Linked from
The 30 pages that link to Chlorofluorocarbon, each with the reason it gives.
Montreal ProtocolBroader topic: Their widespread use made them an early priority for phaseout.
OzoneRelated: In the stratosphere, chlorine released from these compounds catalytically destroys ozone.
Ozone depletionRelated: Stratospheric ultraviolet light breaks these compounds apart, releasing chlorine that catalytically destroys ozone.
RefrigerantCompared with: CFC refrigerants were phased out because they deplete stratospheric ozone.
Atmospheric lifetimeBroader topic: Some members remain aloft long enough to reach the stratosphere and release ozone-destroying chlorine.
Antarctic Bottom WaterBroader topic: CFC measurements reveal how recently Antarctic-sourced waters entered the deep ocean.
Antarctic ozone holeNarrower topic: Their atmospheric breakdown supplies the chlorine responsible for most ozone-hole depletion.
HydrofluorocarbonCompared with: HFCs replaced many CFC uses without the chlorine-driven ozone destruction.
Ozone holeRelated: Their long-lived emissions supplied most of the chlorine behind the Antarctic depletion.
Kigali AmendmentRelated: Their control under the Montreal Protocol shaped the succession of replacement refrigerants.
HydrochlorofluorocarbonCompared with: HCFCs were developed as less ozone-depleting replacements for these compounds.
Ozone-depleting substanceBroader topic: This widely used substance class became a major source of stratospheric chlorine.
Thomas Midgley Jr.Broader topic: Midgley helped develop CFC refrigerants that later proved damaging to stratospheric ozone.
F. Sherwood RowlandRelated: Rowland and Molina identified these persistent chemicals as the source of ozone-destroying chlorine.
Mario MolinaRelated: Molina identified these long-lived compounds as sources of ozone-destroying chlorine.
Polar stratospheric cloudRelated: These gases provide much of the chlorine that cloud reactions convert into ozone-destroying forms.
Aerosol propellantRelated: CFC propellants served many aerosol products before ozone-depletion concerns drove restrictions.
James LovelockRelated: Lovelock detected these compounds in the atmosphere, demonstrating their global distribution.
Carbon tetrachlorideRelated: CCl₄ is an industrial feedstock for producing several chlorofluorocarbons.
InhalerRelated: Their former use as inhaler propellants drove a major device reformulation.
1,1,1-TrichloroethaneRelated: CFC controls under the treaty established the policy precedent for phasing out this related solvent.
HaloalkaneBroader topic: This haloalkane family became a major source of stratospheric ozone depletion.
DichlorodifluoromethaneNarrower topic: CFC-12 belongs to this family of compounds.
HalocarbonBroader topic: CFCs are a well-known halocarbon family associated with stratospheric ozone depletion.
Organochlorine chemistryBroader topic: CFCs connected organochlorine chemistry to stratospheric ozone depletion and global controls.
TrichlorofluoromethaneNarrower topic: CFC-11 belongs to this stable, ozone-depleting family of industrial chemicals.
1,1,1,2-TetrafluoroethaneCompared with: R-134a was adopted in many applications as a replacement for ozone-depleting CFCs.
Carbon tetrafluorideCompared with: Unlike chlorofluorocarbons, CF₄ contains no chlorine and does not deplete stratospheric ozone.
ChlorodifluoromethaneCompared with: HCFC-22 contains hydrogen, unlike fully halogenated CFC refrigerants, and generally has lower ozone-depletion potential.
FluorocarbonBroader topic: CFCs are a major historical fluorocarbon application, later restricted for ozone damage.