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Collected data using guided research for various countries on carbon emissions
Produced a graph to represent this data
Made at least 3 comments on findings
Be able to explain the negative effect of carbon emissions on the environment

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https://www.macrotrends.net/countries/GBR/united-kingdom/carbon-co2-emissions

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Carbon dioxide emissions are those stemming from the burning of fossil fuels and the manufacture of cement. They include carbon dioxide produced during consumption of solid, liquid, and gas fuels and gas flaring.

U.K. carbon (co2) emissions for 2019 was 348,920.01, a 3.27% decline from 2018.

U.K. carbon (co2) emissions for 2018 was 360,730.01, a 1.71% decline from 2017.

U.K. carbon (co2) emissions for 2017 was 367,000.00, a 3.63% decline from 2016.

U.K. carbon (co2) emissions for 2016 was 380,810.00, a 5.05% decline from 2015.

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Carbon dioxide emissions are those stemming from the burning of fossil fuels and the manufacture of cement. They include carbon dioxide produced during consumption of solid, liquid, and gas fuels and gas flaring. U.K. carbon (co2) emissions for 2019 was 348,920.01, a 3.27% decline from 2018. U.K.

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CO2 emissions (metric tons per capita) from The World Bank: Data

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https://ourworldindata.org/co2-emissions

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You can download our complete Our World in Data CO ₂ and Greenhouse Gas Emissions database.

Carbon dioxide emissions are the primary driver of global climate change. It's widely recognised that to avoid the worst impacts of climate change, the world needs to urgently reduce emissions. But, how this responsibility is shared between regions, countries, and individuals has been an endless point of contention in international discussions.

This debate arises from the various ways in which emissions are compared: as annual emissions by country; emissions per person; historical contributions; and whether they adjust for traded goods and services. These metrics can tell very different stories.

We teamed up with the YouTube channel, Kurzgesagt, to produce a video which explored these different metrics in detail: 'Who is responsible for climate change? - Who needs to fix it?'. All of the data and research featured in this video is contained in this article: below we look in detail at the many ways emissions are broken down.

This page is just one in our collection of work on CO ₂ and Greenhouse Gas Emissions. The rest can be explored via the navigation menu at the top of this page. There you can explore emissions of other greenhouse gases; where our emissions come from; what trajectories of future emissions look like; and what is driving emissions across the world.

In the navigation menu you also find Country Profiles, so you can see how your country is doing in reducing emissions, and our CO ₂ Data Explorer where you can browse all of these metrics in one place.

Global CO₂ emissions from fossil fuels

Global CO₂ emissions from fossil fuels

How have global emissions of carbon dioxide (CO ₂) changed over time?

In this chart we see the growth of global emissions from the mid-18th century through to today.

We see that prior to the Industrial Revolution, emissions were very low. Growth in emissions was still relatively slow until the mid-20th century. In 1950 the world emitted 6 billion tonnes of CO ₂ .

By 1990 this had almost quadrupled, reaching more than 22 billion tonnes . Emissions have continued to grow rapidly; we now emit over 34 billion tonnes each year .

Emissions growth has slowed over the last few years, but they have yet to reach their peak.

Global CO₂ emissions from fossil fuels and land use change

How have global emissions of carbon dioxide (CO ₂) from fossil fuels and land use changed over time?

In this chart we see the growth of global emissions from the mid-18th century through to today.

We see that while emissions from fossil fuels have increased, emissions from land use change have declined slightly in recent years. Overall, this means total emissions have roughly stabilised over the past decade.

CO₂ emissions by region

This interactive chart shows the breakdown of global CO ₂ emissions by region.

We see that until well into the 20th century, global emissions were dominated by Europe and the United States. In 1900, more than 90% of emissions were produced in Europe or the US; even by 1950, they accounted for more than 85% of emissions each year.

But in recent decades this has changed significantly.

In the second half of the 20th century we see a significant rise in emissions in the rest of the world, particularly across Asia, and most notably, China.

The US and Europe now account for just under one-third of emissions.

Where in the world does the average person emit the most carbon dioxide (CO ₂) each year?

We can calculate the contribution of the average citizen of each country by dividing its total emissions by its population. This gives us CO ₂ emissions per capita. In the visualization we see the differences in per capita emissions across the world.

Here we look at production-based emissions - that is, emissions produced within a country's boundaries without accounting for how goods are traded across the world. In our post on consumption-based emissions we look at how these figures change when we account for trade. Production figures matter - these are the numbers that are taken into account for climate targets¹ - and thanks to historical reconstructions they are available for the entire world since the mid 18th century.

There are very large inequalities in per capita emissions across the world.

The world's largest per capita CO ₂ emitters are the major oil producing countries; this is particularly true for those with relatively low population size. Most are in the Middle East: In 2017 Qatar had the highest emissions at 49 tonnes (t) per person, followed by Trinidad and Tobago (30t); Kuwait (25t); United Arab Emirates (25t); Brunei (24t); Bahrain (23t) and Saudi Arabia (19t).

However, many of the major oil producers have a relatively small population meaning their total annual emissions are low. More populous countries with some of the highest per capita emissions - and therefore high total emissions - are the United States, Australia, and Canada. Australia has an average per capita footprint of 17 tonnes, followed by the US at 16.2 tonnes, and Canada at 15.6 tonnes.

This is more than 3 times higher than the global average, which in 2017 was 4.8 tonnes per person.

Since there is such a strong relationship between income and per capita CO ₂ emissions, we'd expect this to be the case: that countries with high standards of living would have a high carbon footprint. But what becomes clear is that there can be large differences in per capita emissions, even between countries with similar standards of living. Many countries across Europe, for example, have much lower emissions than the US, Canada or Australia.

