The argument would need to describe both past and possible future events and convince us that they are similar in severity.

 

Techniques and cautions for causal argument

So how does a writer make a case that one thing causes another? The briefest answer is that the writer needs to convince us that the factor and the event are correlated and also that there is some way in which the factor could plausibly lead to the event. Then the writer will need to convince us that they have done due diligence in considering and eliminating alternate possibilities for the cause and alternate explanations for any correlation between the factor and the event.

 

Identify possible causes

If other writers have already identified possible causes, an argument simply needs to refer back to those and add in any that have been missed. If not, the writer can put themselves in the role of detective and imagine what might have caused the event.

 

Determine which factor is most correlated with the event

If we think that a factor may commonly cause an event, the first question to ask is whether they go together. If we are looking for a sole cause, we can ask if the factor is always there when the event happens and always absent when the event doesn’t happen. Do the factor and the event follow the same trends? The following methods of arguing for causality were developed by philosopher John Stuart Mill, and are often referred to as “Mill’s methods.”

  • If the event is repeated and every time it happens, a common factor is present, that common factor may be the cause.
  • If there is a single difference between cases where the event takes place and cases where it doesn’t.
  • If an event and a possible cause are repeated over and over and they happen to varying degrees, we can check whether they always increase and decrease together. This is often best done with a graph so we can visually check whether the lines follow the same pattern.
  • Finally, ruling out other possible causes can support a case that the one remaining possible cause did in fact operate.

 

Explain how that factor could have caused the event

In order to believe that one thing caused another, we usually need to have some idea of how the first thing could cause the second. If we cannot imagine how one would cause another, why should we find it plausible? Any argument about agency, or the way in which one thing caused another, depends on assumptions about what makes things happen. If we are talking about human behavior, then we are looking for motivation: love, hate, envy, greed, desire for power, etc. If we are talking about a physical event, then we need to look at physical forces. Scientists have dedicated much research to establishing how carbon dioxide in the atmosphere could effectively trap heat and warm the planet.

If there is enough other evidence to show that one thing caused another but the way it happened is still unknown, the argument can note that and perhaps point toward further studies that would establish the mechanism. The writer may want to qualify their argument with “may” or “might” or “seems to indicate,” if they cannot explain how the supposed cause led to the effect.

 

Eliminate alternate explanations

The catchphrase “correlation is not causation” can help us to remember the dangers of the methods above. It’s usually easy to show that two things happen at the same time or in the same pattern, but hard to show that one actually causes another. Correlation can be a good reason to investigate whether something is the cause, and it can provide some evidence of causality, but it is not proof. Sometimes two unrelated things may be correlated, like the number of women in Congress and the price of milk. We can imagine that both might follow an upward trend, one because of the increasing equality of women in society and the other because of inflation. Describing a plausible agency, or way in which one thing led to another, can help show that the correlation is not random. If we find a strong correlation, we can imagine various causal arguments that would explain it and argue that the one we support has the most plausible agency.

Sometimes things vary together because there is a common cause that affects both of them. An argument can explore possible third factors that may have led to both events. For example, students who go to elite colleges tend to make more money than students who go to less elite colleges. Did the elite colleges make the difference? Or are both the college choice and the later earnings due to a third cause, such as family connections? In his book Food Rules: An Eater’s Manual, journalist Michael Pollan assesses studies on the effects of supplements like multivitamins and concludes that people who take supplements are also those who have better diet and exercise habits, and that the supplements themselves have no effect on health. He advises, “Be the kind of person who takes supplements — then skip the supplements.”

If we have two phenomena that are correlated and happen at the same time, it’s worth considering whether the second phenomenon could actually have caused the first rather than the other way around. For example, if we find that gun violence and violence within video games are both on the rise, we shouldn’t leap to blame video games for the increase in shootings. It may be that people who play video games are being influenced by violence in the games and becoming more likely to go out and shoot people in real life. But could it also be that as gun violence increases in society for other reasons, such violence is a bigger part of people’s consciousness, leading video game makers and gamers to incorporate more violence in their games? It might be that causality operates in both directions, creating a feedback loop as we discussed above.

Proving causality is tricky, and often even rigorous academic studies can do little more than suggest that causality is probable or possible. There are a host of laboratory and statistical methods for testing causality. The gold standard for an experiment to determine a cause is a double-blind, randomized control trial in which there are two groups of people randomly assigned. One group gets the drug being studied and one group gets the placebo, but neither the participants nor the researchers know which is which. This kind of study eliminates the effect of unconscious suggestion, but it is often not possible for ethical and logistical reasons.

The ins and outs of causal arguments are worth studying in a statistics course or a philosophy course, but even without such a course we can do a better job of assessing causes if we develop the habit of looking for alternate explanations.

 

Sample annotated causal argument

The article “Climate Explained: Why Carbon Dioxide Has Such Outsized Influence on Earth’s Climate” by Jason West, published in The Conversation, can serve as an example. Annotations point out how the author uses several causal argument strategies. 

