Formed through a specific kind of reaction: UV radiation strikes oxygen molecules (O2) and splits them into two atmospheric oxygen atoms (O), which then react with O2 to form O3 (ozone molecules)
Ozone depletion was first discovered in 1985, and it was discovered because of a giant hole or thinning of ozone that formed over the Antarctic pole. This thinning occurs seasonally and is caused by man-made chemicals, which are anthropogenic.
Written in the 1980s to help protect stratospheric ozone from further depletion by phasing out CFCs and replacing them with other chemicals, such as hydrofluorocarbons (HFCs)
A naturally occurring process that keeps our planet warm. Heat from the sun enters Earth's atmosphere and is trapped by greenhouse gases, keeping the surface of the planet warm.
A feedback loop that encourages further warming, such as: Thawing of tundra permafrost, releasing methane, which is a strong greenhouse gas; Melting of ice and snow, reducing albedo (reflectivity) and allowing more heat to be absorbed.
Thawing of permafrost and releasing methane: As temperatures increase, permafrost thaws, releasing methane. Methane is a strong greenhouse gas, encouraging further warming.
Melting of ice and snow: As temperatures increase, ice and snow melt, exposing water. Water has a lower albedo than ice and snow, absorbing more heat and encouraging further warming.
Ice melting leads to loss of primary hunting grounds for species such as polar bears. Species may move into different locations as biomes shift due to temperature increases. Tropical rainforests and savannahs are expanding north and south as temperatures rise.
Diseases spread further north and south as species like mosquitoes move into new areas. Soil productivity changes. Ocean and wind currents shift. Increase in ice melting, leading to sea level rise. Thermal expansion of the ocean, causing ocean volume to increase.
The decrease in the pH level of the ocean over time, caused by the absorption of carbon dioxide from the atmosphere. CO2 absorption by the ocean leads to the formation of carbonic acid, which makes it difficult for shelled organisms to build their shells.