A Crash Course on the Climate Change Debate

Are you a climate change believer or denier?

Trick question.

The climate change debate has become so politicized from both sides that most people have a very rudimentary understanding of it, regardless of which “side” they fall on. Such a lack of public knowledge about the actual scientific aspects involved isn't all that surprising, given how complex the subject appears on its face. But without an understanding of the details we become susceptible to accepting caricatured descriptions of the scientific debate as patent truth, and that prevents us from pursuing the course of action that's best for our society and our world. If we care about being engaged national and global citizens, we have a responsibility to understand what's involved here, because the repercussions of the decisions made either way will impact us all, for our whole lives and beyond.

To set the stage properly, we first need to dispel the central myth implied by the question I posed at the beginning: To “believe” or “deny” is not scientific – it's scientific only to say what is more likely and what is less likely. When we're asking questions about the future, unknowns, and “unknown unknowns,” we're dealing with inherent uncertainty, so we can speak only in probabilities. Contrast to belief or denial, skepticism is always a defensible position because it has to do with examining and interpreting evidence. With that in mind, we can properly analyze the climate debate, and each draw our own conclusions based on what the available evidence tells us (or doesn't tell us). It's best to break the debate down into more specific questions so we can get the fullest possible picture of what we're facing. Those questions are:

  1. Observations: Is Earth's climate changing? Is global warming real?

  2. Attribution: To what degree are humans responsible?

  3. Risks: What could the consequences of climate change be for life on Earth?

  4. Decisions: What should we do about it? What are the trade-offs?


1. Observations

The first thing to do is get our terms right. Strictly speaking, Earth doesn't have a “climate” unless we're comparing broad eras against each other, or broadly comparing our planet to another planet. We talk about “climate change” because of how the properties of certain regional climates around the world are changing. Next, it's important to know that Earth's temperature is always changing, and always has been. Over a timescale contextual to Earth's age – in other words, beyond that of our human perception – flux is the rule, not the exception. By measuring proxy indicators like fossilized tree rings and dissolved gasses in ice cores, scientists are able to get an approximation of the conditions that existed long ago. That data is used to chart the temperature from a given region over a long period of time, resulting in the figures below that show that temperature has varied enormously over the last hundred thousand years, let alone the last million.


Earth's temperature is determined by its “energy balance” – the amount of the Sun's energy that stays in our atmosphere to keep the planet warm, compared to how much of that energy is reflected and lost back into space. The energy balance is in turn determined by net “radiative forcing,” which is a technical term that describes the impact of the different gases and other climate-affecting factors. I'll elaborate more about the factors that affect radiative forcing under the Risks section. But first, let's focus on the actual temperature trends.






As we can see from the third figure, around 12 000 years ago a dramatic warming took place as the planet emerged from the last Ice Age, due to predictable shifts in Earth's axial tilt and orbit around the Sun, known as the Milankovitch cycles. This moment marked the beginning of the Holocene Climatic Optimum that we are still in currently. It's no accident that the Holocene coincided with the agricultural revolution, which enabled human societies to gain complexity and flourish on the back of farming techniques that weren't possible in a colder climate. We can also see that the Holocene has featured its own temperature fluctuations, though they are much smaller than those witnessed over a longer timescale. However, it's important to note that the period two to three hundred years ago, known as the Little Ice Age, was significantly cooler than today.

Finally, the figure above shows that our planet's global average temperature has indeed warmed about 0.8ºC since we began actively measuring it using thermometers toward the end of the 19th century. That fact is not in dispute, even by scientists like Richard Lindzen who are skeptical of the notion that we're headed for imminent catastrophe. Those who refer to climate change as a hoax, on the other hand, are flatly wrong: Earth's climates are changing, and global warming is definitely “real” because the global average temperature is rising. We often hear that Earth is warmer now than it has been in at least two millenia, and that sounds pretty staggering. But we should take that statement with a grain of salt, and pause to consider that 2000 years is literally a blink of an eye relative to our planet's history. The graphs tell us that 0.8ºC of warming over 120 years or so isn't incredibly rare. However, if the century-long warming trend continues at its current pace over the coming decades, it would give much more weight to suspicions that we've entered a unique era that life on Earth hasn't experienced before.

Carbon Dioxide





Another key observation, seen in the first two graphs above, is that Earth's atmosphere now contains 400 parts per million (ppm) of carbon dioxide (CO2), a level not seen for the last 3.6 million years. Again, we need to look at this in context: the third graph above shows that our atmosphere's CO2 content has varied greatly over Earth's history, and has been much, much higher in the (deep) past. Contrary to what you've probably heard, carbon dioxide isn't a pollutant – a higher CO2 concentration encourages plant growth, leading to lush forests. In turn, the presence of all that extra O2-emitting vegetation raises the air's oxygen content. Our atmosphere is currently 21% oxygen, but 300 million years ago it was 35%, which enabled insects to become….larger.

