The average conditions of the atmosphere in a large region over decades or more, including clouds, precipitation, temperature, humidity, atmospheric pressure, solar radiation, and wind
Climate
Can refer to large and small regions - BC has a range of different climate zones
Each region has certain types of plants, animals, ecosystems, and resources
Climate
The weather of a place averaged over a period of time, including normal weather and the range of weather extremes
Weather
The day-to-day state of the atmosphere, and its short-term variation in minutes to weeks
Determining the past climate
1. Studying fossils and sediments
2. Gathering information about ice
Ice cores are used to determine what types and amounts of gases existed in the atmosphere when the ice was formed
Geologic evidence shows that, throughout its history, Earth has undergone major climatic changes, including ice ages and periods of warming
Scientists draw conclusions about current climatic changes by observing present climate and by comparing their observations with evidence of past climates
What effects climate
Composition of Earth's atmosphere
Earth's tilt, axis of rotation, and orbit around Sun
The water cycle
Ocean currents
The carbon cycle
Catastrophic events
Climate change
Changes in long-term weather patterns in certain regions that affect the redistribution of thermal energy around Earth
Global warming
An increase in Earth's average global temperature, which is one aspect of climate change
Greenhouse effect
The ability of the atmosphere to absorb and emit more thermal energy as greenhouse gases increase
Global warming potential (GWP)
The ability of a substance to warm the atmosphere by absorbing and emitting thermal energy
General circulation models (GCMs)
Computer models designed to study climate, taking into account multiple factors such as changes in greenhouse gas concentrations, ocean currents, winds, surface temperatures, and albedo
The albedo at Earth's surface affects the amount of solar radiation that a region receives
GCMs can determine both past and present climate, and some models predict a temperature rise of 6°C in northern regions and a sea level rise of almost 88 cm within the next 100 years
Climate change is more extreme in developing countries
How the Sun heats the Earth
1. Sun's rays radiate heat towards the Earth
2. Rays reflect off the surface of the Earth, with some heat trapped by the atmosphere and some reflected back into space
3. Light surfaces on Earth absorb heat
4. Dark surfaces on Earth absorb heat
There are more greenhouse gases in the Earth's atmosphere than ever before, and these gases trap more heat in the atmosphere
In Earth's history, there was usually 220-228ppm of CO2, but due to human emissions, there is currently 415ppm
Temperatures have risen approximately 1 degree Celsius since industrial times
What Canada is doing about climate change
Investing in energy-efficient housing, model codes for new and existing buildings
Investing in clean transportation, more electric vehicle charging stations, developing stringent vehicle standards, cleaner fuels
Investing in clean electricity, pricing industrial emissions, reducing methane in the oil and gas sector
Supporting clean agriculture and bioproducts, conserving more nature for carbon sequestration, reforestation, reducing waste including plastic pollution
Phasing out coal-fired electricity, increasing investment in renewable energy, increasing investment in smart grids