In fact, some European countries have emissions not far from the global average: In 2017 emissions in Portugal are 5.3 tonnes; 5.5t in France; and 5.8t per person in the UK. This is also much lower than some of their neighbours with similar standards of living, such as Germany, the Netherlands, or Belgium. The choice of energy sources plays a key role here: in the UK, Portugal and France, a much higher share of electricity is produced from nuclear and renewable sources - you can explore this electricity mix by country here. This means a much lower share of electricity is produced from fossil fuels: in 2015, only 6% of France's electricity came from fossil fuels, compared to 55% in Germany.

Prosperity is a primary driver of CO ₂ emissions, but clearly policy and technological choices make a difference.

Many countries in the world still have very low per capita CO ₂ emissions. In many of the poorest countries in Sub-Saharan Africa - such as Chad, Niger and the Central African Republic - the average footprint is around 0.1 tonnes per year. That's more than 160 times lower than the USA, Australia and Canada. In just 2.3 days the average American or Australian emits as much as the average Malian or Nigerien in a year.

This inequality in emissions across the world I explored in more detail in my post, ' Who emits more than their share of CO 2 emissions? '

Who emits the most CO ₂ each year? In the treemap visualization we show annual CO ₂ emissions by country, and aggregated by region. Treemaps are used to compare entities (such as countries or regions) in relation to others, and relative to the total. Here each inner rectangle represents a country - which are then nested and colored by region. The size of each rectangle corresponds to its annual CO ₂ emissions in 2017. Combined, all rectangles represent the global total.

The emissions shown here relate to the country where CO ₂ is produced (i.e.production-based CO ₂) , not to where the goods and services that generate emissions are finally consumed. We look at the difference in each country's production vs. consumption (trade-adjusted) emissions here.

Asia is by far the largest emitter, accounting for 53% of global emissions. As it is home to 60% of the world's population this means that per capita emissions in Asia are slightly lower than the world average, however.

China is, by a significant margin, Asia's and the world's largest emitter: it emits nearly 10 billion tonnes each year, more than one-quarter of global emissions.

North America - dominated by the USA - is the second largest regional emitter at 18% of global emissions. It's followed closely by Europe with 17%. Here we have grouped the 28 countries of the European Union together, since they typically negotiate and set targets as a collective body. You can see the data for individual EU countries in the interactive maps which follow.

Africa and South America are both fairly small emitters: accounting for 3-4% of global emissions each. Both have emissions almost equal in size to international aviation and shipping. Both aviation and shipping are not included in national or regional emissions. This is because of disagreement over how emissions which cross country borders should be allocated: do they belong to the country of departure, or country of origin? How are connecting flights accounted for? The tensions in reaching international aviation and shipping deals are discussed in detail at the Carbon Brief here.

The same data is also explorable by country and over time in the interactive map.

By clicking on any country you can see how its annual emissions have changed, and compare it with other countries.

In the interactive chart you can explore each country's share of global emissions. Using the timeline at the bottom of the map, you can see how the global distribution has changed since 1751. By clicking on any country you can see its evolution and compare it with others.

If you're interested in which countries emit more or less than their 'fair share' based on their share of global population, you can explore this here.

The distribution of emissions has changed significantly over time. The UK was - until 1888, when it was overtaken by the US - the world's largest emitter. This was because the UK was the first country to industrialize, a transition which later contributed to in massive improvements in living standards for much of its population.

Whilst rising CO ₂ emissions have clear negative environmental consequences, it is also true that they have historically been a by-product of positive improvements in human living conditions. But, it's also true that reducing CO ₂ emissions is important to protect the living conditions of future generations. This perspective - that we must consider both the environmental and human welfare implications of emissions - is important if we are to build a future that is both sustainable and provides high standards of living for everyone.

Rising emissions and living standards in North America and Oceania followed soon after developments in the UK.

Many of the world's largest emitters today are in Asia. However, Asia's rapid rise in emissions has only occurred in very recent decades. This too has been a by-product of massive improvements in living standards: since 1950 life expectancy in Asia has increased from 41 to 74 years; it has seen a dramatic fall in extreme poverty; and for the first time most of its population received formal education.

Whilst all countries must work collectively, action from the very top emitters will be essential. China, the USA and the 28 countries of the EU account for more than half of global emissions. Without commitment from these largest emitters, the world will not come close to meeting its global targets.

Annual change in CO₂ emissions

This interactive chart shows the year-on-year growth rate of CO ₂ emissions.

A positive figure in a given year indicates that emissions were higher than the previous year. A negative figure indicates they were lower than the year before. For example, a change of 1.5% indicates that global emissions were 1.5% higher than the previous year [-1.5% would mean they were 1.5% lower].

This measure allows us to see firstly where emissions are rising, and where they are falling; and secondly the rate at which emissions are changing - whether the growth in emissions are slowing down or accelerating.

Since 1751 the world has emitted over 1.5 trillion tonnes of CO ₂.² To reach our climate goal of limiting average temperature rise to 2°C, the world needs to urgently reduce emissions. One common argument is that those countries which have added most to the CO ₂ in our atmosphere - contributing most to the problem today - should take on the greatest responsibility in tackling it.

We can compare each country's total contribution to global emissions by looking at cumulative CO₂. We can calculate cumulative emissions by adding up each country's annual CO ₂ emissions over time. We did this calculation for each country and region over the period from 1751 through to 2017.³

The distribution of cumulative emissions around the world is shown in the treemap. Treemaps are used to compare entities (such as countries or regions) in relation to others, and relative to the total. Here countries are presented as rectangles and colored by region. The size of each rectangle corresponds to the sum of CO ₂ emissions from a country between 1751 and 2017. Combined, all rectangles represent the global total.

There are some key points we can learn from this perspective:

the United States has emitted more CO₂ than any other country to date: at around 400 billion tonnes since 1751, it is responsible for 25% of historical emissions;

this is twice more than China - the world's second largest national contributor;

the 28 countries of the European Union (EU-28) - which are grouped together here as they typically negotiate and set targets on a collaborative basis - is also a large historical contributor at 22%;

many of the large annual emitters today - such as India and Brazil - are not large contributors in a historical context;

Africa's regional contribution - relative to its population size - has been very small. This is the result of very low per capita emissions - both historically and currently.