In other words, carbon dioxide by itself isn't necessarily bad. The first problem, as we can see from the second graph, is that by burning fossil fuels we have greatly increased the atmosphere's CO2 content virtually overnight, as far as the planet is concerned. Earth may have experienced much higher CO2 levels before, but those increases always occurred so gradually that plant life had time to adapt and accommodate it into the carbon cycle. Since the first industrial revolution began roughly a century ago, combustion of fossil fuels has artificially added more than 100 ppm of CO2 to the atmosphere – at least 1 ppm per year. Our current pace is more like 2-3 ppm per year, and other things being equal, that rate is only going to increase from here as our economic activity continues to expand. It's impossible to know for sure, but it's doubtful that the carbon cycle will be able to accommodate this new CO2 fast enough to prevent it from having knock-on effects that will increase Earth's energy balance (ie. warm the planet). It's estimated that, at minimum, we're locked into another 0.6ºC of global warming thanks to the CO2 that's already been emitted.


2. Attribution

As was mentioned earlier, there's little to no dispute over whether Earth's average temperature has been rising over the last century. The question that skeptics raise, however, is how much human activity has contributed to that rise. The technical name for human culpability is Anthropogenic Global Warming (AGW). In fact, some believe that human impact on the planet is having such profound consequences that in the last two centuries we've moved beyond the Holocene era, and entered the Anthropocene era (the prefix anthro- meaning “human”).

By comparing the graphs showing our CO2 emissions since 1880 with the temperature rise over the same period, and noting that the curves look suspiciously similar, it seems obvious that human activity plays a large role in warming the planet artificially. Not only do we artificially release CO2 by burning fossil fuels, but we also cut down forests that would otherwise remove CO2 from the air (known as “carbon sinks”), and we raise livestock that emit large amounts of methane – a greenhouse gas whose lifetime in the atmosphere is short, but that traps 30 times more heat than CO2.

But while the Intergovernmental Panel on Climate Change (IPCC) attributes most of the warming to human action, skeptics like Richard Lindzen (Professor of Meteorology at MIT until his retirement in 2013) are much more reluctant to conclude the same, arguing that according to his interpretation of the evidence, AGW accounts for maybe half of the observed warming at most (the other half being caused by natural factors). For those so inclined, you can watch Lindzen explain his views in depth here.

Skeptics have two main criticisms of the AGW hypothesis. First, they point out that there has been very little rise in the average global temperature since 1998, even though CO2 emissions have been steadily increasing the whole time. If human emissions are responsible for warming, why hasn't the warming trend also continued in a predictable fashion?

An apparent reply to this point is that Earth's thermal inertia delays the full amount of warming, and that in any case much of the “missing” warming can in fact be accounted for in the ocean. Also, it's the much longer trends spanning a century or more that we should pay the most attention to, because short term variability is inevitable. Still, only more time and study will allow us to answer these sorts of questions with greater confidence.

Skeptics' second criticism has to do with the IPCC's computer models, which are responsible for having produced the predictions of warming ranging from 2ºC to 6ºC (above the 20th century's average temperature) by the 21st century's end given various possible emission scenarios. As the figure below demonstrates, the models used to predict global warming have diverged considerably from the observed temperature so far. Skeptics ask how we can put so much faith in the models' future predictions, given that their predictions so far have been disproven by reality.

Climate Modelling


The economist William Nordhaus explains that the modelling process involves

An experiment in which (case 1) modelers put the changes in CO2 concentrations and other climate influences in a climate model and estimate the resulting temperature path, and then (case 2) modelers calculate what would happen in the counterfactual situation where the only changes were due to natural sources, for example, the sun and volcanoes, with no human-induced changes….This experiment showed that the projections of climate models are consistent with recorded temperature trends over recent decades only if human impacts are included.i

But climate modelling isn't perfect, and it relies on the assumption that if we can understand the factors that caused past climate trends, and use that data in the models, then in theory our models should be able to predict future trends fairly accurately. The IPCC acknowledges that the power offered by models is limited, and wrote in its Third Assessment Report that

In climate research and modeling, we should recognize that....the long-term prediction of future climate states is not possible. The most we can expect to achieve is the prediction of the probability distribution of the system’s future possible states by the generation of ensembles of model solutions.ii

Rather than being able to predict the future precisely, the models offer a range of possible outcomes. However, as the above graph shows, most of the models have so far estimated that warming was going to be greater than it's actually been over the last 22 years. Many of the models have given high warming estimates because they assume that CO2 emissions will trigger “positive feedback loops” that will magnify warming, though it's tough to say by how much. Skeptics like Lindzen argue that the models fail because they overestimate the effects of those positive feedback loops. In fact, in his opinion the models don't account enough for negative feedback loops. I'll explain more about feedback loops in the next section.