 

Exercises

Reflect on the following to construct a causal argument. What would be the best intervention to introduce in society to reduce the rate of violent crime? Below are some possible causes of violent crime.  Choose one and describe how it could lead to violent crime.  Then think of a way to intervene in that process to stop it.  What method from among those described in this section would you use to convince someone that your intervention would work to lower rates of violent crime?  Make up an argument using your chosen method and the kind of evidence, either anecdotal or statistical, you would find convincing.

Possible causes of violent crime:

  • Homophobia and transphobia
  • PTSD
  • Testosterone
  • Child abuse
  • Violence in the media
  • Role models who exhibit toxic masculinity
  • Depression
  • Violent video games
  • Systemic racism
  • Lack of education on expressing emotions
  • Unemployment
  • Not enough law enforcement
  • Economic inequality
  • The availability of guns

Screen-Reader Accessible Annotated Causal Argument

Format note: This version is accessible to screen reader users.  Refer to these tips for reading our annotated sample arguments with a screen reader. For a more traditional visual format, see the PDF version of “Climate Explained: Why Carbon Dioxide Has Such Outsized Influence on Earth’s Climate” above.

Jason West

From The Conversation

September 13, 2019

 

Climate Explained: Why Carbon Dioxide Has Such Outsized Influence on Earth’s Climate

(Note: The title frames the article as a causal argument, a demonstration of how carbon dioxide affects the climate.)

Climate Explained is a collaboration between The Conversation, Stuff and the New Zealand Science Media Centre to answer your questions about climate change.

 

Question

I heard that carbon dioxide makes up 0.04% of the world’s atmosphere. Not 0.4% or 4%, but 0.04%! How can it be so important in global warming if it’s such a small percentage?

I am often asked how carbon dioxide can have an important effect on global climate when its concentration is so small – just 0.041% of Earth’s atmosphere. And human activities are responsible for just 32% of that amount. (Note: Jason West presents his article as a rebuttal to a counterargument.)

I study the importance of atmospheric gases for air pollution and climate change. (Note: West establishes his credibility as a researcher on the subject.)The key to carbon dioxide’s strong influence on climate is its ability to absorb heat emitted from our planet’s surface, keeping it from escaping out to space. (Note: West summarizes his causal argument by explaining a mechanism that could account for CO2’s surprising effect on temperature.)

 

Early greenhouse science

The scientists who first identified carbon dioxide’s importance for climate in the 1850s were also surprised by its influence. (Note: This bit of history underlines West’s sympathy for the surprise expressed in the opening question.)Working separately, John Tyndall in England and Eunice Foote in the United States found that carbon dioxide, water vapor and methane all absorbed heat, while more abundant gases did not.

Scientists had already calculated that the Earth was about 59 degrees Fahrenheit (33 degrees Celsius) warmer than it should be, given the amount of sunlight reaching its surface. The best explanation for that discrepancy was that the atmosphere retained heat to warm the planet.

Tyndall and Foote showed that nitrogen and oxygen, which together account for 99% of the atmosphere, had essentially no influence on Earth’s temperature because they did not absorb heat. (Note: West shows how scientists eliminated what seemed like likely causes for the warming effect.) Rather, they found that gases present in much smaller concentrations were entirely responsible for maintaining temperatures that made the Earth habitable, by trapping heat to create a natural greenhouse effect.

 

A blanket in the atmosphere

(Note: Comparing heat-trapping gases to a blanket helps readers visualize the causal argument.)

Earth constantly receives energy from the sun and radiates it back into space. For the planet’s temperature to remain constant, the net heat it receives from the sun must be balanced by outgoing heat that it gives off. (Note: West gives background on what influences the earth’s temperature.)

Since the sun is hot, it gives off energy in the form of shortwave radiation at mainly ultraviolet and visible wavelengths. Earth is much cooler, so it emits heat as infrared radiation, which has longer wavelengths.

Figure 2: Shows the connection between the wavelength of light and the amount of energy

Figure 2: The electromagnetic spectrum is the range of all types of EM radiation – energy that travels and spreads out as it goes. The sun is much hotter than the Earth, so it emits radiation at a higher energy level, which has a shorter wavelength. NASA

Carbon dioxide and other heat-trapping gases have molecular structures that enable them to absorb infrared radiation. The bonds between atoms in a molecule can vibrate in particular ways, like the pitch of a piano string. When the energy of a photon corresponds to the frequency of the molecule, it is absorbed and its energy transfers to the molecule. (Note: This section establishes agency, an explanation for how CO2 could trap heat.)

Carbon dioxide and other heat-trapping gases have three or more atoms and frequencies that correspond to infrared radiation emitted by Earth. Oxygen and nitrogen, with just two atoms in their molecules, do not absorb infrared radiation.  (Note: West explains why two other possible causes of warming, oxygen and nitrogen, do not trap heat.)