All of this data is also explorable by country and over time in the interactive map. By clicking on any country you can see the country's cumulative emissions over time, and compare it with other countries.

In the visualizations above we focused on each country or region's total cumulative emissions (1) in absolute terms; and (2) at a single point in time: as of 2017.

In the chart we see the change in the share of global cumulative emissions by region over time - from 1751 through to 2017.

Up until 1950, more than half of historical CO ₂ emissions were emitted by Europe. The vast majority of European emissions back then were emitted by the United Kingdom; as the data shows, until 1882 more than half of the world's cumulative emissions came from the UK alone.

Over the century which followed, industrialization in the USA rapidly increased its contribution.

It's only over the past 50 years that growth in South America, Asia and Africa have increased these regions' share of total contribution.

In the final visualization you can explore the same cumulative CO ₂ emissions as you have seen above but now visualizes by country. Using the timeline at the bottom of the chart you can see how contribution across the world has evolved since 1751. By clicking on a country you can see an individual country's cumulative contribution over time.

The map for 2017 shows the large inequalities of contribution across the world that the first treemap visualization has shown. The USA has emitted most to date: more than a quarter of all historical CO ₂: twice that of China which is the second largest contributor. In contrast, most countries across Africa have been responsible for less than 0.01% of all emissions over the last 266 years.

What becomes clear when we look at emissions across the world today is that the countries with the highest emissions over history are not always the biggest emitters today. The UK, for example, was responsible for only 1% of global emissions in 2017. Reductions here will have a relatively small impact on emissions at the global level - or at least fall far short of the scale of change we need. This creates tension with the argument that the largest contributors in the past should be those doing most to reduce emissions today. This is because a large fraction of CO ₂ remains in the atmosphere for hundreds of years once emitted.⁴

This inequality is one of the main reasons which makes international agreement on who should take action so challenging.

Consumption-based (trade-adjusted) emissions

CO ₂ emissions are typically measured on the basis of 'production'. This accounting method - which is sometimes referred to as 'territorial' emissions - is used when countries report their emissions, and set targets domestically and internationally.⁵

In addition to the commonly reported production-based emissions statisticians also calculate 'consumption-based' emissions. These emissions are adjusted for trade. To calculate consumption-based emissions we need to track which goods are traded across the world, and whenever a good was imported we need to include all CO ₂ emissions that were emitted in the production of that good, and vice versa to subtract all CO ₂ emissions that were emitted in the production of goods that were exported.

Consumption-based emissions reflect the consumption and lifestyle choices of a country's citizens.

In the interactive map we see the emissions of traded goods. To give a perspective on the importance of trade these emissions are put in relation to the country's domestic, production-based emissions.⁶

Countries shown in red are net importers of emissions - they import more CO₂ embedded in goods than they export.

For example, the USA has a value of 7.7% meaning its net import of CO₂ is equivalent to 7.7% of its domestic emissions. This means emissions calculated on the basis of 'consumption' are 7.7% higher than their emissions based on production.

Countries shown in blue are net exporters of emissions - they export more CO₂ embedded in goods than they import.

For example, China's value of -14% means its net export of CO₂ is equivalent to 14% of its domestic emissions. The consumption-based emissions of China are 14% lower than their production-based emissions.

We see quite a regional East-West split in net exporters and importers: most of Western Europe, the Americas, and many African countries are net importers of emissions whilst most of Eastern Europe and Asia are net exporters.

You can find these figures in absolute (tonnes of CO ₂) and per capita terms for each country in the Additional Information section.

How did the differences between a country's production and consumption-based emissions change over time?

In the interactive charts you can compare production- and consumption-based emissions for many countries and world regions since the first data is available in 1990.⁷ One chart shows total annual emissions, the other one shows the same on a per capita basis. Using the 'change country' toggle of the chart you can switch between them.

Individual maps of consumption-based annual and per capita emissions can also be found in the Additional Information which follows this post.

We see that the consumption-based emissions of the US are higher than production: In 2016 the two values were 5.7 billion versus 5.3 billion tonnes - a difference of 8%. This tells us that more CO ₂ is emitted in the production of the goods that Americans import than in those products Americans export.

The opposite is true for China: its consumption-based emissions are 14% lower than its production-based emissions. On a per capita basis, the respective measures are 6.9 and 6.2 tonnes per person in 2016. A difference, but smaller than what many expect.

Whilst China is a large CO ₂ emissions exporter, it is no longer a large emitter because it produces goods for the rest of the world. This was the case in the past, but today, even adjusted for trade, China now has a per capita footprint higher than the global average (which is 4.8 tonnes per capita in 2017). In the Additional Information you find an interactive map of how consumption-based emissions per capita vary across the world.

These comparisons provide the answer to the question whether countries have only achieved emissions reductions by offshoring emissions intensive production to other countries. If only production-based emissions were falling whilst consumption-based emissions were rising, this would suggest it was 'offshoring' emissions elsewhere.

There are some countries where this is the case. Examples where production-based emissions have stagnated whilst consumption-based CO ₂ steadily increased include Ireland in the early 2000s; Norway in the late 1990s and early 2000s; and Switzerland since 1990.

On the other hand there are several very rich countries where both production- and consumption-based emissions have declined. This has been true, among others, for the UK ( chart), France ( chart), Germany ( chart), and the USA ( chart). These countries have achieved some genuine reductions without outsourcing the emissions to other countries. Emissions are still too high in all of these countries, but it shows that genuine reductions are possible.

In most countries emissions increased when countries become richer, but this is also not necessarily the case: by comparing the change in consumption-based emissions and economic growth we see that many countries have become much richer while achieving a reduction of emissions.

In-depth: how much emissions are embedded in trade?

Decoupling CO₂ emissions from economic growth

Historically, CO ₂ emissions have been strongly correlated with how much money we have. This is particularly true at low-to-middle incomes. The richer we are, the more CO ₂ we emit. This is because we use more energy - which often comes from burning fossil fuels.