3. Risks

So we know that Earth is warming, and we know that we're rapidly adding CO2 to the atmosphere. What we don't know is the precise effects it will have on the biosphere, much less individual ecosystems. But we have some idea of the possibilities.

Cascade of Uncertainty

The picture above is known as the Cascade of Uncertainty. As the name suggests, it represents the range of possible (and not entirely known) effects that greenhouse gas (GHG) emissions could have on the globe's temperature, and the further effects that that rise in temperature could have on individual geographic areas. The greatest uncertainty revolves around what's known as “climate sensitivity”: we simply can't be sure how easily regional climates or local ecosystems will be altered by shifts in air and ocean temperature, or by the changing balance of gasses in the air and water. Perhaps, as climate skeptics contend, various climates will prove resilient to change: maybe human action is in fact relatively impotent, and we can't control nearly as much as we thought we could. That would mean that we haven't really got much to worry about, or at least that reducing our GHG emissions is futile, and that we should focus instead on adapting to our impending new situation.

But maybe regional climates are more delicate than we had anticipated, and human action is in the process of setting off chain reactions called “positive feedback loops” and “tipping points” – some that we might not even be aware of – that could cause enormous upheaval in the coming decades. It's the possibility of this second scenario that demands our prudence.

Feedback Loops

Probably the most well understood positive feedback loop has to do with albedo, which refers to how much light reflects off of a given surface. Dark-coloured surfaces have less albedo and absorb more energy, which is why they are darkly coloured (because less light reflects off of them back to our eye). For the same reason, light-coloured surfaces, like ice and snow, have a high albedo. This has important implications for Earth's net radiative forcing, because as ice and snow melt due to warmer temperatures, less of the Sun's energy is reflected back into space, which warms the planet further, melts even more ice, and further reduces Earth's albedo.

There are several other confirmed and suspected feedback loops, most of which are “positive” (which is bad). These include an increase in water vapour, changes to the land and ocean carbon cycle, ocean acidification, and cloud formation, all of which you can read more about here.

Another big reason that Richard Lindzen is skeptical about climate “alarmism,” as he calls it, is that in his opinion most estimates of future warming don't account enough for the role played by aerosols, which are very fine particles like dust, smoke, and other pollutant byproducts of human activity (there are also natural aerosols, though). Clouds can't form without aerosols, because water vapour needs a focal point to condense upon in order to form water droplets. Clouds reflect some of the Sun's rays back into space, but also reflect back to Earth some of the light that's reflected off of Earth's surface. Because the exact net effects are still not well understood, and tougher still to model, there's debate over whether aerosols and clouds add to Earth's energy balance, or reduce it as part of a negative feedback loop.

Tipping Points and Irreversibility

There are some suspected positive feedback loops that could represent dangerous “tipping points” because of the sudden and disruptive change they could potentially cause. One of these, mentioned in the link on feedback loops, is the possibility that as arctic permafrost melts, it could release into the atmosphere an enormous amount of dissolved carbon dioxide and methane that's trapped as bubbles in the ice. Such a large dose of GHGs into the air would theoretically accelerate other feedback loops.

Another major risk is posed by disruption to thermohaline circulation. This effect, which has to do with the ocean's heat and salt content, drives ocean currents like the North Atlantic Current, which dictates weather and climate for Europe and North America's east coast. As the video in the link illustrates, it's possible that if global warming caused enough of the Greenland ice sheet to melt, it would dilute the northern Atlantic Ocean, reduce its salt concentration, and could potentially slow or stop the North Atlantic Current. Without that, the European and North American climates would be much colder.

These possible scenarios are both examples of irreversible events. Climatologists also talk about how, as mentioned earlier, even if hypothetically we stopped releasing CO2 into the atmosphere tomorrow, cold-turkey, the GHGs that have already been emitted combined with those that will be released due to feedback loops have locked us into at least another 0.6ºC of further warming. The graph below shows how once released, GHGs linger in the biosphere for hundreds of years, making their presence effectively irreversible on human timescales. If you're interested in learning more about the science involved, this lecture explains it well.


