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Formation of Ozone
O2 + UV-C = O + O
O2 + O = O3
Destruction of Ozone (By humans)
Cl + O3 = ClO + O2
CFCs
Chlorofluorocarbon (GWP 4,000 - 10,000)
Refrigerants
Coolants
Aerosol
Montrell Protocol
Cuts down the CFC usage by 50% by 2020
GWP
Global warming potential - 1
CO2
Carbon Dioxide (GWP - 1)
Most abundant greenhouse gas which is mainly let out through the burning of fossil fuels in cars
N2O
Nitrous Oxide (GWP - 300)
Found in agricultural systems such as fertilizer
CH4
Methane (GWP - 20)
Released from cows and the decomposition of trash
GHGs
An increase in this has led to an increase global temperatures which also leads to climate change
Greenhouse Effect
Some solar radiation reflects off the atmosphere and some is absorbed by the ground (soil and ocean)
Infrared (heat) is released out into space
Greenhouse gases trap the heat in the troposphere (Which is a natural process)
Excess greenhouse gases trap heat in our atmosphere, causing the earth to warm
UV-C
100% of this is absorbed by the Ozone layer
UV-B
95% of this absorbed by the Ozone layer
UV-A
5% of this absorbed by the Ozone layer
Has the lowest radiation and energy
Albedo
Is the measure of a surface's reflectivity.
The higher this is the more reflective whereas the lower it is the less reflective it is
Bleached Coral Reefs
Coral gets stressed easily, spitting out algae causing the coral to bleach
Melting Ice Caps
Since ice is a habitat and has a high albedo, the ice starts to melt. This results in the permafrost land underneath the ice to melt, releasing methane. This is a positive feedback.
Ocean Warming
Oceans absorbing greenhouse gases which leads the oceans to warm. This is mainly in the arctic which causes land ice to melt.
Thermal Expansion
When heated, particles within a substance gain kinetic energy, causing them to move more vigorously and occupy more space. As a result, the substance expands, leading to an increase in its volume.
Habitat Loss
The result of rising sea temperatures causing the destruction of marine ecosystems, impacting biodiversity, and disrupting food chains.
Ocean Acidification
The ongoing decrease in pH levels of Earth's oceans due to the absorption of carbon dioxide from the atmosphere, resulting in increased acidity. This process can harm marine life, particularly organisms with calcium carbonate shells or skeletons, such as coral reefs and shellfish.
This process can harm marine life, particularly organisms with calcium carbonate shells or skeletons, such as coral reefs and shellfish.
The Effects of Ocean Acidification
The Decrease in pH in the Ocean
CO2 + H20 → H2CO2 (Carbonic acid)
Breaks into H+ (Hydrogen Ions) and HCO3- (Bicarbonate Ions)
Coral gets stressed and can’t form reefs which results in the bottom of the food chain disappearing
Impacts on Marine Food Webs
Native Species
A group of organisms that normally live in an area
Introduced Species
An organism that is not native to an area and most likely brought by humans
Invasive Species
An organism that is not native that causes damage to an ecosystem
Endangered Species
Species at risk of extinction due to low population numbers or habitat destruction.
Solutions to Invasive Species
Pesticides
Controlled burns
Endangered Species Act
Put into place to protect and conserve endangered and threatened species and their habitats in the United States.
CITES
Is an international agreement that regulates and monitors the trade of endangered species to protect them from exploitation and ensure their survival.