But this relationship no longer holds true at higher incomes. Many countries have managed to achieve economic growth while reducing emissions. They have decoupled the two.

Take the UK as an example. It is shown in the chart. This chart shows the change in GDP and annual CO ₂ emissions per capita since 1990. We see that the UK's GDP has increased a lot over the last 30 years, while its emissions have fallen. You can also see the data without per capita adjustments.

It's not just the UK. Many other countries have achieved this decoupling. Using the "Change country" button on the chart, you can see this for yourself. France, Germany, Sweden, Finland, Denmark, Italy, Czechia and Romania are some examples of countries where we see this.

More countries have managed to decouple more recently. Emissions in the US, for example, increased substantially in the 1990s. This means that its emissions today are still higher than in 1990. But if we look at the change since 2000 [you can do this by adjusting the time-slider on the bottom of the chart] we see a large drop in emissions alongside a rise in GDP. It's only over the last 20 years that this decoupling has started to happen.

There are two key reasons why emissions have fallen in these countries. First, some countries have managed to decouple energy use and economic growth. GDP has increased while total energy use has remained flat, or even fallen. But the second is the most important: countries are replacing fossil fuels with low-carbon energy. We can produce more energy, without the emissions that used to come with it.

It would be wrong to assume that this reduction in emissions in rich countries was only achieved by offshoring production overseas - by transferring emissions to manufacturing economies such as China and India. In the chart we see that consumption-based emissions - which adjust for emissions from goods that are imported or exported - have also fallen. Some emissions have been exported overseas, but this is not the only driver of this decline.

These countries show that economic growth is not incompatible with reducing emissions.

A key question is whether we can decarbonize fast enough, and across more countries. The continued decline in the cost of low-carbon technologies makes this acceleration more realistic every day.

Global inequalities in CO₂ emissions

Global inequalities by production

There are two parameters that determine our collective carbon dioxide (CO ₂) emissions: the number of people, and quantity emitted per person. We either talk about total annual or per capita emissions. They tell very different stories and this often results in confrontation over who can really make an impact: rich countries with high per capita emissions, or those with a large population.

To help us understand the global distribution of per capita emissions and population, we have visualized global CO 2 emissions by (1) World Bank income group and (2) by world region.

The world's total CO ₂ emissions⁹ are shown on the basis of two axes: the height of the bar (y-axis) is the average per capita CO ₂ emissions and the length of the box (x-axis) is the total population. Since total emissions are equal to per capita emissions multiplied by the number of people, the area of each box represents total emissions.¹⁰

When aggregated in terms of income, we see in the visualization that the richest half (high and upper-middle income countries) emit 86 percent of global CO ₂ emissions. The bottom half (low and lower-middle income) only 14%. The very poorest countries (home to 9 percent of the global population) are responsible for just 0.5 percent. This provides a strong indication of the relative sensitivity of global emissions to income versus population. Even several billion additional people in low-income countries - where fertility rates and population growth is already highest - would leave global emissions almost unchanged. 3 or 4 billion low income individuals would only account for a few percent of global CO ₂. At the other end of the distribution however, adding only one billion high income individuals would increase global emissions by almost one-third.¹¹

Note here that the summary by income is on the basis of country income groupings, rather than that of individuals. For example, 'low income' is the total emissions of all countries defined as low income, rather than the lowest income individuals in the world. These figures therefore don't take account of inequalities in emissions within countries. It's estimated that within-country inequalities in emissions can be as large as those between countries.¹²

If we were to calculate this distribution by the income of individuals, rather than countries, we'd see that the global inequalities in emissions would be even greater. The richest of the global population would be responsible for an even larger share of global emissions.

When aggregated by region we see that North America, Oceania, Europe, and Latin America have disproportionately high emissions relative to their population. North America is home to only five percent of the world population but emits nearly 18 percent of CO ₂ (almost four times as much). Asia and Africa are underrepresented in emissions. Asia is home to 60 percent of the population but emits just 49 percent; Africa has 16 percent of the population but emits just 4 percent of CO ₂. This is reflected in per capita emissions; the average North American is more than 17 times higher than the average African.

This inequality in global emissions lies at the heart of why international agreement on climate change has (and continues to be) so contentious. The richest countries of the world are home to half of the world population, and emit 86 percent of CO ₂ emissions. We want global incomes and living standards - especially of those in the poorest half - to rise. To do so whilst limiting climate change, it's clear that we must shrink the emissions of high-income lifestyles. Finding the compatible pathway for levelling this inequality is one of the greatest challenges of this century.
[Clicking on the visualization will open it in higher-resolution].

Global inequalities by consumption

The initial comparison of emissions by income group and region was based on 'territorial' emissions (those emitted within a country's borders) - these are termed 'production-based' and are the metrics by which emissions are commonly reported. However, these emissions do not account for traded goods (for which CO ₂ was emitted for their production). If a country is a large importer of goods its production-based emissions would underestimate the emissions required to support its standard of living. Conversely, if a country is a large goods exporter, it includes emissions within its accounts which are ultimately exported for use or consumption elsewhere.

'Consumption-based' emissions correct for this by adjusting for trade. Consumption-based emissions are therefore: (production-based emissions - embedded CO ₂ in exported goods + embedded CO2 in imported goods). The Global Carbon Project (GCP) publishes estimates of these adjustments in their carbon budget.¹³ You can find much more information and data on emissions in trade in our full entry here.

How do consumption-based emissions change the emission shares by income group and region? In the table I compare each group's share of the world population, production- and consumption-based CO ₂ emissions.

On a production basis we had previously found that the richest (high and upper-middle income) countries in the world accounted for half of the population but 86 percent of emissions.¹⁴ On a consumption basis we find the same result, but resulting from the fact that upper-middle income countries primarily export emissions to high income countries. High income countries' collective emissions increase from 39 to 46 percent when adjusted for trade (with only 16 percent of the population); upper-middle income countries' emissions decrease by the same amount (7 percentage points) from 48 to 41 percent. Overall, this balances out in the top half of the world population: upper-middle income countries are net exporters whilst high income net importers.