4. Decisions

The most important thing to understand when it comes to the question of “What should we do?” is that the way many people answer that question is determined at least as much by their personal ideological bent as it is by their understanding (or lack thereof) of the relevant science.

It's no surprise that in Canada, people who identify as politically conservative are more likely to oppose state action that legislates measures like carbon taxes or cap-and-trade regimes, purportedly because the measures mentioned would reduce fossil fuel production, and could limit job-creation in the private sector. While they surely care about the future of humanity's place in the natural environment, they place a higher priority on economic benefits in the here and now. People who consider themselves politically progressive, on the other hand, tend to support government action that would discourage or limit GHG emissions, because they view the possible risks posed by AGW as outweighing the immediate economic sacrifices that will have to be made.

But there's a deeper dimension to this debate as well. Progressives tend to approve of government intervention in the economy because they see such action as necessary for preserving a just society, and the possible negative externalities posed by climate change qualify as an injustice that needs to be avoided. Conservatives would generally prefer that government play a smaller role in their lives, so tend to oppose high taxation and what they see as government interference in the economy. This article isn't about ideological divides, but those divides shouldn't be overlooked because many people have political biases one way or another that can cloud their judgment, and can prevent us from pursuing the best policies based on what the balance of the scientific evidence indicates.

The Precautionary Principle

The Precautionary Principle has long been invoked regarding climate change, and operates on the logic of “better safe than sorry,” especially when the stakes are high.

First, a word of caution is necessary, because the Principle has limitations. If it's misapplied, we could end up forsaking potential benefits offered by economic expansion just to avoid frightening climate scenarios that might have a very small chance of coming true. Some climate skeptics argue that abandoning the use of fossil fuels immediately would prevent people in places like China and India from reaching the same standard of living that we in the West enjoy, and that would be profoundly unfair. In his famous TED Talk, the Danish political scientist Bjorn Lomborg argues that in a world of scarcity, we should devote our money and attention to solving more pressing problems first, like hunger, poverty, and disease. Arguments like these shouldn't be dismissed.

But William Nordhaus compares the climate change predicament to a roulette wheel in a casino. Each time we spin the wheel, we resolve one of the uncertainties we face – let's use the steps shown in the Cascade of Uncertainty as a guide. Our first spin determines our accumulated level of GHG emissions a decade from now; a second spin, two decades, etc. Subsequent spins reveal the effects those emissions have on the carbon cycle, global climate sensitivity, and regional ecosystems. If the roulette ball lands on black, the outcomes across these dimensions are better than expected: we all breath a collective sigh of relief, the skeptics tell us that they told us so, and the world continues on with business as usual. If the ball lands on red, the results match or slightly exceed the IPCC's worrying predictions, and the world scrambles to mitigate or adapt to shifting climates and damaged ecosystems.

But if the ball lands on zero or double-zero, our worst fears are confirmed, and humanity is faced with a scenario that it's simply not prepared for. Tipping points are reached, ecosystems are destroyed, certain animal species go extinct, sea levels rise dramatically as the ice sheets in Greenland and West Antarctica melt, and flooding makes low-lying coastal areas like Venice and the Maldives uninhabitable. Furthermore, Nordhaus points out that costly outcomes are more likely: we remain uncertain about how climate works in several ways, and those uncertainties could interact with one another to magnify the changes that might otherwise have been smaller on their own. We also need to try and account for the possibility of “unknown unknowns,” – the questions that we haven't thought to ask yet. Those are the factors that we don't know that we don't know.

Nordhaus says that climate skeptics are in effect suggesting that “the ball will always land in the black pocket,” whereas “a sensible policy would pay a premium to avoid the roulette wheel in a Climate Casino.”iii Most climate skeptics would probably agree that we're playing on a roulette wheel, but they would say that there are more black pockets than red ones, and that “climate alarmism” is more of a political construct than a scientific fact. Still, Richard Lindzen himself has acknowledged that if he turns out to be wrong, and humans really are the main cause of climate change, we can take action in fifty years.

As a single scientist giving an opinion, that's fine. But as a society, we need to make decisions now based both on what the balance of evidence is telling us, and on our level of uncertainty compared to the risks we face. That inherent uncertainty means that there are some things science can't help us with, and those decisions will be informed by how we answer questions of what we value: What level of risk is acceptable? What potential benefits are we willing to sacrifice?


i William D. Nordhaus. March 22, 2012. Why the Global Warming Skeptics Are Wrong. The New York Review of Books. p. 12.

ii IPCC TAR, Working Group I report, Chapter (Emphasis added.)

iii Nordhaus, p. 28.