Most incoming shortwave radiation from the sun passes through the atmosphere without being absorbed. But most outgoing infrared radiation is absorbed by heat-trapping gases in the atmosphere. Then they can release, or re-radiate, that heat. Some returns to Earth’s surface, keeping it warmer than it would be otherwise.

Figure 3: Earth receives solar energy from the sun (yellow), and returns energy back to space by reflecting some incoming light and radiating heat (red). Greenhouse gases trap some of that heat and return it to the planet’s surface. NASA via Wikimedia. (Note: Figure 3, with the rightmost red stripe pointing back to earth, makes a visual argument that greenhouse gases trap heat.)

Figure 3: Earth receives solar energy from the sun (yellow), and returns energy back to space by re-flecting some incoming light and radiating heat (red). Greenhouse gases trap some of that heat and return it to the planet’s surface. NASA via Wikimedia

 

Research on heat transmission

During the Cold War, the absorption of infrared radiation by many different gases was studied extensively. The work was led by the U.S. Air Force, which was developing heat-seeking missiles and needed to understand how to detect heat passing through air.

This research enabled scientists to understand the climate and atmospheric composition of all planets in the solar system by observing their infrared signatures. For example, Venus is about 870 F (470 C) because its thick atmosphere is 96.5% carbon dioxide. (Note: The comparison to Venus shows that a high concentration of carbon dioxide in the atmosphere correlates with high temperature on another planet.)

It also informed weather forecast and climate models, allowing them to quantify how much infrared radiation is retained in the atmosphere and returned to Earth’s surface.

People sometimes ask me why carbon dioxide is important for climate, given that water vapor absorbs more infrared radiation and the two gases absorb at several of the same wavelengths. The reason is that Earth’s upper atmosphere controls the radiation that escapes to space. The upper atmosphere is much less dense and contains much less water vapor than near the ground, which means that adding more carbon dioxide significantly influences how much infrared radiation escapes to space. (Note: In this paragraph, West eliminates another possible driver of climate change, heat-trapping water vapor.)

Carbon dioxide levels rise and fall around the world, changing seasonally with plant growth and decay.

 

Observing the greenhouse effect

Have you ever noticed that deserts are often colder at night than forests, even if their average temperatures are the same? Without much water vapor in the atmosphere over deserts, the radiation they give off escapes readily to space. In more humid regions radiation from the surface is trapped by water vapor in the air. Similarly, cloudy nights tend to be warmer than clear nights because more water vapor is present.

The influence of carbon dioxide can be seen in past changes in climate. Ice cores from over the past million years have shown that carbon dioxide concentrations were high during warm periods – about 0.028%. During ice ages, when the Earth was roughly 7 to 13 F (4-7 C) cooler than in the 20th century, carbon dioxide made up only about 0.018% of the atmosphere. (Note: West gives more evidence from Earth’s history to show a correlation between high carbon dioxide concentration and higher temperatures.)

Even though water vapor is more important for the natural greenhouse effect, changes in carbon dioxide have driven past temperature changes. In contrast, water vapor levels in the atmosphere respond to temperature. As Earth becomes warmer, its atmosphere can hold more water vapor, which amplifies the initial warming in a process called the “water vapor feedback.” (Note: West describes a feedback loop or vicious circle where warming leads to more warming.) Variations in carbon dioxide have therefore been the controlling influence on past climate changes.

Small change, big effects

It shouldn’t be surprising that a small amount of carbon dioxide in the atmosphere can have a big effect. We take pills that are a tiny fraction of our body mass and expect them to affect us. (Note: West supports his causal claim by making a comparison to something more familiar, pills.)

Today the level of carbon dioxide is higher than at any time in human history. Scientists widely agree that Earth’s average surface temperature has already increased by about 2 F (1 C) since the 1880s, and that human-caused increases in carbon dioxide and other heat-trapping gases are extremely likely to be responsible. (Note: West points to a correlation between CO2 and temperature. Here he relies on experts to support the idea of causation.)

Without action to control emissions, carbon dioxide might reach 0.1% of the atmosphere by 2100, more than triple the level before the Industrial Revolution. This would be a faster change than transitions in Earth’s past that had huge consequences. Without action, this little sliver of the atmosphere will cause big problems. (Note: West ends with a brief prediction. He compares the potential rise in carbon dioxide with past changes to imply that the consequences of human-induced climate change will be more dramatic than in the past.)

 

 

Attribution

This article is republished from The Conversation under a Creative Commons CC BY-ND 4.0 license. Annotations are by Anna Mills and licensed CC BY-NC 4.0.

 

Chapter Attribution

This chapter is from “Forming a Research-Based Argument” in in How Arguments Work: A Guide to Writing and Analyzing Texts in College by Anna Mills under a CC BY-NC 4.0 license.

 

 

License

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Upping Your Argument and Research Game Copyright © 2022 by Liona Burnham is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, except where otherwise noted.

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