In the bottom half, it appears that very little changes for the collective of lower-middle and low income countries: their production and consumption emissions shares are effectively the same.

By region we see that traded emissions tend to flow from Asia to North America and Europe (Asia's share reduces when adjusted for trade whilst North America and Europe's share increases).

Note here that consumption-based emissions are not available for all countries. Collectively, countries without consumption-based estimates due to poor data availability account for approximately 3 percent of global emissions. Many of the missing countries are at low and lower-middle incomes. With the addition of these countries, we would expect small percentage point shifts across the distribution. The challenges in accounting for carbon embedded in global trade¹⁵ mean these estimates are not perfect; nonetheless they should provide a good approximation of the global transfers across the world.

On a consumption basis, high-income countries (Europe and North America in particular) account for an even larger share of global emissions (46 percent - nearly three times their population share of 16 percent).

Income or regional group

Share of population (%)

Share of production-based CO₂ emissions (%)

Share of consumption-based CO₂ emissions (%)

How do we measure or estimate CO₂ emissions?

Historical fossil fuel CO ₂ emissions can be reconstructed back to 1751 based on energy statistics. These reconstructions detail the production quantities of various forms of fossil fuels (coal, brown coal, peat and crude oil), which when combined with trade data on imports and exports, allow for national-level reconstructions of fossil fuel production and resultant CO ₂ emissions. More recent energy statistics are sourced from the UN Statistical Office, which compiles data from official national statistical publications and annual questionnaires. Data on cement production and gas flaring can also be sourced from UN data, supplemented by data from the US Department of Interior Geological Survey (USGS) and US Department of Energy Information Administration. A full description of data acquisition and original sources can be found at the Carbon Dioxide Information Analysis Center (CDIAC).

As an example: how do we estimate Canada's CO 2 emissions in 1900? Let's look at the steps involved in this estimation.

Step 1: we gather industrial data on how much coal, brown coal, peat and crude oil Canada extracted in 1900. This tells us how much energy it could produce if it used all of this domestically.

Step 2: we cannot assume that Canada only used fuels produced domestically-it might have imported some fuel, or exported it elsewhere. To find out how much Canada actually burned domestically, we therefore have to correct for this trade. If we take its domestic production (account for any fuel it stores as stocks), add any fuel it imported, and subtract any fuel it exported, we have an estimate of its net consumption in 1900. In other words, if we calculate: Coal extraction − Coal exported + Coal imported − Coal stored as stocks, we can estimate the amount of coal Canada burned in 1900.

Step 3: converting energy produced to CO₂ emissions. we know, based on the quality of coal, its carbon content and how much CO₂ would be emitted for every kilogram burned (i.e. its emission factor). Multiplying the quantity of coal burned by its emission factor, we can estimate Canada's CO₂ emissions from coal in 1900.

Step 4: doing this calculation for all fuel types, we can calculate Canada's total emissions in 1900.

Providing good estimates of CO ₂ emissions requires reliable and extensive coverage on domestic and traded energy-the international framework and monitoring of this reporting has significantly improved through time. For this reason, our understanding of emissions in the late 20th and 21st centuries is more reliable than our long-term reconstructions. The Intergovernmental Panel on Climate Change (IPCC) provide clear guidelines on methodologies and best practice for measuring and monitoring CO ₂ estimates at the national level.¹⁶

There are two key ways uncertainties can be introduced: the reporting of energy consumption, and the assumption of emissions factors (i.e. the carbon content) used for fuel burning. Since energy consumption is strongly related to economic and trade figures (which are typically monitored closely), uncertainties are typically low for energy reporting. Uncertainty can be introduced in the assumptions nations make on the correct CO ₂ emission factor for certain fuel types.

Country size and the level of uncertainty in these calculations have a significant influence on the inaccuracy of our global emissions figures. In the most extreme example to date, Lui et al. (2015) revealed that China overestimated its annual emissions in 2013 by using global average emission factors, rather than specific figures for the carbon content of its domestic coal supply.¹⁷

As the world's largest CO ₂ emitter, this inaccuracy had a significant impact on global emissions estimates, resulting in a 10% overestimation. More typically, uncertainty in global CO ₂ emissions ranges between 2-5%.¹⁸

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How much CO2 does the world emit? Which countries emit the most?

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The students will have produced posters showing their findings and presentations will be recorded. These could then be presented at an assembly in school.

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Example graph comparing carbon emissions in different countries

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Example graph comparing carbon emissions in different countries

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At the end of the project, students can present their findings to the rest of the school to raise awareness to the rest of the school about the impact of climate change and why it is important for us to make changes now

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Take data on carbon emissions from relatable countries (including the UK and other countries students may come from/visit).
Realise that these issues are not "far away" and can be avoided.
Understand the impact of carbon emissions on the environment.
Understand how we can lower carbon emissions and help fight climate change.

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Calculating averages.
Plotting bar charts, line graphs, histograms.
Interpreting graphs.
Analysing data.
Teamwork.
Presenting findings in a visual way alongside explanations.

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The comparison of carbon emissions around the world.
The impact of carbon emissions on the environment.

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Since our students are based in Birmingham City they may be exposed to types of carbon emissions like local factories that burn fossil fuels/power stations and also transportation. These examples can be presented to support the students in understanding the context for an environment they are familiar in

Relevance: Students will feel the lesson is more relatable and therefore this should increase engagement.

Students have previously expressed dissatisfaction in climate change lessons because they are based on other countries which are far away. If the data that the students use refers to countries like the UK or other countries, which are represented throughout the class, it will be more relatable. This will lead to increased engagement and the message about climate change will be stronger.

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Ensure students can calculate averages:
mean, median, mode, range.

