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How do we know what happened 10,000 years ago?
A lot of the information on climate change is reviewed by the “Intergovernmental Panel on Climate Change” (IPCC). This panel involves over 2,000 of the world’s climate experts. Many of the climate change facts and future predictions we read about come from information reviewed by the IPCC. To get the full story on “How do we know”, check out Backgrounder 5)
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The world’s climate is getting warmer. The average temperature of the globe increased by about 0.6° C between 1900 and 2000. Many regions of the Arctic have warmed up by as much as 5° C in the same 100year period!
Climate change and Global Warming: Same or different? People sometimes call the warming up of the world “global warming”. However, “climate change” describes the full range of changes that are happening. We are getting more than just warmer weather: So climate change includes global warming. Climate change is the bigger picture.
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Warmer temperatures may sound kind of nice, especially in the winter. However, climate change is about a lot more than just warmer temperatures! Here are a few things that are already happening because of climate change:
Worldwide, there are more “extreme” weather events like hurricanes, floods and extended dry periods (called droughts). These extreme events can damage buildings, injure or kill people and wildlife, and destroy food crops. As average temperatures continue to rise, some of these impacts will happen more and more often. (For more details on the impacts of climate change, see Backgrounders 6 to 12).
If the world continues along its present course, scientists predict the average global temperature is expected to rise by 1.4° to 5.8°C between 1990-2100. So what’s the big deal with a few degrees?
Well, in the last ice age, the world was only about 4° to 6°C cooler than it is today. This difference in temperature caused huge areas of the world to be covered by ice. Some animal species disappeared completely. So a few degrees can make a big difference!
And in the North, it is predicted our temperatures will change even more than temperatures in southern Canada. By 2080, winter temperatures over the land areas in the Arctic could rise 2.5° to 14°C above current normal temperatures. Summer temperatures are expected to increase by 4° to 7.5°C above what we now usually get. Remember, a few degrees can make a big difference!

It is true that the world’s climate has always changed. There have been ice ages and there have been warm periods. Isn’t this latest increase in temperature just part of the natural change in the climate? It doesn’t look like it.
Climate change in the past has been caused by natural forces. Sometimes the sun put out more energy. Other times, large volcanoes erupted and the ash they spewed into the air shaded the world from the sun’s warmth. However, since the last ice age – about 10,000 years ago – our temperatures have been pretty stable. That is, they have been stable until the last 100 years or so.
The big difference between warming after the last ice age and current global warming is that this latest change doesn’t appear to be caused by the sun or by volcanoes. It seems to be caused mainly by human activity. And the change is happening very quickly.
“There is new and stronger evidence that most of the warming observed over the last 50 years is attributable to human activity.” The Intergovernmental Panel of Climate Change (IPCC), a United Nation’s organization involving over 2,000 of the |
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The earth is surrounded by a layer of gases we call the atmosphere. When the sun shines down on our world, some of the sun’s energy is reflected back into space by the atmosphere but most of the sun’s energy travels down to us. The land and water also reflect a bit of this energy back into the atmosphere. However, most of the sun’s energy – its heat – is absorbed by the land and water. This absorbed heat is slowly released back up to the atmosphere during day and night.
The atmosphere helps trap some of the heat in. If the atmosphere was not there, the world would get really cold every night. The atmosphere acts like a blanket or a greenhouse. It holds the sun’s heat in and slows down it release into space.
Some of the gases in the atmosphere are key to keeping this heat in. They have been called “greenhouse gases” or GHGs for short. Carbon dioxide, methane and nitrous oxide are the three most common GHGs.

However, you can have too much of a good thing. We need the right amount of GHGs in the atmosphere to keep the right amount of heat in. Too much heat – or too little – can hurt humans and our environment.
The problem is that human activities are adding too many heat-trapping GHGs to the atmosphere. We are tipping the natural balance and that is why our climate is changing.
We put these extra GHGs into the environment in many ways. For example, we put carbon dioxide (CO2) into the atmosphere when we burn gas, diesel, propane and other “fossil fuels”. We burn these fuels to get around in planes and cars, to create electricity, to heat our homes, or to run our industries. When we use these fossil fuels, they release a lot of carbon dioxide into the air.
Fossil fuels |
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Trees and plants help take carbondioxide out of the atmosphere when they make food through a process called “photosynthesis”. But we are cutting down more and more of the world’s forests so we are reducing the number of plants and trees that can help absorb some of the carbon dioxide. (This is a shapshot of the greenhouse effect and greenhouse gases. For more details see backgrounders 2 and 3).
The good news is that if humans are the main cause of this latest change in the climate, then we can help slow down these changes! There are many things that we can do at home or at school. Businesses and governments from around the world are also taking action to reduce the GHGs going into the atmosphere.
For example, people are developing better ways to use renewable energy like the wind and sun so that we don’t have to use as much fossil fuel. Also, new types of fuels are being created from things like sugar cane or cow manure that release fewer GHGs! New cars that can travel much farther on one tank of gas are already on the road. All of these efforts help to reduce the GHGs going into the atmosphere.
Much of the electricity in the world is produced by burning fossil fuels like diesel or coal. So reducing how much electricity you use at home can help reduce the GHGs going into the atmosphere. This can be as simple as turning off lights or computers when you’re not using them. It may mean washing clothes in cold water because it takes electricity or fuel to heat the water. People are also putting more insulation into the walls and attics of their houses so that they will use less oil or gas for heat.
The less electricity and heat you use, the less carbon dioxide you put into the atmosphere. And the less money you spend on electricity and heat! Bonus!
These are just a few ideas about how people can reduce their use of fossil fuels. (For more ideas on solutions to climate change, see backgrounders 13 to 17). Can you think of other things people are doing to reduce how much energy they use?
So climate change is going to have a big impact on our lives and it is something we can’t ignore. This backgrounder provided an overview of what climate change is, how it might impact us, and what we can do to help slow down the changes. For more details on all of these topics, check out the rest of the backgrounders!
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There are many websites on climate change. Here are some starters:
Climate change backgrounders in this Series:
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