Chlorofluorocarbons (CFCs) are synthetic chemicals that were widely used in various industrial and consumer products, such as refrigerators, air conditioners, and aerosol sprays. When released into the atmosphere, CFCs rise to the stratosphere, where they break down and release chlorine atoms. These chlorine atoms then react with ozone molecules, destroying them and leading to ozone depletion.

The ozone layer in the Earth's atmosphere plays a crucial role in protecting life from harmful ultraviolet (UV) radiation emitted by the sun. Ozone molecules absorb UV radiation, preventing it from reaching the Earth's surface. This protection is essential for the survival of many organisms, including humans, as excessive UV radiation can cause skin cancer, cataracts, and other health issues.

Ozone depletion is primarily associated with negative consequences, such as increased risk of skin cancer, damage to crops and marine life, and potential impacts on climate. Improved air quality is not a direct consequence of ozone depletion.

The Montreal Protocol is an international agreement that was adopted in 1987 to address the issue of ozone depletion. It aims to phase out the production and use of ozone-depleting substances, such as chlorofluorocarbons (CFCs), in order to protect the ozone layer.

Solar flares are powerful bursts of energy from the sun that can release high levels of ultraviolet (UV) radiation. This UV radiation can interact with oxygen molecules in the stratosphere, breaking them down and leading to the formation of ozone-depleting substances, such as nitric oxide (NO).

The ozone layer is a relatively thin layer in the Earth's atmosphere, located in the stratosphere. It typically ranges from about 10 to 20 kilometers above the Earth's surface.

Ozone depletion is associated with several adverse effects on human health, including increased risk of cataracts, weakened immune system, and reduced lung function. Improved cardiovascular health is not a known impact of ozone depletion.

The term 'ozone hole' refers to a significant thinning of the ozone layer over certain regions of the Earth, particularly over the Antarctic. This thinning is caused by the accumulation of ozone-depleting substances in the stratosphere, leading to a reduction in ozone concentration.

Ultraviolet (UV) radiation from the sun is classified into three main types: UVA, UVB, and UVC. UVD is not a type of UV radiation.

Ozone-depleting substances, such as chlorofluorocarbons (CFCs), release chlorine and bromine atoms when they break down in the stratosphere. These atoms then react with ozone molecules, destroying them and leading to ozone depletion.

Ozone-depleting substances, such as chlorofluorocarbons (CFCs), were commonly used in various applications, including as refrigerants, aerosol propellants, and fire extinguishers. Medical inhalers typically do not contain ozone-depleting substances.

The observed recovery of the ozone layer in recent years is primarily attributed to the implementation of the Montreal Protocol, an international agreement that phased out the production and use of ozone-depleting substances.

Ozone depletion can have several negative impacts on marine ecosystems, including reduced phytoplankton productivity, increased coral bleaching, and damage to marine larvae. Enhanced fish growth is not a known impact of ozone depletion.

Tropospheric transport refers to the process by which ozone-depleting substances, such as chlorofluorocarbons (CFCs), are transported from the Earth's surface to the stratosphere through various atmospheric processes, including convection, advection, and diffusion.

Ozone depletion can have several negative impacts on terrestrial ecosystems, including reduced crop yields, increased forest fires, and damage to tree seedlings. Enhanced plant growth is not a known impact of ozone depletion.