Climate change literacy:
carbon emissions - define keyword and describe how these emissions impact us and contribute to climate change.

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Names: Grace Sinclair, Sufyaan Khan, Jakub Miskiewicz, Adil Suleman
Group: 5
Subject: Maths

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1. To enable pupils to analyse data around carbon emissions around the world.

2. To make cross-country comparisons by calculating per capita emissions which compares the carbon emissions against total population for different countries for one specific year (i.e. 2019)

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Effect of carbon dioxide on climate change

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Effect of carbon dioxide on climate change

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Based on the annual report from NOAA's Global Monitoring Lab, global average atmospheric carbon dioxide was 417.06 parts per million ("ppm" for short) in 2022, setting a new record high. The increase between 2021 and 2022 was 2.13 ppm-the 11 th year in a row where the amount of carbon dioxide in the atmosphere increased by more than 2 ppm. At Mauna Loa Observatory in Hawaii, where the modern carbon dioxide record began in 1958, the annual average carbon dioxide in 2022 was 418.56.

Carbon dioxide concentrations are rising mostly because of the fossil fuels that people are burning for energy. Fossil fuels like coal and oil contain carbon that plants pulled out of the atmosphere through photosynthesis over many millions of years; we are returning that carbon to the atmosphere in just a few hundred. Since the middle of the 20 th century, annual emissions from burning fossil fuels have increased every decade, from close to 11 billion tons of carbon dioxide per year in the 1960s to an estimated 36.6 billion tons in 2022 according to the Global Carbon Budget 2022.

Carbon cycle experts estimate that natural "sinks"-processes that remove carbon from the atmosphere-on land and in the ocean absorbed the equivalent of about half of the carbon dioxide we emitted each year in the 2011-2020 decade. Because we put more carbon dioxide into the atmosphere than natural sinks can remove, the total amount of carbon dioxide in the atmosphere increases every year.

The more we overshoot what natural processes can remove in a given year, the faster the atmospheric concentration of carbon dioxide rises. In the 1960s, the global growth rate of atmospheric carbon dioxide was roughly 0.8± 0.1 ppm per year. Over the next half century, the annual growth rate tripled, reaching 2.4 ppm per year during the 2010s. The annual rate of increase in atmospheric carbon dioxide over the past 60 years is about 100 times faster than previous natural increases, such as those that occurred at the end of the last ice age 11,000-17,000 years ago.

Why carbon dioxide matters

Carbon dioxide is Earth's most important greenhouse gas: a gas that absorbs and radiates heat. Unlike oxygen or nitrogen (which make up most of our atmosphere), greenhouse gases absorb heat radiating from the Earth's surface and re-release it in all directions-including back toward Earth's surface. Without carbon dioxide, Earth's natural greenhouse effect would be too weak to keep the average global surface temperature above freezing. By adding more carbon dioxide to the atmosphere, people are supercharging the natural greenhouse effect, causing global temperature to rise. According to observations by the NOAA Global Monitoring Lab, in 2021 carbon dioxide alone was responsible for about two-thirds of the total heating influence of all human-produced greenhouse gases.

Another reason carbon dioxide is important in the Earth system is that it dissolves into the ocean like the fizz in a can of soda. It reacts with water molecules, producing carbonic acid and lowering the ocean's pH (raising its acidity). Since the start of the Industrial Revolution, the pH of the ocean's surface waters has dropped from 8.21 to 8.10. This drop in pH is called ocean acidification.

Past and future carbon dioxide

Natural increases in carbon dioxide concentrations have periodically warmed Earth's temperature during ice age cycles over the past million years or more. The warm episodes (interglacials) began with a small increase in incoming sunlight in the Northern Hemisphere due to variations in Earth's orbit around the Sun and its axis of rotation. (For more details, see the "Milankovitch cycles and ice ages" section of our Climate change: incoming sunlight article.) That little bit of extra sunlight caused a little bit of warming. As the oceans warmed, they outgassed carbon dioxide-like a can of soda going flat in the heat of a summer day. The extra carbon dioxide in the atmosphere greatly amplified the initial, solar-driven warming.

Based on air bubbles trapped in mile-thick ice cores and other paleoclimate evidence, we know that during the ice age cycles of the past million years or so, atmospheric carbon dioxide never exceeded 300 ppm. Before the Industrial Revolution started in the mid-1700s, atmospheric carbon dioxide was 280 ppm or less.

By the time continuous observations began at Mauna Loa Volcanic Observatory in 1958, global atmospheric carbon dioxide was already 315 ppm. Carbon dioxide levels today are higher than at any point in human history. In fact, the last time atmospheric carbon dioxide amounts were this high was more than 3 million years ago, during the Mid-Pliocene Warm Period, when global surface temperature was 4.5-7.2 degrees Fahrenheit (2.5-4 degrees Celsius) warmer than during the pre-industrial era. Sea level was at least 16 feet higher than it was in 1900 and possibly as much as 82 feet higher.

If global energy demand continues to grow rapidly and we meet it mostly with fossil fuels, human emissions of carbon dioxide could reach 75 billion tons per year or more by the end of the century. Atmospheric carbon dioxide could be 800 ppm or higher-conditions not seen on Earth for close to 50 million years.

More on carbon dioxide
NOAA carbon dioxide observations Carbon cycle factsheet Carbon dioxide emissions by country over time Comparing greenhouse gases by their global warming potential Ocean acidification
References

Collins, M., R. Knutti, J. Arblaster, J.-L. Dufresne, T. Fichefet, P. Friedlingstein, X. Gao, W.J. Gutowski, T. Johns, G. Krinner, M. Shongwe, C. Tebaldi, A.J. Weaver and M. Wehner, 2013: Long-term Climate Change: Projections, Commitments and Irreversibility. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.

