8.2 kiloyear event

E87434

The 8.2 kiloyear event was a sudden, short-lived global cooling episode during the early Holocene, likely triggered by massive meltwater outbursts disrupting North Atlantic ocean circulation.

Aliases (1)

Statements (46)
Predicate Object
instanceOf Holocene cooling event
abrupt climate change event
climatic event
paleoclimatic anomaly
alsoKnownAs 8.2 ka event
8.2 kyr event
8.2 thousand years ago cooling event
approximateAgeBeforePresent 8200 years
associatedWith Laurentide Ice Sheet decay
drainage of proglacial lakes Agassiz and Ojibway
cause disruption of North Atlantic thermohaline circulation
freshwater influx into North Atlantic Ocean
massive meltwater outburst
characteristic global or near-global impact
short-lived cooling
sudden onset
chronologicalPosition approximately 6200 BCE
duration about 100 to 200 years
effect changes in atmospheric circulation patterns
changes in monsoon systems
cooling in North Atlantic region
hydrological changes in many regions
reduction in Northern Hemisphere temperatures
evidenceFrom Greenland ice cores
lake sediment records
marine sediment cores
pollen records
speleothem records
follows Younger Dryas termination
geographicExtent Northern Hemisphere
global climate system
primarily North Atlantic region
impactOn agricultural development in the Near East
early Neolithic societies in some regions
linkedTo temporary weakening of North Atlantic Deep Water formation
partOf Holocene climate variability
precedes 4.2 kiloyear event
relatedTo Atlantic Meridional Overturning Circulation
freshwater forcing experiments in climate models
significance constraint on climate model sensitivity to freshwater input
natural analogue for abrupt climate change
studiedIn Holocene climate research
Quaternary science
paleoclimatology
temperatureAnomaly cooling of about 1 to 3 degrees Celsius in some regions
timePeriod early Holocene

Referenced by (2)
Subject (surface form when different) Predicate
8.2 kiloyear event ("8.2 kyr event")
alsoKnownAs
Holocene
containsEvent

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