Antarctic ozone hole

E729843

The Antarctic ozone hole is a region of severely depleted ozone in the stratosphere above Antarctica that forms each spring due to chemical reactions involving human-made pollutants like chlorofluorocarbons (CFCs).

All labels observed (1)

Label Occurrences
Antarctic ozone hole canonical 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf atmospheric phenomenon ⓘ
ozone depletion region ⓘ
affects southern high-latitude ecosystems ⓘ
ultraviolet radiation levels over Antarctica ⓘ
causedBy CFCs ⓘ
linked to: Freon

chlorofluorocarbons ⓘ
halons ⓘ
human-made pollutants ⓘ
other ozone-depleting substances ⓘ
dependsOn Antarctic polar vortex ⓘ
very low stratospheric temperatures ⓘ
discoveredIn 1980s ⓘ
expectedRecovery mid-21st century or later ⓘ
firstMajorPublicationYear 1985 ⓘ
firstReportedBy British Antarctic Survey ⓘ
hasArea up to about 25 million square kilometers ⓘ
hasCause catalytic destruction of ozone by bromine radicals ⓘ
catalytic destruction of ozone by chlorine radicals ⓘ
hasConsequence increased risk of eye damage from UV exposure ⓘ
increased risk of skin cancer from UV exposure ⓘ
hasMechanism activation of chlorine from reservoir species ⓘ
formation of polar stratospheric clouds ⓘ
heterogeneous chemistry on polar stratospheric cloud particles ⓘ
springtime sunlight-driven photochemistry ⓘ
hasPart severely depleted ozone layer ⓘ
hasPeakExtentMonth October ⓘ
September ⓘ
hasProperty enhanced ultraviolet radiation at surface ⓘ
recurring annually ⓘ
seasonal ⓘ
severe ozone depletion ⓘ
locatedAbove Antarctic continent ⓘ
linked to: Antarctica
locatedIn stratosphere ⓘ
location Antarctica ⓘ
measuredInUnits Dobson Units ⓘ
mitigatedBy Montreal Protocol ⓘ
phase-out of CFCs ⓘ
observedBy balloon-borne instruments ⓘ
ground-based Dobson spectrophotometers ⓘ
satellite instruments ⓘ
occursInMonth October ⓘ
September ⓘ
early November ⓘ
occursInSeason austral spring ⓘ
relatedTo Arctic ozone depletion ⓘ
global ozone depletion ⓘ
trend signs of gradual recovery in early 21st century ⓘ
typicalMinimumOzoneColumn less than 100 Dobson Units ⓘ
typicalUndisturbedOzoneColumn about 300 Dobson Units ⓘ

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

OMPS → monitors → Antarctic ozone hole ⓘ