Friedlingstein, P., O'Sullivan, M., Jones, M. W., Andrew, R. M., Gregor, L., Hauck, J., Le Quéré, C., Luijkx, I. T., Olsen, A., Peters, G. P., Peters, W., Pongratz, J., Schwingshackl, C., Sitch, S., Canadell, J. G., Ciais, P., Jackson, R. B., Alin, S. R., Alkama, R., ... Zheng, B. (2022). Global Carbon Budget 2022. Earth System Science Data, 14(11), 4811-4900. https://doi.org/10.5194/essd-14-4811-2022

Lan, X., B. D. Hall, G. Dutton, J. Mühle, J. W. Elkins, and I. J. Vimont. (2022). Long-lived greenhouses gases [in State of the Climate in 2021, Chapter 2: Global Climate]. Bulletin of the American Meteorological Society, 103 (8), S81-S84. https://doi.org/10.1175/BAMS-D-22-0092.1.

Lüthi, D., M. Le Floch, B. Bereiter, T. Blunier, J.-M. Barnola, U. Siegenthaler, D. Raynaud, J. Jouzel, H. Fischer, K. Kawamura, and T.F. Stocker. (2008). High-resolution carbon dioxide concentration record 650,000-800,000 years before present. Nature, Vol. 453, pp. 379-382. doi:10.1038/nature06949.

Woods Hole Oceanographic Institution. (2015). Introduction to ocean acidification. Accessed October 4, 2017.

Lindsey, R. (2009). Climate and Earth's energy budget. Accessed October 4, 2017.

Based on the annual report from NOAA's Global Monitoring Lab, global average atmospheric carbon dioxide was 417.06 parts per million ("ppm" for short) in 2022, setting a new record high. The increase between 2021 and 2022 was 2.13 ppm-the 11 th year in a row where the amount of carbon dioxide in the atmosphere increased by more than 2 ppm. At Mauna Loa Observatory in Hawaii, where the modern carbon dioxide record began in 1958, the annual average carbon dioxide in 2022 was 418.56.

Carbon dioxide concentrations are rising mostly because of the fossil fuels that people are burning for energy. Fossil fuels like coal and oil contain carbon that plants pulled out of the atmosphere through photosynthesis over many millions of years; we are returning that carbon to the atmosphere in just a few hundred. Since the middle of the 20 th century, annual emissions from burning fossil fuels have increased every decade, from close to 11 billion tons of carbon dioxide per year in the 1960s to an estimated 36.6 billion tons in 2022 according to the Global Carbon Budget 2022.

Carbon cycle experts estimate that natural "sinks"-processes that remove carbon from the atmosphere-on land and in the ocean absorbed the equivalent of about half of the carbon dioxide we emitted each year in the 2011-2020 decade. Because we put more carbon dioxide into the atmosphere than natural sinks can remove, the total amount of carbon dioxide in the atmosphere increases every year.

The more we overshoot what natural processes can remove in a given year, the faster the atmospheric concentration of carbon dioxide rises. In the 1960s, the global growth rate of atmospheric carbon dioxide was roughly 0.8± 0.1 ppm per year. Over the next half century, the annual growth rate tripled, reaching 2.4 ppm per year during the 2010s. The annual rate of increase in atmospheric carbon dioxide over the past 60 years is about 100 times faster than previous natural increases, such as those that occurred at the end of the last ice age 11,000-17,000 years ago.

Why carbon dioxide matters

Carbon dioxide is Earth's most important greenhouse gas: a gas that absorbs and radiates heat. Unlike oxygen or nitrogen (which make up most of our atmosphere), greenhouse gases absorb heat radiating from the Earth's surface and re-release it in all directions-including back toward Earth's surface. Without carbon dioxide, Earth's natural greenhouse effect would be too weak to keep the average global surface temperature above freezing. By adding more carbon dioxide to the atmosphere, people are supercharging the natural greenhouse effect, causing global temperature to rise. According to observations by the NOAA Global Monitoring Lab, in 2021 carbon dioxide alone was responsible for about two-thirds of the total heating influence of all human-produced greenhouse gases.

Another reason carbon dioxide is important in the Earth system is that it dissolves into the ocean like the fizz in a can of soda. It reacts with water molecules, producing carbonic acid and lowering the ocean's pH (raising its acidity). Since the start of the Industrial Revolution, the pH of the ocean's surface waters has dropped from 8.21 to 8.10. This drop in pH is called ocean acidification.

Past and future carbon dioxide

Natural increases in carbon dioxide concentrations have periodically warmed Earth's temperature during ice age cycles over the past million years or more. The warm episodes (interglacials) began with a small increase in incoming sunlight in the Northern Hemisphere due to variations in Earth's orbit around the Sun and its axis of rotation. (For more details, see the "Milankovitch cycles and ice ages" section of our Climate change: incoming sunlight article.) That little bit of extra sunlight caused a little bit of warming. As the oceans warmed, they outgassed carbon dioxide-like a can of soda going flat in the heat of a summer day. The extra carbon dioxide in the atmosphere greatly amplified the initial, solar-driven warming.

Based on air bubbles trapped in mile-thick ice cores and other paleoclimate evidence, we know that during the ice age cycles of the past million years or so, atmospheric carbon dioxide never exceeded 300 ppm. Before the Industrial Revolution started in the mid-1700s, atmospheric carbon dioxide was 280 ppm or less.

By the time continuous observations began at Mauna Loa Volcanic Observatory in 1958, global atmospheric carbon dioxide was already 315 ppm. Carbon dioxide levels today are higher than at any point in human history. In fact, the last time atmospheric carbon dioxide amounts were this high was more than 3 million years ago, during the Mid-Pliocene Warm Period, when global surface temperature was 4.5-7.2 degrees Fahrenheit (2.5-4 degrees Celsius) warmer than during the pre-industrial era. Sea level was at least 16 feet higher than it was in 1900 and possibly as much as 82 feet higher.

If global energy demand continues to grow rapidly and we meet it mostly with fossil fuels, human emissions of carbon dioxide could reach 75 billion tons per year or more by the end of the century. Atmospheric carbon dioxide could be 800 ppm or higher-conditions not seen on Earth for close to 50 million years.

More on carbon dioxide
NOAA carbon dioxide observations Carbon cycle factsheet Carbon dioxide emissions by country over time Comparing greenhouse gases by their global warming potential Ocean acidification
References

Collins, M., R. Knutti, J. Arblaster, J.-L. Dufresne, T. Fichefet, P. Friedlingstein, X. Gao, W.J. Gutowski, T. Johns, G. Krinner, M. Shongwe, C. Tebaldi, A.J. Weaver and M. Wehner, 2013: Long-term Climate Change: Projections, Commitments and Irreversibility. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.

Friedlingstein, P., O'Sullivan, M., Jones, M. W., Andrew, R. M., Gregor, L., Hauck, J., Le Quéré, C., Luijkx, I. T., Olsen, A., Peters, G. P., Peters, W., Pongratz, J., Schwingshackl, C., Sitch, S., Canadell, J. G., Ciais, P., Jackson, R. B., Alin, S. R., Alkama, R., ... Zheng, B. (2022). Global Carbon Budget 2022. Earth System Science Data, 14(11), 4811-4900. https://doi.org/10.5194/essd-14-4811-2022

Lan, X., B. D. Hall, G. Dutton, J. Mühle, J. W. Elkins, and I. J. Vimont. (2022). Long-lived greenhouses gases [in State of the Climate in 2021, Chapter 2: Global Climate]. Bulletin of the American Meteorological Society, 103 (8), S81-S84. https://doi.org/10.1175/BAMS-D-22-0092.1.

Lüthi, D., M. Le Floch, B. Bereiter, T. Blunier, J.-M. Barnola, U. Siegenthaler, D. Raynaud, J. Jouzel, H. Fischer, K. Kawamura, and T.F. Stocker. (2008). High-resolution carbon dioxide concentration record 650,000-800,000 years before present. Nature, Vol. 453, pp. 379-382. doi:10.1038/nature06949.

Woods Hole Oceanographic Institution. (2015). Introduction to ocean acidification. Accessed October 4, 2017.

Lindsey, R. (2009). Climate and Earth's energy budget. Accessed October 4, 2017.

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Climate Change: Atmospheric Carbon Dioxide

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In the past 60 years, carbon dioxide in the atmosphere has increased 100 times faster than it did during the end of the last ice age.

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Pupils are faced with data on carbon emissions in different countries. They must work in groups to compare this data through the use of various data comparison techniques and present this to the class. Based on what they have found, pupils must make conclusions about how countries around the world contribute to climate change.

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Students are taught how to plot different types of graphs, some they may have seen before (e.g. bar charts).
Examples are given for each type with reasons why this type of graph might be chosen e.g. line graphs can track changes over time, bar charts can help compare categories, histograms show distribution of data etc.
Model to students how to plot each type of graph from data.
Give students time to practice plotting different graphs to ensure they are confident before giving context.

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Students are sent to find data online for carbon emissions for different countries which they will later analyse and interpret.

Differentiation: To ensure we are meeting differentiated needs, teacher would have some prior researched data that can be given to students who are struggling to find data, also can give more guidance on what data would be good to interpret and analysis - more guidance for those who are struggling to find good data on their own. Those who are confident in finding their own research can be given a greater degree of independence

Collaboration: Students collect their research and as a group, students consider the best way to compare the given data on carbon emissions. Ability to choose from the various examples given in previous lesson

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4. Producing visual representations using data

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4. Producing visual representations using data

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Asking students to produce at least one bar chart, line graph and one histogram for each of the countries they research, and asking them to find data for 5 countries at least. This will ensure the instructions are specific and that everyone does not choose to go for the easy option i.e. just doing a few bar charts and also ensures there is enough work to be getting on with

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Students will use their graphs to work out the aforementioned averages, find relationships between their data and reach conclusions, which will then be presented to the rest of the class.

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- Line graphs
- Histograms
- Bar charts
- Calculate averages - Mean, Median, Mode, Range

Extension task 1: Consider changes in pollution over time (1970 to 2022)

- Use rates of change

Extension task 2: Extrapolate data to look at future trend and consequences

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Include scaffolding such as the empty frequency table above to support students in the creation of their graphs.
Questions such as a and b may support students on what information to include on their posters alongside their graphs.

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Teacher demonstrating how to interpret and plot graphs.

Access to iPad's or computer suite for research

Drawing pencils, paper, rulers, colours

Camera to record presentation assembly for school website

Book a time with a TA to have a look over posters before presenting.

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A group of 30 mixed ability Year 9 students from a range of different backgrounds in a secondary school in Birmingham

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A group of 30 mixed ability Year 9 students from a range of different backgrounds in a secondary school in Birmingham

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This group will have prior knowledge in calculating averages (mean, median, range, mode) but have not yet been exposed to interpreting graphs. Therefore, the students will first need to be taught the different methods for comparing data such as histograms and plotting line graphs. By working in groups, they can develop their collaborative skills such as negotiation and teamwork to present their findings in the final lesson.

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Teaching through a wide variety of pedagogies 

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Teaching through a wide variety of pedagogies 

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Peer to peer dialogue

Research methodologies - critical pedagogy

Not only focusing on impact on the UK - including all student-backgrounds

Live modelling

Opportunities for purposeful practice

Collaborative work - negotiation and discussion when in groups

Empowering student voice - critical pedagogy - enabling learners to choose how they will analyse data and present it to their peers

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L01: Research data for various countries on carbon emissions
L02: Use data to produce graphical representations including line graphs, bar charts and histograms
L03: Interpreting the data by using measures of dispersion and average including mean, median, mode, range
L04: Consider changes over time by calculating rates of change
L05: Extrapolate data to consider future trends

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Students present their findings to the class. This may include showing any graphs that have been created based on the data. With students contributing their methods, reasonings and findings.  At least 3 conclusions based on students findings.
Questions and/or feedback given by peers
Presentation 15 mins.